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Item 7 - Appendix 1

West Dunbartonshire Council · 19 August 2026
Back to Infrastructure, Regeneration & Economic Development Committee — 19 August 2026 and its agenda

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CLYDEBANK
SURFACE
WATER
MANAGEMENT
PLAN 
SWMP
West Dunbartonshire Council
16th July 2026   
ITEM 7 - APPENDIX 1

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Notice
This document and its contents have been prepared and are intended solely as information for West
Dunbartonshire Council and use in relation to Draft for comment
AtkinsRéalis UK Limited assumes no responsibility to any other party in respect of or arising out of or in connection
with this document and/or its contents.
This document has 97 pages including the cover. 
Document history
Document title: Clydebank Surface Water Management Plan 
Revision Purpose description Originated Checked Reviewed Authorised Date
1.0 Draft for comment HP AD CA - 30/04/2024
2.0 Client comments HP AW BC ZT 16/07/2026       
Client signoff
Client West Dumbartonshire Council
Project SWMP
Job number  
Client
signature/date

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Contents
1. Introduction ............................................................................................................................................... 5
1.1 Legislative Background .................................................................................................................. 5
1.2 Area Specific Background .............................................................................................................. 5
1.3 Potentially Vulnerable Area Summary ........................................................................................... 6
1.4 Surface Water Management Plan Stages...................................................................................... 6
1.5 Catchment Background.................................................................................................................. 7
2. Data Collection and Gap Analysis .......................................................................................................... 8
3. Methodology ............................................................................................................................................. 9
3.1 Steps .............................................................................................................................................. 9
3.1.1 Define Catchment Extent (Step 1) ................................................................................................. 9
3.1.2 Review of Historical Flood Data (Step 2) ..................................................................................... 10
3.1.3 Define Hotspots (Step 3) .............................................................................................................. 11
3.1.4 Hotspot Delineation (Step 4) ........................................................................................................ 13
3.1.5 Hotspot Interactions ..................................................................................................................... 14
4. Improved Understanding of Flood Risk ............................................................................................... 16
4.1 Root Cause Analysis Summary ................................................................................................... 16
4.2 Root Cause Analysis: Desktop .................................................................................................... 18
4.2.1 Second Avenue / Ramsey Street ................................................................................................. 18
4.2.2 Western Isles Road ...................................................................................................................... 19
4.2.3 Duntocher Road ........................................................................................................................... 19
4.2.4 Livingstone Street ........................................................................................................................ 20
4.2.5 Melbourne Avenue ....................................................................................................................... 21
4.2.6 Low Crescent ............................................................................................................................... 22
4.2.7 Dumbarton Road .......................................................................................................................... 22
4.2.8 Dunedin Terrace .......................................................................................................................... 23
4.2.9 Kilbowie Road .............................................................................................................................. 24
4.2.10 Station Road ................................................................................................................................ 25
4.3 Root Cause Analysis: Modelling .................................................................................................. 26
4.3.1 1D Sewer Network Modelling ....................................................................................................... 26
4.3.2 Pluvial Only Flood Modelling ........................................................................................................ 38
4.3.3 Integrated 1D - 2D Runoff Model ................................................................................................. 47
4.3.4 Model Limitations ......................................................................................................................... 57
4.3.5 Future Flood Risk ......................................................................................................................... 57
5. Set Objectives ......................................................................................................................................... 59
6. Option Appraisal ..................................................................................................................................... 61
6.1 Scoping Option Appraisal............................................................................................................. 61
6.2 Options Assessed ........................................................................................................................ 63
6.2.1 Non-Structural .............................................................................................................................. 63
6.2.2 Structural ...................................................................................................................................... 65
6.2.3 Property Level Protection ............................................................................................................. 66
6.2.4 SuDS Types ................................................................................................................................. 67
6.3 Develop Preferred Option / Screening ......................................................................................... 70
6.3.1 Second Avenue / Ramsay Street ................................................................................................. 70
6.3.2 Western Isles Road ...................................................................................................................... 72
6.3.3 Duntocher Road ........................................................................................................................... 73
6.3.4 Livingstone Street ........................................................................................................................ 75
6.3.5 Melbourne Avenue ....................................................................................................................... 76
6.4 Prioritising Options ....................................................................................................................... 78
6.4.1 Second Avenue / Ramsay Street ................................................................................................. 79
6.4.2 Western Isles Road ...................................................................................................................... 80
6.4.3 Duntocher Road ........................................................................................................................... 81
6.4.4 Livingstone Street ........................................................................................................................ 82
6.4.5 Melbourne Avenue ....................................................................................................................... 83
6.5 Baseline: ‘Do minimum’................................................................................................................ 84
6.6 Options: ‘Do something’ ............................................................................................................... 84

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7. Develop preferred option: confirm funding ......................................................................................... 86
8. Conclusions ............................................................................................................................................ 89
8.1 Recommendations ....................................................................................................................... 91
Appendix A. Objectives .................................................................................................................................. 94

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1. Introduction
AtkinsRéalis was commissioned by West Dunbartonshire Council (WDC) in 2023 to undertake a Surface Water
Management Plan (SWMP) for the Clydebank catchment. The initial SWMP was completed and submitted in
April 2024, based on the best available information at that time, including SEPA Flood Maps, historical flood
records, stakeholder information and hydraulic modelling outputs.
Following submission of the report, a stakeholder workshop was held in December 2025, with representatives
from WDC, Scottish Water (ScW), Network Rail and Scottish Canals to discuss flooding mechanisms, ongoing
investigations, known data gaps and opportunities for collaboration across the catchment. In addition, the release
of the updated 2025 SEPA Flood Maps provided a revised understanding of surface water flood risk, resulting in
notable changes to the extent and significance of flooding predicted at a number of hotspot locations.
This report revisits the original SWMP findings considering the updated flood mapping, stakeholder feedback and
ongoing investigations to provide an updated understanding of flood risk within the Clydebank catchment. The
review identifies where the understanding of flood mechanisms has changed, highlights key uncertainties and
knowledge gaps, and makes recommendations for future investigation and flood risk management activities. It
should be noted that the flood management options developed as part of the original SWMP have not been
revisited or remodelled as part of this update. Consequently, the options should be considered in the context of
the improved understanding of flood risk now available, considering the need for a collaborative approach in the
catchment and reviewed before any future progression to detailed appraisal or implementation.
1.1 Legislative Background
Under the Flood Risk Management (Scotland) Act 2009, all Local Authorities are required to develop a SWMP
for the areas as outlined in SEPA’s Flood Risk Management Plan (FRMP) document which fall under their
responsibility. These plans need to assess the objectives set out in the FRMP. The actions typically include
identifying and assessing the risk of surface water flooding in the urban areas and proposing a course of action
for the next steps to reduce the flood risk through a risk-based approach. This assessment includes considering
present and future flood risk.
1.2 Area Specific Background
Clydebank was outlined as an area requiring a Sewer Flood Risk Assessment to be completed in Cycle 2 of the
FRMP (2022 – 2028) in the Clyde 2. This involves the volume of water that would overwhelm the sewer system
and cause flooding from manholes or inside homes to be assessed, to support understanding the performance
of the urban drainage network. ScW will complete this assessment within the highest priority sewer catchments,
this includes the Dalmuir catchment. This will help improve knowledge and understanding of potential surface
water flood risk. 
Clydebank was outlined as requiring a SWMP to be completed after Cycle 2. The indicative timescales are after
June 2028. The specific action reference is 54021. The additional information uncovered in the Sewer flood risk
assessment and through developments in flood risk management planning between 2022-2028 should be
considered when this commences.
The specific action outlined was “Areas at risk of heavy or prolonged rainfall causing flooding due to water
ponding on man-made surfaces or overwhelming the drainage system are to be identified. This priority area will
provide a baseline for the identification of next steps in managing water ponding or over-whelmed drainage
systems. This should guide adaptive planning to allow for the impacts of climate change to be monitored,
understood, and managed”.
This report will therefore: 
1 Flood risk management plans 2021 (sepa.org.uk)

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 Summarise the areas identified as being at risk of flooding because of water ponding caused by heavy or
prolonged rainfall within the urban catchment. 
 Select priority areas based on the outcomes of a multi-criteria assessment.
 Set out the next steps.
1.3 Potentially Vulnerable Area Summary
The Potentially Vulnerable Area (PVA) is situated in Clydebank, which is located on the River Clyde within the
West Dunbartonshire local authority area (refer to Figure 1-1). This area is most at risk from surface water and
sewer flooding. However, there is also a risk of river and coastal flood risk from the tidally influenced River Clyde.
According to the Local Flood Risk Management Report there are approximately 1,800 people at risk of flooding
and approximately 1,200 homes and businesses. This is estimated to increase to 2,700 people and 1,700 homes
and businesses by 2080 due to climate change.2 
Figure 1-1 - Map showing Clydebank PVA defined by SEPA
1.4 Surface Water Management Plan Stages
To help develop the SWMP, this report follows the structure set out in the stages of SWMP wheel (see Figure 1-
2) outlined in the Scottish Government’s SWMP Guidance (2018).3 This outlines the stages when developing a
surface water management plan to ensure a plan is developed in accordance with the Flood Risk Management
(Scotland) Act 2009. 
2 https://www.west-dunbarton.gov.uk/media/ewmdtdtz/local-flood-risk-management-plan-2022-2028.pdf
3 2 The surface water management planning process - Surface water management planning: guidance (2018) - gov.scot (www.gov.scot)

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Figure 1-2 - Stages of Surface Water Management Plan Process (Scottish Government)
This study follows the ‘Develop Plan’ phase of the SWMP wheel stages. This includes:
 Prepare: data collection and desktop analysis of flooding records and SEPA flood maps
 Understand flood risk: this will build and improve on the initial understanding of flood risk by developing
hydraulic models to inform root causes analysis. 
 Set objectives: establish an understanding of the key objectives the Council have for development of
the SWMP, based on the increased understanding of flood risk in the hotspot areas.
 Option appraisal: high-level assessment of potential mitigation opportunities
 Option development: refinement of indicative opportunities identified
 Future actions and stakeholder engagement: Summarize key findings, recommendations and
outputs and include proposals for monitoring.
1.5 Catchment Background
Clydebank is a town situated just 10km northwest of Glasgow City Centre. The town is situated on the north bank
of the River Clyde, which flows from southeast to northwest. Clydebank is bound to the north by the Kilpatrick
Hills, which reach a height of approximately 400m. 
The area was largely rural until the end of the 19th century, when the growth of the shipbuilding industry on the
river led to the foundations of Clydebank. Today, Clydebank is heavily urbanised and has a population of
approximately 26,220. 4The town is served by the Dalmuir sewage network. 
4 https://www.west-dunbarton.gov.uk/media/w50dczjc/clydebank-data-pack-final.pdf

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2. Data Collection and Gap Analysis
A critical element of a SWMP is the accuracy of the data collected and the analysis. Data shared by stakeholders
was reviewed for quality, accuracy, completeness and to understand if there were any gaps in the provided data
and how the lack of this data would impact the confidence in outputs of this project. Table 2-1 summarises the
data requested and how it was used in the study to assess flood risk.
Data Source Study Purpose
OS MasterMap West Dunbartonshire
Council
Plan production / reporting and study planning
OS OpenMap
(Building Outlines)
Open-Source Data To aid identification of flooding hotspots
Ground Data (LiDAR
data). 1m resolution.
National LiDAR Programme
– data.gov.uk
Produce a Digital Terrain Model (DTM) of the study
area
National Receptor
Database
SEPA Assess properties that are at medium or high
surface water flood risk as outlined by SEPA Flood
Maps
SEPA Flood Maps
Extents
SEPA To aid identification of flooding hotspot areas based
on where the SEPA medium and high-risk flood
maps intersected National Receptor Data building
centroids or OS Building maps
Hydraulic Models (1D
Sewer Model – ICM
Model: DOA000333
Dalmuir Current v24)
ScW To aid root cause analysis of flooding, determining
engineered subcatchments to hotspots, and more
detailed integrated modelling
Hydraulic Model
Maintenance Report
ScW Provides additional background information in
relation to the model build, model calibration and
verification.
Historic Flooding
Records (GIS
format)/ Hotspot Data
West Dunbartonshire
Council
To assist in identification of flooding hotspot areas
and in root cause analysis
Information on
flooding from the
sewer network
ScW To assist in identification of flooding hotspot areas
and in root cause analysis
Table 2-1 - Data Requested and Usage

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3. Methodology
3.1 Steps
A methodology was developed to understand surface water flood risk within Clydebank. This methodology is
summarised in Table 3-1 Error! Reference source not found.and explained in more detail in the subsequent
sections of the report.
Step Process Why?
1 Define Catchment Extent 
Delineate natural watershed
contributing flows to PVA to
determine ‘area of interest’
To identify the catchment extent that may be
contributing flows to the PVA target areas and the
area where the 'hotspot' will be identified. 
2 Review of historical flooding data To support understanding of catchment issues
and help define flooding ‘hotspots’.
3 Define 'Hotspots' Using SEPA flood maps identify the most at-risk
areas within the 'area of interest' to help
understand the worst-hit flooding areas within the
catchments and obtain an initial understanding of
where funding may be targeted.
4 Hotspot Delineation 
Define Natural Watershed for each
hotspot area. 
Define engineered catchment for
each hotspot area.
To identify the catchment extent that may be
contributing flows to each individual 'hotspot'
area. 
To identify the engineered catchment conveying
flows to each individual ‘hotspot’ areas. 
Mitigation measures will likely be installed
upstream to help mitigate flooding at the
downstream location. Therefore, we must
understand the area in which measures could be
installed.
5 Root Cause Analysis To understand the origin of flooding at the
hotspot to quantify the extent of the issue and
establish the potential interaction of different
causes of flooding and what actions are needed
to mitigate this flooding.
Table 3-1 - Methodology Steps
3.1.1 Define Catchment Extent (Step 1)
The natural watershed for the PVA Action area was obtained because this would be used as the initial pluvial
extent (‘area of interest’). This was to ensure that the assessment was accounting for all natural flows that may
contribute to the SWMP extent.

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Figure 3-1 shows the ‘area of interest’ in relation to the Clydebank PVA. 
Figure 3-1 - Map showing the area that naturally drains via gravity towards the PVA target areas ('area
of interest')
3.1.2 Review of Historical Flood Data (Step 2)
Historical flood information was reviewed to support the understanding of flood risk and flood mechanisms within
the study area. Following the initial submission, a stakeholder workshop was held in December 2025 with
representatives from WDC, ScW, Network Rail and Scottish Canals to discuss known flooding issues and provide
additional local knowledge. This information has been used throughout the updated assessment to validate
hotspot identification and improve understanding of the factors contributing to flooding.
The following sections summarise the available historical flooding information. A desktop review of the historical
flood records, stakeholder information and supporting datasets was undertaken to identify likely flooding
mechanisms and contributing factors at each location. The findings of this assessment are summarised within
Section 4.2 – Root Cause Analysis, which presents the evidence used to develop an understanding of the causes
of flooding at each hotspot and to assess the implications of the updated 2025 SEPA Flood Maps on the original
SWMP findings.
3.1.2.1 West Dunbartonshire Council 
The WDC flood records were used to help validate areas identified as being susceptible to flooding and to provide
additional insight into local flood mechanisms. In particular, the records assisted in distinguishing between
locations affected primarily by surface water flooding and those influenced by interactions between surface water,
watercourses and sewerage infrastructure. The information also helped identify locations where flooding has
resulted in impacts to residential properties, transport infrastructure and access routes.

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3.1.2.2 Scottish Water 
Historical flood information was obtained through engagement with ScW, including the workshop held in
December 2025 and subsequent discussions relating to individual hotspot locations. This information was
supplemented by a review of the hydraulic model. Collectively, these sources provided valuable insight into
previous flooding incidents, known sewer network constraints, ongoing investigations and potential flood
mechanisms across the study area.
3.1.3  Define Hotspots (Step 3)
As part of the initial assessment undertaken for the first submission of the SWMP, potential surface water flood
risk was identified using the SEPA flood maps available at the time. Surface water flooding, otherwise referred
to as pluvial flooding, occurs when rainfall-generated runoff is unable to infiltrate into the ground or enter a
watercourse, drainage system or sewer network, resulting in water collecting on the surface or flowing overland. 
SEPA flood maps assess flooding associated with severe rainfall events for the following annual exceedance
probabilities (AEP):
 1 in 10 year (10%) Annual Exeedance Probability (‘High’ likelihood);
 1 in 200 year (0.5%) Annual Exeedance Probability (‘Medium’ likelihood); and
 1 in 1000 year (0.1%) Annual Exeedance Probability (‘Low’ likelihood).
Hotspots were identified as areas containing six or more residential and/or non-residential properties located
within the SEPA medium-likelihood (0.5% AEP) surface water flood extent. In addition, locations identified by
WDC where flooding could result in significant disruption to transport, access for emergency services, or wider
economic activity were also designated as hotspots, regardless of the number of properties affected. Hotspot
polygons were delineated to encompass the full extent of the mapped surface water flooding associated with the
affected properties.
The historical flood records from WDC, information provided by ScW, and other available evidence sources were
used alongside the SEPA flood maps to build confidence in hotspot identification and to improve understanding
of the underlying flood mechanisms. During the initial assessment, hotspots were ranked according to the scale
of potential impact, with locations containing the greatest number of properties at risk receiving the highest
priority, these were then agreed with WDC. The hotspots identified for Clydebank are presented in Figure 3-2
and Table 3-2.

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Figure 3-2 - Map showing flood 'hotspot' areas 
Rank Hotspot Name Council Ward / Within PVA Action Areas
1 Second Avenue / Ramsay Street Clydebank Central / Yes
2 Western Isles Road Clydebank Waterfront / No
3 Duntocher Road Clydebank Central / Yes - partial
4 Livingstone Street Clydebank Central / Yes - partial
5 Melbourne Avenue Clydebank Central / No
6 Low Crescent Clydebank Waterfront / No
7 Dumbarton Road Clydebank Waterfront / Yes
8 Dunedin Terrace Clydebank Waterfront / Yes
9 Kilbowie Road Clydebank Central / Yes
10 Station Road Clydebank Waterfront / No
11 Dumbarton Road (west) Dumbarton / No
Table 3-2 - List of Hotspots and the Council Ward they are located within
Following publication of the updated 2025 SEPA Flood Maps, the hotspot assessment was reviewed as part of
this updated SWMP submission. The revised mapping resulted in changes to the extent and severity of surface
water flood risk at a number of locations, and consequently some hotspots identified during the initial assessment
no longer met the original screening criteria. The implications of the 2025 SEPA Flood Maps are described in
Section 4.2, Root Cause Analysis: Desktop.

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3.1.4 Hotspot Delineation (Step 4)
3.1.4.1 Natural Watersheds
When the capacity of the engineered drainage system is exceeded, surface water runoff is unable to enter the
drainage network and remains on the ground surface. The runoff therefore follows natural overland flow pathways
governed by local topography. In urban areas, surface water will typically convey along road corridors and kerb
lines, whereas in rural areas it generally follows natural drainage routes and topographic gradients before
accumulating in low-lying areas or local depressions. Where significant volumes of runoff accumulate, this can
result in pluvial flooding.
To better understand the natural drainage characteristics of the catchment, watershed boundaries were
delineated upstream of each hotspot using a Digital Terrain Model (DTM). This analysis was undertaken to
identify contributing catchment areas and determine the natural overland flow paths that could influence flooding
at each location. The DTM was derived from LiDAR data obtained through the National LiDAR Programme and
has a maximum spatial resolution of 0.5 m, providing a high level of detail for assessing local topographic controls
on surface water flow.
Figure 3-3 provides a map showing the natural (or overland) catchments for each hotspot. 
Figure 3-3 - Map showing natural watershed boundaries for each hotspot
3.1.4.2 Engineered Systems
The ScW sewer model incorporates subcatchment boundaries that have been delineated based on the areas
expected to drain to the sewer network. This approach represents the engineered urban drainage system,
whereby surface runoff is conveyed to road gullies and roof drainage systems before entering the below-ground
sewer network. Once within the network, flows are routed through a series of pipes and associated infrastructure
towards treatment facilities or, in the case of storm systems, designated outfalls.

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Under typical conditions, the drainage system is designed to accommodate more frequent rainfall events, with
road gullies generally intended to intercept runoff up to approximately the 1 in 5-year return period event. As a
result, the volume of water entering the sewer network is constrained by both gully capacity and the hydraulic
capacity of the sewer system itself. During more extreme rainfall events, runoff can exceed the capacity of the
engineered drainage network, preventing flows from entering the system. When this occurs, excess surface water
remains above ground and follows natural overland flow routes governed by local topography, potentially
resulting in exceedance flows, flow ponding and pluvial flooding.
Figure 3-4 provides a map showing the engineered (or below ground sewers) catchments for each hotspot.It
should be noted that the hotspots “Station Road” and “Dunbarton Road (west) are not covered by the sewer
model, and therefore not considered to contribute engineered flows to the sewer network. 
Figure 3-4 - Map showing the engineered catchment for each hotspot
3.1.5 Hotspot Interactions
Interactions between the hotspots were assessed to determine how runoff and potential solutions in one location
may influence the hydraulics of another. For example, Duntocher Road is in the upstream extents of the
catchment, and so surface water removed from the system at that point may influence Second Avenue further
downstream, with the hydraulic benefit accumulating increasingly further downstream. Figure 3-5 shows a
simplified schematic of hotspot interactions in the catchment. As solutions have also been accounted for on the
surface water sewer system, watercourses may subsequently benefit from the attenuation of retrofitted SuDS. 
More complex interactions between the systems may occur which have not been captured, such as overflows
between the foul / combined system and storm systems, in addition to bifurcations.

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Figure 3-5 – Schematic of the hydraulic linkages between the hotspots within the Clydebank area

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4. Improved Understanding of Flood
Risk
4.1 Root Cause Analysis Summary
Analysis is required to identify the root causes of flooding at each hotspot, as this provides the evidence base for
determining whether intervention is needed and, if so, the most appropriate actions to pursue. Without a clear
understanding of the root causes, there is a risk that solutions may be progressed which do not maximise the
potential hydraulic benefits or effectively reduce flood risk.
To identify effective flood mitigation options, it is important to understand:
• The source of flooding – i.e. surface water, sewer flooding, river flooding, groundwater flooding, or a
combination of flood mechanisms.
• The pathway taken by flood waters from source to receptor.
• The location of receptors where flooding occurs and water ultimately ponds or accumulates.
An initial root cause analysis was undertaken for the eleven flood hotspots identified across Clydebank using the
best available information at the time, including historic flood records, SEPA Flood Maps and ScW sewer model
outputs. Since completion of the original assessment, SEPA has published updated Flood Maps (2025),
incorporating enhanced datasets and modelling methodologies. These updates indicate changes in predicted
flood risk at a number of locations and have been taken into account during this review.
Following submission of the first iteration of the Clydebank SWMP in April 2024, a workshop was held in
December 2025 involving WDC, ScW, Scottish Canals and Network Rail. The workshop explored opportunities
to align flood risk management interventions with existing and planned investment programmes across the
catchment. Discussions highlighted the interconnected nature of surface water, sewerage, railway drainage,
watercourse and canal systems, reinforcing the importance of continued collaboration to develop sustainable,
catchment-wide solutions. Particular focus was placed on flooding affecting Clydebank Station, opportunities
associated with the Forth and Clyde Canal, and ongoing ScW investigations, including the Dalmuir System Plan,
through which ScW is seeking to better understand local authority priorities and identify potential opportunities
for coordinated investment.
The hotspot assessments presented in the following sections have been updated to reflect the outcomes of the
December 2025 workshop, the publication of the 2025 SEPA Flood Maps, and subsequent engagement with
ScW regarding ongoing investigations within the catchment. The review comprised two stages: an initial desktop
assessment of available evidence, followed by a modelling-based appraisal using sewer, pluvial and integrated
hydraulic modelling outputs.
It should be noted that the hydraulic modelling was completed prior to the December 2025 workshop and
publication of the 2025 SEPA Flood Maps. Consequently, the modelling results have been interpreted alongside
more recent information, including updated flood mapping, emerging findings from ongoing investigations, and
an improved understanding of interactions across the drainage network. In some locations, this newer evidence
suggests that elements of the original modelling assessment may need to be revisited as the outcomes of current
ScW investigations become available. The updated analysis therefore draws on both the original study findings
and the latest understanding of flood risk across the catchment.
The initial areas at greatest risk (‘flood hotspot’) were identified and are summarised in Table 4-1.
Table 4-1 - Hotspot summary
Hotspot
Number
Hotspot
Name Flooding Mechanism
Historic
Flooding
Reported
Flooding
Impact Data Gaps
1
Second
Avenue /
Ramsay Street
Surface water / sewer  Yes (LA
and ScW)
Building /
road

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2 Western Isles
Road Surface water / sewer  Yes (LA) Building /
road 
3 Duntocher
Road
Surface water / sewer / potential fluvial
(unnamed watercourse north of
Duntocher Road)
Yes (LA
and ScW) Road
Unnamed
watercourse and its
interaction with
storm system
upstream not
represented in ScW
model
4 Livingstone
Street
Surface water / sewer / potential fluvial
(unnamed watercourse travelling west
past Drumry Station)
Yes (LA
and ScW)
Building /
road
Unnamed
watercourse data is
missing from
existing ScW
model.
5 Melbourne
Avenue Surface water / sewer Yes (LA) Building /
road 
6 Low Crescent Surface water / sewer / fluvial Yes (LA
and ScW)
Building /
road 
7 Dumbarton
Road
Surface water / sewer / fluvial and
potential tidal influence No Building /
road 
7 Dunedin
Terrace Surface water / sewer No Building /
road 
9 Kilbowie Road Surface water / sewer
No (noted
ScW
reported
flooding
north of the
hotspot)
Building /
road 
10 Station Road Surface water Yes (LA) Road Road drainage
11 Dumbarton
Road (west) Surface water   Yes (LA) Road Road drainage

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4.2 Root Cause Analysis: Desktop
4.2.1 Second Avenue / Ramsey Street
An initial review of the SEPA surface water flood maps identified a number of residential properties within the
medium-risk surface water flooding extent (0.5% AEP; 200-year return period). However, the updated SEPA
national flood maps published in 2025 indicate a marginal reduction in the extent of predicted surface water flood
risk in this area compared to the previous mapping. Despite this, the area around Second Avenue continues to
be identified as a local flooding hotspot due to the recorded history of flooding and known drainage constraints.
Historic flooding information provided by WDC indicates that the area has experienced flooding during previous
severe rainfall events. Records show that a flash flooding incident occurred at Second Avenue on 9 June 2018,
attributed to pluvial flooding associated with a blockage or restriction within the drainage system. WDC records
also identify a flooding incident at Queen Elizabeth Gardens/Court during the same event, where flooding was
attributed to a combination of pluvial runoff and sewer flooding. These records demonstrate a history of surface
water and drainage-related flooding within the local area and provide supporting evidence of flood susceptibility,
irrespective of the differences between the previous and updated SEPA flood mapping datasets. 
Second Avenue is recorded on ScW’s external flood register and has also been reported as an internal flooding
incident. ScW believes that an uncharted sewer may be present in this location, potentially associated with the
historic Boquhanran Burn. ScW has confirmed that further investigations are being undertaken, including
additional surveys, to better understand the cause of flooding and the configuration of the local drainage network.   
Figure 4-1 - Past flooding photos from local residents    
Figure 4-2 – SEPA Flood Risk Map Comparison (200-year RP) and Flow Path Analysis (Scalgo)
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4.2.2 Western Isles Road
An initial review of the SEPA surface water flood maps identified a number of residential properties within the
medium-risk surface water flooding extent (0.5% AEP; 200-year return period). However, the updated SEPA
national flood maps published in 2025 indicate a reduced extent of predicted surface water flooding in this area,
with fewer properties identified as being at risk compared to the previous mapping. Despite this reduction, the
area remains a recognised local flooding hotspot due to the history of flooding incidents and known drainage
network constraints.
Historic flooding information provided by WDC identifies flooding at Durban Avenue during a rainfall event on 29
January 2020. The recorded source of flooding was attributed to the sewer network, with reports of sewer
surcharging at the location. The incident was reported to ScW by a resident, indicating ongoing drainage and
sewer capacity issues within the local area. These records provide evidence of historical flooding associated with
the drainage network and support the continued designation of the area as being susceptible to flood risk,
notwithstanding the reduced extent of flooding shown within the updated SEPA mapping. 
Durban Avenue is recorded on ScW external flood register and has been subject to previous investigations
relating to sewer flooding. 
Figure 4-3 – SEPA Flood Risk Map Comparison (200-year RP) and Flow Path Analysis (Scalgo)
4.2.3 Duntocher Road
An initial review of the SEPA surface water flood maps identified substantial surface water flood risk along
Duntocher Road within the medium-risk surface water flooding extent (0.5% AEP; 200-year return period). The
updated SEPA national flood maps published in 2025 show broadly similar patterns of flood risk, with only minor
changes to the mapped flood extents. While no residential properties are shown to be directly affected, primarily
due to housing being set back from the road corridor, Duntocher Road continues to be identified as an area
susceptible to surface water flooding.
Historic flooding information provided by WDC confirms a history of flooding at this location. Records describe
flash flooding at the low point on Duntocher Road, flooding associated with blocked road gullies, and overtopping
of an unnamed watercourse running adjacent to the road during heavy rainfall events. Flooding has previously
resulted in road closures, with raised manhole covers reported during the June 2018 event. WDC records from
both 2016 and 2018 indicate that flooding was related to a combination of intense rainfall, drainage exceedance,
blocked gullies and overtopping of the adjacent watercourse, highlighting the interaction between the road
drainage system and local watercourses. 
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It should be noted that two storm pipes represented within the drainage model discharge to the adjacent park
area and convey runoff from the residential catchment to the north. Furthermore, the unnamed burn referred to
within the WDC flooding records, which appears to run parallel to Duntocher Road, is not represented within the
model. SEPA mapping also identifies a spring to the north-east of the area. The connectivity between the storm
drainage system, the small burn/drain and the wider sewer network is currently uncertain and should be
investigated as part of any future detailed study to ensure the flooding mechanism is fully understood. ScW has
indicated that the burn may connect to the combined sewer network, which could have implications for flood
routing and sewer exceedance during storm events.   
Figure 4-4 – SEPA Flood Risk Map Comparison (200-year RP) and Flow Path Analysis (Scalgo)
4.2.4 Livingstone Street
An initial review of the SEPA surface water flood maps identified a number of residential properties at risk of
surface water flooding within the Livingstone Street/Linnvale area, with Livingstone Street representing the area
of greatest susceptibility. However, the updated SEPA national flood maps published in 2025 indicate a
substantially reduced extent of surface water flood risk compared to the previous mapping. Consequently, while
flood risk remains present, the number of properties now shown to be affected is significantly lower and would
no longer meet the previous hotspot screening criterion of six residential properties being at risk. Despite this
reduction in mapped risk, the area remains of interest due to its history of flooding and the potential consequences
of disruption to local access routes.
Historic flooding information provided by WDC identifies flooding at Livingstone Street during the June 2018
rainfall event. Records indicate that flooding was associated with surface water runoff from the Cripps Avenue
area, combined with drainage restrictions and blocked gullies within the local network. WDC records describe
runoff flowing towards Livingstone Street and contributing to localised flooding during intense rainfall. These
records are supported by reports from previous flood events which highlight the strategic importance of the
location, noting that flooding can render Livingstone Street impassable. As the road provides the sole vehicular
access route into Linnvale, flooding has the potential to affect residents, local businesses and emergency service
access. 
The Linnvale area, which encompasses the Livingstone Street location, has also been identified by ScW as a
High Impact location. ScW has confirmed that they are leading investigations to better understand the causes of
flooding in this area. Initial findings suggest that a historic burn located to the north of the railway may be
connected to the combined sewer network at Drumry Station, potentially contributing additional flows to an
already constrained system during rainfall events. The outcome of these investigations will be important in refining
the understanding of local flooding mechanisms and identifying appropriate long-term solutions. Despite the
reduced extent of flooding shown on the updated SEPA mapping, the recorded history of flooding, the critical
access function of Livingstone Street and the ongoing investigations by ScW indicate that flood risk remains an
important consideration within the area.
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Figure 4-5 – SEPA Flood Risk Map Comparison (200-year RP) and Flow Path Analysis (Scalgo)
4.2.5 Melbourne Avenue
An initial review of the SEPA surface water flood maps identified surface water flood risk along Melbourne
Avenue, affecting sections of the road corridor and adjacent residential properties. The updated SEPA national
flood maps published in 2025 show broadly similar flood extents, with only minor changes compared to the
previous mapping, although noted that a greater extent of Melbourne Avenue carriageway is shown to be at risk. 
Historic flooding information provided by WDC confirms a history of flooding at Melbourne Avenue associated
with both surface water and sewer-related drainage issues. Records from 2015 and 2018 indicate flooding linked
to blocked road drainage and gullies, with heavy rainfall resulting in exceedance of the local drainage system. In
particular, WDC records identify the old cast-iron vented manhole located outside 55 Melbourne Avenue as a
recurring flooding location. During periods of intense rainfall, water is reported to surcharge through the vented
manhole cover at the low point of the street, resulting in localised flooding. WDC records also note incidents
where road drainage became blocked, contributing to the accumulation of surface water on the carriageway. 
The historical flooding records indicate that flooding at Melbourne Avenue is primarily driven by local drainage
constraints and sewer interactions rather than overland flow from a wider catchment. The recurring nature of
incidents associated with the manhole outside 55 Melbourne Avenue suggests an ongoing capacity or surcharge
issue within the drainage network. 
Figure 4-6 – SEPA Flood Risk Map Comparison (200-year RP) and Flow Path Analysis (Scalgo)
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4.2.6 Low Crescent
An initial review of the SEPA surface water flood maps identified a number of residential properties at risk of
flooding within the Low Crescent area. However, the updated SEPA national flood maps published in 2025
indicate a significant reduction in the extent of predicted surface water flooding compared to the previous
mapping, with substantially fewer properties now shown to be affected. Notwithstanding this reduction in mapped
surface water risk, the location remains of interest due to its documented flooding history and the presence of
fluvial flood risk. SEPA mapping continues to identify areas susceptible to fluvial flooding, including during higher-
probability events, with potential impacts to residential properties and sections of the local road network.
Historic flooding information provided by WDC indicates that flooding at Low Crescent has been attributed to a
combination of pluvial and sewer-related mechanisms. Records from the December 2015 event identify a
capacity issue within the drainage system, suggesting that flooding results from interactions between surface
water runoff and the sewer network during periods of intense rainfall. These records demonstrate that, although
the updated SEPA mapping shows a considerably reduced surface water flood extent, local drainage constraints
and sewer exceedance influence flood risk at the site. 
Figure 4-7 – SEPA Flood Risk Map Comparison (200-year RP) and Flow Path Analysis (Scalgo)
4.2.7 Dumbarton Road
During the first iteration of the SWMP, SEPA surface water flood mapping identified a significant area of flood
risk at this location, with potential impacts to residential and commercial properties, a school and the A814
Dumbarton Road. However, the updated SEPA Flood Maps published in 2025 indicate a substantial reduction in
predicted surface water flood risk, with only limited areas of flooding now identified and minimal risk to properties.
Based on the previous hotspot screening criterion of six or more residential properties being at risk, this location
would no longer qualify as a flood hotspot under the updated mapping.
No historic flooding incidents have been identified for this location from records provided by WDC, nor were any
relevant flood reports identified through the review of available media sources. The absence of recorded flooding
is consistent with the significantly reduced level of risk shown in the updated SEPA mapping.
A review of overland flow pathways using Scalgo suggests that the more extensive flooding predicted by the
earlier SEPA mapping may have been influenced by limitations within the underlying digital terrain model. The
analysis indicates that flow paths are routed along the Duntocher Burn corridor from the north and appear to be
obstructed where the watercourse passes beneath the A814 Dumbarton Road. In reality, the burn is conveyed
beneath the road via a bridge or culvert structure that is not fully represented within the terrain data. A similar
issue occurs further downstream where the Duntocher Burn passes beneath the Forth and Clyde Canal. These
crossings can create "false blockages" within terrain models, resulting in artificial ponding and exaggerated flood
extents. Observations from the site visit support this interpretation and are consistent with the notable reduction
in flood risk shown by the updated 2025 SEPA Flood Maps.
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Figure 4-8 illustrates the flood risk identified by the SEPA surface water flood maps used during the initial iteration
of the study, with a comparison revised flood extents presented within the 2025 SEPA Flood Maps. The
comparison demonstrates the significant reduction in predicted risk and supports the conclusion that this location
is no longer considered a priority hotspot based on the current mapping evidence. 
Figure 4-8 – SEPA Flood Risk Map Comparison (200-year RP) and Flow Path Analysis (Scalgo)
4.2.8 Dunedin Terrace
An initial review of the SEPA surface water flood maps identified several residential properties at risk of flooding
within the medium-risk surface water flooding extent (0.5% AEP; 200-year return period). However, the updated
SEPA Flood Maps published in 2025 indicate a notable reduction in the extent of predicted surface water flooding
at this location, with fewer properties shown to be affected and only limited areas of flooding depth exceeding 0.3
m. As a result, the location would not necessarily meet the previous hotspot screening criterion of six or more
residential properties being at risk and may not have been classified as a flood hotspot based on the updated
mapping.
No historic flooding incidents have been identified for this location from records provided by WDC, and no relevant
flooding reports were identified through the review of available media sources. The absence of recorded flooding
is consistent with the reduced level of risk indicated by the updated SEPA surface water flood maps. 
While some residual surface water flood risk remains evident within the updated mapping, the reduction in both
the extent and severity of predicted flooding suggests that the location is less vulnerable than previously
indicated. Consequently, although the area should continue to be considered within any wider catchment-scale
assessment, the available evidence does not currently support its identification as a priority flood hotspot.
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Figure 4-9 – SEPA Flood Risk Map Comparison (200-year RP) and Flow Path Analysis (Scalgo)
4.2.9 Kilbowie Road
An initial review of the SEPA surface water flood maps identified substantial surface water flood risk in the vicinity
of Clyde Shopping Centre, with a number of surrounding commercial and residential properties shown to be
susceptible to flooding within the medium-risk surface water flooding extent (0.5% AEP; 200-year return period).
The updated SEPA Flood Maps published in 2025 indicate a modest reduction in the extent of predicted flooding
compared to the previous dataset. However, significant areas of surface water flood risk remain, and the location
continues to be identified as an area of notable flood susceptibility within the catchment.
No historic flooding incidents have been identified for this location from records provided by WDC. However, ScW
has identified a location on its flood register at Cambridge Avenue, immediately to the north of the hotspot,
indicating a history of drainage and sewer-related flooding issues within the wider area. The proximity of this
recorded flooding location suggests that local drainage constraints may influence flood risk in the vicinity of the
shopping centre. 
Although no flooding records have been identified from WDC, media reports provide evidence of flooding within
the area. In August 2021, reports described flooding on Kilbowie Road near Clyde Shopping Centre, with sections
of the road reported to be underwater following heavy rainfall. The incident required attendance by emergency
services, with fire crews rescuing a vehicle from a deep flooded area adjacent to the shopping centre. These
reports demonstrate that significant surface water accumulation can occur locally during intense rainfall events,
affecting both road users and access through the area. 
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Figure 4-10 – SEPA Flood Risk Map Comparison and Flow Path Analysis (Scalgo)
4.2.10 Station Road
An initial review of the SEPA surface water flood maps identified substantial surface water flood risk at the low
point on Station Road, with flooding largely confined to the road corridor and adjacent low-lying areas. The
updated SEPA Flood Maps published in 2025 show broadly similar flood extents and depths to the previous
dataset, indicating that there has been little change in the understanding of flood risk at this location. Station
Road therefore continues to be identified as an area susceptible to flooding, particularly during intense rainfall
events.
Historic flooding information provided by WDC confirms a history of flooding at this location. Records from
December 2015 describe deep flooding at the low point on Station Road associated with a combination of pluvial
and fluvial flooding, including overtopping of an unnamed burn. Subsequent flooding during February 2020 was
attributed to debris and runoff from adjacent agricultural land, which blocked road gullies and reduced the
effectiveness of the highway drainage system. Both incidents resulted in road closures, highlighting the
susceptibility of Station Road to flooding from multiple sources and the importance of maintaining drainage
infrastructure. 
The WDC records indicate that flooding at Station Road is influenced by a combination of overland runoff,
interactions with the adjacent watercourse and blockages within the road drainage network. The contribution of
runoff from neighbouring agricultural land suggests that catchment processes outside the urban area also play a
role in flood generation at this location. The upstream natural watershed is large and is likely to play a key role in
terms of rural runoff reaching this site.
During subsequent engagement, WDC highlighted that flooding at Station Road can have a disproportionately
large impact on the surrounding area despite the limited number of properties directly affected. Flooding at the
low point can lead to drivers attempting to pass through deep water, creating a safety risk, whilst closures of the
road can affect access to nearby businesses and disrupt the slip road connection to the A82. As a result, the
significance of this location is linked not only to the flood hazard itself but also to the wider transport and access
implications associated with flooding events.
Social media reports of previous flood events provide further evidence of the site's susceptibility to flooding, with
Station Road reported to have been closed on several occasions due to floodwater. These reports are consistent
with the historical records held by WDC and reinforce the importance of the route as a potential point of disruption
during severe weather events.

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Figure 4-11 – SEPA Flood Risk Map Comparison and Flow Path Analysis (Scalgo)
4.3 Root Cause Analysis: Modelling
Different stakeholder requirements generate a need for different types of models, varying from small, localized
studies, to large strategic catchment wide studies. Models can include representation of foul/combined sewer
networks, storm sewer systems, watercourses, overland flow pathways, and/or all these elements integrated
together.
For a SWMP, how runoff is represented in the model is key. Runoff modelling defines how much of the rainfall
falling on a catchment becomes runoff and how quickly this enters the drainage system, should capacity allow.
For this study, to build a clearer understanding of root causes of flooding within Clydebank, the model assessment
was broken down into three phases:
 1D sewer network modelling: the sewer network model, as received from ScW, representing predicted
out-of-sewer flooding. Subcatchments are directed to specific manholes so as there is no surface, where
flow runoff is directed if it cannot enter the system is not modelled.
 2D pluvial modelling: representing flows over the surface, with gully losses represented. No interaction
with the sewer network.
 1D – 2D integrated modelling: the sewer network, with rainfall applied to the mesh and gullies.
Represents the combined impact of pluvial and out-of-sewer flooding/sewer capacity constraints, for a
more accurate representation of the true extent of flooding. 
4.3.1 1D Sewer Network Modelling
The 1D hydraulic model obtained by ScW to cover the hotspots in the Clydebank area was DOA000333 Dalmuir
Current v24, which was last committed on 18/11/2024, base scenario. This was used to obtain an understanding
of the predicted sewer performance and flooding within the hotspots.
Water companies typically use InfoWorks models to represent the below ground (engineered) system. Prediction
of flow within pipes is based on runoff from predefined surface areas draining to “nodes” (which are typically
manholes). Calculations are made at each node, determining flow arriving, continuing downstream, and water
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levels in the nodes. Flood volumes and depths is predicted at ground level, giving the user an estimation of
flooding likely to occur at each node – giving an idea of what might be impacted by flood water nearby.
In 1D models, predefined surface areas are set in subcatchments. Subcatchments make up the total catchment
of a drainage network but serve to add detail on where water will enter the drainage system on a local level. Each
subcatchment calculates runoff in response to rainfall depending based on the proportion of runoff surfaces
applied. In other words, the speed and volume of runoff is dependent on how much impermeable (roads and
roofs) or permeable (gardens / soils) the subcatchment covers. Highly impermeable subcatchments generate
faster responses with less infiltration losses, while highly permeable subcatchments generate slower responses
with more infiltration losses. 
Figure 4-12 shows a subcatchment in a 1D hydraulic urban drainage model. The green boundary indicates what
area the subcatchment is draining (roofs, road, and some garden space), and the green arrow indicates where
it’s draining to. The red lines are pipes, and red dots are manholes (or nodes). The figure demonstrates how
subcatchments cover the total catchment area, like a jigsaw puzzle. 
Figure 4-12 - 1D hydraulic model visual representation
These models are useful for wastewater studies, whereby the performance of the piped system is the primary
focus of assessment. Water companies invest to build these models and undertake flow verification to ensure
high confidence in flow predictions in their underground network (for which they are responsible). However, a
fundamental limitation of 1D drainage models is they assume runoff either enters the engineered piped system
directly or is lost it (i.e. it never reaches the system) – which can happen for a whole manner of reasons (e.g.
such as capacity of gullies, pooling on the surface, walls blocking flow paths). For this reason, 1D models are not
appropriate for assessing pluvial flooding and flow paths, as per required for a SWMP.
While the primary goal of the SWMP is to address surface water flooding, it is important to understand where
sewer flooding is likely to occur and consider how this may impact surface water solutions. Simulations were run
for the existing 1D models for 1 in 30-year return period event and 1 in 200-year return period event and outlined
in the following section.
The following section provides a summary of the predicted flooding from the piped network for the high priority
hotspots within Clydebank.

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4.3.1.1 Second Avenue / Ramsay Street 
In the 1 in 30-year return period event, the sewer network conveys flows towards the topographic low point within
the hotspot, where approximately 1,500m³ of out-of-sewer flooding is predicted from combined manhole
NS48718301. This represents significant sewer flooding and indicates that the existing sewer network is unable
to contain and convey flows during the event. The volume of flooding predicted from a single manhole suggests
that sewer network exceedance is a primary flooding mechanism at this location and reflects a significant capacity
constraint within the combined sewer system. Figure 4-13 illustrates predicted flooding from the 1D model. 
Figure 4-13 - Map of flooded nodes in the 1D hydraulic model during the 30-year 60 minute event

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4.3.1.2 Western Isles Road 
Several combined sewer manholes along Durban Avenue are predicted to surcharge during the 1 in 30-year
return period event (refer to Figure 4-14). Manhole NS47716601 is predicted to experience the greatest flood
volume, at approximately 151 m³. This represents a significant volume of out-of-sewer flooding and indicates that
the local combined sewer network is unable to contain and convey flows during the event. The modelling therefore
suggests that sewer network exceedance is a primary contributor to flooding at this location, highlighting capacity
constraints within the existing drainage system.  
Figure 4-14 - Map of flooded nodes in the 1D hydraulic model during the 30-year 60 minute event

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4.3.1.3 Duntocher Road
The 1D modelling indicates that four combined sewer manholes are predicted to surcharge by more than 100 m³
during the 1 in 30-year return period event, with NS49726001 and NS49725003 each predicted to flood by more
than 500 m³ (Figure 4-15). These manholes are located within, or immediately upstream of, the low point on
Duntocher Road and collectively represent a substantial volume of out-of-sewer flooding. The modelling indicates
that the combined sewer network is unable to contain and convey flows during the event, resulting in significant
sewer flooding at this location. The magnitude of the predicted flood volumes suggests that sewer network
exceedance is a primary flooding mechanism at Duntocher Road and highlights a significant capacity constraint
within the existing drainage system.
However, these results should be considered alongside the limitations identified in the desktop root cause
analysis. In particular, the unnamed watercourse referenced within the WDC flood records is not represented
within the hydraulic model, despite evidence that it may interact with the combined sewer network. ScW is
currently investigating the potential connectivity between this watercourse, the sewer system and the wider
drainage network. In addition, the interaction between the storm drainage outfalls, adjacent parkland and the
unnamed watercourse remains uncertain. Consequently, whilst the modelling indicates that sewer flooding is a
significant contributor to flood risk at this location, the results should be treated with caution pending the outcome
of the ongoing ScW investigations and any subsequent refinement of the flooding mechanisms. 
Figure 4-15 - Map of flooded nodes in the 1D hydraulic model during the 30-year 60 minute event

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4.3.1.4 Livingstone Street
Several combined sewer manholes along Livingstone Street are predicted to surcharge during the 1 in 30-year
return period event (refer to Figure 4-16). In particular, manholes NS50706301 and NS50705302 are predicted
to flood by approximately 110 m³ and 187 m³ respectively. These represent significant volumes of out-of-sewer
flooding and indicate that the local combined sewer network is unable to contain and convey flows during the
event. The modelling therefore suggests that sewer network exceedance is a primary contributor to flooding
within the Livingstone Street area, highlighting capacity constraints within the existing drainage system.
However, the limitations and uncertainties identified within the desktop root cause analysis should be taken into
account when interpreting these results. In particular, the ongoing ScW investigations into the potential interaction
between historic drainage features and the combined sewer network may provide additional information
regarding the flooding mechanisms operating within the area. Consequently, the model results should be treated
with a degree of caution pending the outcome of these investigations and any subsequent updates to the
understanding of flood risk at this location.  
Figure 4-16 - Map of flooded nodes in the 1D hydraulic model during the 30-year 60 minute event

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4.3.1.5 Melbourne Avenue
Several sewer manholes along Melbourne Avenue are predicted to surcharge during the 1 in 30-year return
period event. Manhole NS47728501 has the highest predicted flood volume at approximately 345 m³, whilst
NS47728502 and NS47727402 are predicted to flood by approximately 135 m³ and 62 m³ respectively. These
represent significant volumes of out-of-sewer flooding and indicate that the local combined sewer network is
unable to contain and convey flows during the event. The resulting exceedance flows would discharge onto the
surface and follow the road gradient towards the low point on Melbourne Avenue, contributing to flooding within
the hotspot. The modelling therefore suggests that sewer network exceedance is a significant contributor to
flooding at this location and highlights local capacity constraints within the drainage system.
The model results are consistent with the historical flood information provided by WDC, which identifies recurring
flooding associated with surcharge from the vented manhole outside 55 Melbourne Avenue, as well as incidents
linked to blocked road gullies and drainage infrastructure. These records support the conclusion that both sewer
capacity limitations and local drainage constraints influence flood risk within the area.  
Figure 4-17 - Map of flooded nodes in the 1D hydraulic model during the 30-year 60 minute event

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4.3.1.6 Low Crescent
Numerous combined sewer manholes within the Low Crescent hotspot are predicted to surcharge during both
the 1 in 30-year RP event. The predicted out-of-sewer flood volumes are substantial, with the largest flood
volumes occurring at NS50696702 (564m³), NS50697802 (234m³), NS50695803 (199m³) and NS51690601
(192m³) (Figure 4-18). These results indicate that the combined sewer network is unable to contain and convey
flows during storm events, resulting in significant sewer flooding within the hotspot. The magnitude and
distribution of the predicted flood volumes suggest that sewer network exceedance is a significant contributor to
the overall flooding mechanism and highlight capacity constraints within the existing drainage system.
The desktop assessment also identified that flood risk within the area is influenced by a combination of surface
water and fluvial processes, with the updated SEPA Flood Maps continuing to indicate areas of fluvial flood risk. 
Figure 4-18 - Map of flooded nodes in the 1D hydraulic model during the 30-year 60 minute event

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4.3.1.7 Dumbarton Road
Several combined sewer manholes along Dumbarton Road and Swindon Street are predicted to surcharge during
the 1 in 30-year return period event (refer to Figure 4-19). In particular, manholes NS48712201 and NS48713303
are predicted to flood by approximately 133 m³ and 184 m³ respectively. These represent significant volumes of
out-of-sewer flooding and indicate that the local combined sewer network is unable to contain and convey flows
during the event. The modelling therefore suggests that sewer network exceedance is a significant source of
flooding within the area and highlights local capacity constraints within the existing drainage system. 
Figure 4-19 - Map of flooded nodes in the 1D hydraulic model during the 30-year 60 minute event

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4.3.1.8 Dunedin Terrace
Several combined sewer manholes along Dunedin Terrace and North Douglas Street are predicted to surcharge
during the 1 in 30-year return period event (refer to Figure 4-20). The predicted out-of-sewer flood volumes are
generally less than 100 m³, indicating a comparatively lower level of sewer flooding than at a number of the other
assessed hotspots. Nevertheless, the results demonstrate that the local combined sewer network is unable to
fully contain and convey flows during the event, resulting in localised sewer exceedance within the area. 
Figure 4-20 - Map of flooded nodes in the 1D hydraulic model during the 30-year 60 minute event

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4.3.1.9 Kilbowie Road
Sewer flooding is predicted at the junction of Kilbowie Road and Second Avenue, with approximately 250 m³ of
out-of-sewer flooding predicted during the 1 in 30-year return period event. Once discharged from the sewer
network, these flows are likely to be conveyed along the road corridor towards lower ground on Kilbowie Road.
The modelling therefore indicates that sewer network exceedance is a significant contributor to flooding within
this hotspot and reflects capacity constraints within the local combined sewer system. 
Figure 4-21 - Map of flooded nodes in the 1D hydraulic model during the 30-year 60 minute event 
4.3.1.10 Station Road
The Station Road hotspot was not covered by the 1D sewer model, therefore, predicted out of sewer flooding
could not be analysed.
4.3.1.11 Dumbarton Road (west) 
The Dumbarton Road (west) hotspot was not covered by the 1D sewer model, therefore, predicted out of sewer
flooding could not be analysed.

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4.3.2 Pluvial Only Flood Modelling
A 2D pluvial model was developed to understand overland flow routes within the catchment when rainfall was
directly applied to the model surface (also known as a rainfall-to-mesh model). Scottish Publicly Available LiDAR
data5 of 0.5m resolution was used to create a Digital Terrain Model (DTM), to represent the topography of the
study area. 
Mastermap GIS data was imported into the model to explicitly represent building and roads, which can influence
flow paths by obstructing of channelling water. These modifications replicate the impact of raised and dropped
kerbs, which can influence the direction and destination of water on the surface. Buildings with a considerable
roof area (>10 m2) were modelled with 10% porosity to replicate the impact of water moving through the property,
either through ventilation in a building’s foundation or through the property itself once the threshold is breached.
Buildings with roof area <10 m2 (e.g. garden sheds) were modelled simplistically as 200 mm stubs.
This model was set up to represent how the sewer network “should-be”. In other words, in optimal condition (e.g.
no blockages, sediment), and capable of coping with a 30-year return period storm event. This means that outputs
from this model highlight what surface water flooding would remain if the existing drainage system was working
optimally. 
The following sections summarise the findings of this assessment, illustrating the predicted extents when only
pluvial flooding is considered. It should be noted that depths below 150mm have been filtered out, so that depths
that would be considered to cause disruption to infrastructure and property flooding are visualised.
4.3.2.1 Second Avenue / Ramsay Street
When the sewer network is not considered, there is still significant flooding that can be attributed to pluvial causes
at this hotspot, with properties impacted with likely internal flooding, and significant depths predicted in the road.
Most of the surface water flooding predicted at Second Avenue / Ramsay Street is because of overland flow
paths. The residential streets Park Road and Duntocher Road are key surface water conveyance paths into the
hotspot. Park Road has a relatively steep fall directly to the low point of the hotspot, which lies between St
Stephens Church and St Stephens Primary School. Therefore, most of the surface water routes towards this area
where the drainage system in place is not effective enough to drain it and/or convey it downstream. Therefore,
surface water spreads out overland. 
5Scottish Remote Sensing Portal. Available at: https://remotesensingdata.gov.scot/data#/map

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Figure 4-22 - Predicted pluvial only flood extents at the 1 in 30-year return period event
4.3.2.2 Western Isles Road
Most of the surface water flooding experienced at the Western Isles Road hotspot is due to overland flow paths.
Western Isles Road, Delhi Avenue and Durban Avenue are key surface water conveyance paths. Western Isles
Road falls the most steeply towards the hotspot and has the highest flow contribution. The model predicts that
most pluvial flooding is contained within the road for this event, and does not impact properties. 
Figure 4-23 - Predicted pluvial only flood extents at the 1 in 30-year return period event

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4.3.2.3 Duntocher Road
When pluvial flooding is assessed in isolation, the model predicts that the impact is not significant, although does
cause disruption to the road. Most of this surface water originates from Briar Drive and Kilbowie Road from the
southeast. Additionally, some surface water comes from the high point on Duntocher Road from the west. As
noted though, at this hotspot, complex interactions and data gaps mean that the true mechanism of flooding may
not be understood. 
Figure 4-24 - Predicted pluvial only flood extents at the 1 in 30-year return period event

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4.3.2.4 Livingstone Street
When considering pluvial flooding in isolation, the modelling predicts limited and localised areas of surface water
ponding, primarily within a number of cul-de-sac areas located within the hotspot. The predicted flood extents
and depths suggest some disruption to the local road network; however, the flooding is generally contained and
does not indicate widespread surface water flood risk. These results are consistent with the updated 2025 SEPA
Flood Maps, which show a similarly limited extent of surface water flooding within the area. 
Figure 4-25 - Predicted pluvial only flood extents at the 1 in 30-year return period event

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4.3.2.5 Melbourne Avenue
The pluvial-only modelling indicates that surface water runoff accumulates at the low point on Melbourne Avenue,
with the majority of runoff conveyed from higher ground further north along the road. Whilst the predicted flooding
is generally localised, model results indicate that flood depths are sufficient to result in impacts to the carriageway
and disruption to road users during the design event. This suggests that surface water runoff contributes to flood
risk at the location, particularly where flows concentrate at the low point on Melbourne Avenue. 
Figure 4-26 - Predicted pluvial only flood extents at the 1 in 30-year return period event

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4.3.2.6 Low Crescent
The pluvial-only modelling indicates localised surface water ponding at the junction of Abbott Crescent and North
Elgin Street, with runoff primarily conveyed from the higher ground around Johnson Avenue before accumulating
at the local topographic low point. Additional isolated ponding is also predicted on Sinclair Street. The predicted
flooding is generally confined to the road network and surrounding low spots, with depths indicating potential
disruption to local access routes during the design event. These results are consistent with the updated 2025
SEPA Flood Maps, which show residual surface water flood risk concentrated around the same low-lying areas
rather than widespread flooding across the hotspot. 
Figure 4-27 - Predicted pluvial only flood extents at the 1 in 30-year return period event

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4.3.2.7 Dumbarton Road
The pluvial-only modelling indicates localised surface water ponding on Dumbarton Road in the vicinity of the
junction with French Street during the 1 in 30-year return period event. The predicted flooding is largely confined
to the road corridor, with depths suggesting some disruption to road users but limited wider impacts. These results
are broadly consistent with the updated 2025 SEPA Flood Maps, which indicate a substantially reduced extent
of surface water flood risk compared to the previous mapping and support the conclusion that pluvial flood risk
at this location is relatively limited. 
Figure 4-28 - Predicted pluvial only flood extents at the 1 in 30-year return period event

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4.3.2.8 Dunedin Terrace
The pluvial-only modelling indicates localised surface water ponding along North Douglas Street and Dunedin
Terrace during the 1 in 30-year return period event. The predicted flooding is generally shallow and confined to
isolated low points within the road network, with limited potential for wider impacts. These results are consistent
with the updated 2025 SEPA Flood Maps, which show a reduced extent of surface water flood risk at this location
and support the conclusion that pluvial flooding is relatively limited compared to that indicated by the previous
mapping. 
Figure 4-29 - Predicted pluvial only flood extents at the 1 in 30-year return period event

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4.3.2.9 Kilbowie Road
The pluvial-only modelling indicates notable surface water ponding on Coldstream Road during the 1 in 30-year
return period event, with runoff conveyed from higher ground to the east. Additional isolated areas of ponding are
also predicted within the Clyde Shopping Centre area. The model results indicate flood depths that could result
in disruption to the local road network and access routes during intense rainfall events. These findings are broadly
consistent with both the previous and updated 2025 SEPA Flood Maps, which continue to identify this location
as being susceptible to surface water flooding, albeit with a slightly reduced extent compared to the previous
mapping. 
Figure 4-30 - Predicted pluvial only flood extents at the 1 in 30-year return period event
4.3.2.10 Station Road
Due to limitations on the extent of network model, this hotspot was not assessed in the pluvial only model.
4.3.2.11 Dumbarton Road (west)
Due to limitations on the extent of network model, this hotspot was not assessed in the pluvial only model.

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4.3.3 Integrated 1D - 2D Runoff Model 
The 1D sewer network elements from the ScW Dalmuir hydraulic model were integrated with the 2D pluvial model
to improve understanding of the interaction between the underground drainage system (e.g. sewers, culverts and
manholes) and overland surface water flow pathways. This integrated modelling approach enabled assessment
of the exchange of flows between the sewer network and the ground surface during storm events, helping to
identify the dominant flood mechanisms within each hotspot.
The integrated model output provides a representation of the combined impact of pluvial flooding and sewer
exceedance, allowing areas affected by both surface water runoff and surcharging drainage infrastructure to be
identified. This supports a more comprehensive understanding of flood risk than consideration of either source in
isolation and assists in determining the relative contribution of surface water and sewer network constraints to
observed flooding at each location.
The following sections summarise the findings of the integrated modelling assessment for each hotspot and
compare the predicted flooding mechanisms and extents against the SEPA surface water flood maps. This
comparison has been used to identify areas of agreement and discrepancy between the datasets, improve
confidence in the understanding of flood risk. Please note that this modelling assessment was undertaken prior
to the release of the 2025 SEPA flood maps and the visual comparison is to the previous dataset.
4.3.3.1 Second Avenue / Ramsay Street
This hotspot is predicted to flood due to a combination of surface water runoff and sewer exceedance. The
integrated 1D-2D model indicates that flooding results from the combined effects of pluvial runoff and surcharging
within the sewer network. The predicted flood extents from the integrated modelling align closely with the updated
SEPA Flood Maps, providing confidence in the representation of flood risk at this location.
Model results show that the principal surface water flow pathways originate from Park Road and Duntocher Road
to the north, with runoff conveyed rapidly downslope towards the low point located between St Stephen’s Church
and St Stephen’s Primary School. As water accumulates within this topographic depression, the capacity of the
local sewer network is exceeded, limiting its ability to accept and convey incoming flows downstream.
Consequently, a significant proportion of the runoff remains on the surface, contributing to the observed flood
extents.
The modelling indicates that sewer flooding is a significant component of the overall flood mechanism, with sewer
surcharge contributing to flooding within the area. Evidence gathered during the site visit supports this finding,
with the presence of toilet paper around roadside gullies suggesting that sewer surcharge has occurred
historically. Model results further demonstrate that both surface water flooding and sewer exceedance occur
during the more frequent 1 in 1-year return period event, indicating that drainage system constraints are present
even during relatively modest rainfall events.

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Figure 4-31 – Integrated model predicted flooding compared to SEPA pluvial flood maps (200 year RP)
4.3.3.2 Western Isles Road
The integrated modelling indicates that flooding at the Western Isles Road hotspot is influenced by a combination
of overland flow and sewer network exceedance. Surface water runoff is primarily conveyed along Western Isles
Road, Delhi Avenue and Durban Avenue, with Western Isles Road contributing the greatest proportion of runoff
due to its steeper gradient towards the hotspot. The relatively flat topography within the low-lying area around
Durban Avenue limits the ability of surface water to drain effectively, resulting in localised ponding.
During the initial SWMP assessment, the integrated modelling predicted a considerably smaller flood extent than
that shown by the SEPA surface water flood maps available at the time. However, the updated 2025 SEPA Flood
Maps indicate a reduced extent of surface water flood risk and are now much more closely aligned with the
integrated model predictions. Both datasets identify flooding concentrated around the low-lying areas of the
hotspot, increasing confidence in the current understanding of flood risk at this location.
The modelling also indicates that several gullies and combined sewer manholes within and upstream of the
hotspot are predicted to surcharge during heavy rainfall events, demonstrating that the combined sewer network
is unable to effectively accommodate flows. Consequently, whilst the updated SEPA flood maps continue to
identify the location as being susceptible to flooding, the modelling suggests that the flooding mechanism is not
solely driven by overland surface water runoff. Instead, sewer network exceedance is considered to be a
significant contributor to the observed flooding, with interactions between the surface and below-ground drainage
systems influencing the overall flood risk at this location.

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Figure 4-32 - Integrated model predicted flooding compared to SEPA pluvial flood maps (200 year RP)

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4.3.3.3 Duntocher Road
The integrated modelling indicates that flooding at Duntocher Road is driven by a combination of overland flow
and sewer network exceedance. Surface water runoff is conveyed towards the low point on Duntocher Road from
Briar Drive and Kilbowie Road to the south-east, together with additional runoff from higher ground to the west
along Duntocher Road.
During the initial SWMP assessment, the integrated modelling results showed good agreement with the SEPA
surface water flood maps available at the time. Following publication of the 2025 SEPA Flood Maps, this
agreement remains evident, with the updated mapping continuing to identify Duntocher Road as a significant
flood risk location. The close alignment between the integrated modelling outputs, the updated SEPA Flood Maps
and historical flooding records provided by WDC provides a high level of confidence in the understanding of flood
risk at this location. In particular, the modelling supports historical reports of flooding at the low point on Duntocher
Road, including road flooding, disruption to the local road network and flooding associated with the adjacent
drainage system.
The modelling indicates that sewer exceedance is a significant contributor to the overall flood mechanism, with
drainage system capacity constraints resulting in surcharging and surface flooding during relatively frequent
rainfall events. This suggests that sewer flooding is a key driver of flood risk at this location, acting in combination
with overland runoff conveyed towards the local topographic low point.
It should be noted that the unnamed watercourse referred to in the WDC flooding records is not represented
within the hydraulic model. As discussed in Section 4.2, ScW considers that this watercourse may connect to the
combined sewer network and is currently investigating its connectivity and influence on flooding within the area.
Consequently, whilst the available evidence indicates that sewer flooding is a key contributor to flood risk at
Duntocher Road, the results should be interpreted with caution and reviewed in light of the findings from the
ongoing ScW investigations. 
Figure 4-33 - Integrated model predicted flooding compared to SEPA pluvial flood maps (200-year RP)

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4.3.3.4 Livingstone Street
The integrated modelling indicates that flooding within the Livingstone Street hotspot is influenced by a
combination of surface water runoff and sewer network exceedance, with flooding primarily concentrated on
Livingstone Street and extending to adjacent roads including Shinwell Avenue and Silkin Avenue. The modelling
suggests that the dominant flooding mechanism is sewer exceedance, with several gullies and manholes
connected to the combined sewer network predicted to surcharge and discharge flows onto the surface during
storm events. As a result, sewer flooding is considered to make a significant contribution to the observed flood
extents.
During the initial SWMP assessment, the integrated modelling predicted a substantially smaller flood extent than
that shown by the SEPA surface water flood maps available at the time. However, the updated 2025 SEPA Flood
Maps indicate a significantly reduced extent of surface water flood risk and are now much more closely aligned
with the integrated model predictions. This improved agreement between the modelling and the updated SEPA
mapping increases confidence that flood risk at Livingstone Street is more localised than previously indicated
and that widespread pluvial flooding is unlikely to be the principal driver of flooding within the area.
The modelling results are also consistent with the historical flooding records and information provided by ScW,
which has identified the Linnvale area as a High Impact location. Together, the available evidence suggests that
sewer network performance is a key contributor to flood risk at this location. However, as discussed in the desktop
root cause analysis, ScW is currently undertaking investigations into the potential influence of historic
watercourses and their interaction with the combined sewer network. Consequently, whilst sewer flooding is
currently considered to be the primary flooding mechanism at Livingstone Street, the modelling results should be
interpreted with caution and reviewed following completion of the ongoing ScW investigations. 
Figure 4-34 - Integrated model predicted flooding compared to SEPA pluvial flood maps (200-year RP)

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4.3.3.5 Melbourne Avenue
The integrated modelling indicates that flooding at the Melbourne Avenue hotspot is influenced by a combination
of surface water runoff and sewer network exceedance. Surface water runoff is conveyed from higher ground to
the north along Melbourne Avenue before accumulating at the local topographic low point. The modelling also
predicts surcharge from a number of combined sewer manholes and gullies, indicating that sewer flooding
contributes significantly to the observed flood extents.
The integrated model results are consistent with the historical flooding information provided by WDC, which
identifies repeated flooding associated with the vented manhole outside 55 Melbourne Avenue, together with
reports of blocked highway drainage and gully infrastructure. This evidence supports the conclusion that flooding
at the site is influenced by both local drainage constraints and sewer network performance.
The predicted flood extents also show reasonable agreement with both the original and updated 2025 SEPA
Flood Maps, which continue to identify Melbourne Avenue as an area susceptible to flooding. Collectively, the
model results, flood records and SEPA mapping indicate that flooding is concentrated around the low point on
Melbourne Avenue and is driven by the interaction between overland runoff and sewer surcharge.
Consequently, the available evidence suggests that sewer network exceedance is a significant contributor to
flood risk at this location, with surface water runoff acting to exacerbate flooding once the capacity of the local
drainage system is exceeded. However, the results should be interpreted alongside the historical flood evidence
and wider understanding of local drainage conditions when considering future mitigation measures. 
Figure 4-35 - Integrated model predicted flooding compared to SEPA pluvial flood maps (200-year RP)

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4.3.3.6 Low Crescent
The integrated modelling indicates that flooding within the Low Crescent hotspot is influenced by a combination
of surface water runoff and sewer network exceedance. Flooding is concentrated around local topographic low
points, particularly in the vicinity of Abbott Crescent, North Elgin Street and Sinclair Street, with runoff conveyed
from higher ground including the Johnson Avenue area before accumulating within the hotspot.
During the initial SWMP assessment, the integrated modelling showed a smaller extent of flooding than that
indicated by the SEPA surface water flood maps available at the time. However, the updated 2025 SEPA Flood
Maps indicate a substantially reduced extent of surface water flood risk and are now more closely aligned with
the integrated model predictions. Both datasets suggest that flooding is generally localised and focused around
the principal low points within the hotspot rather than being widespread across the wider area.
The available evidence indicates that sewer network performance is a significant contributor to flood risk, with
sewer capacity constraints likely acting in combination with localised surface water ponding.
In addition, the updated SEPA Flood Maps continue to identify areas of fluvial flood risk within and around the
hotspot. Whilst the integrated model does not explicitly represent fluvial flooding mechanisms, the mapped fluvial
flood extents indicate that flooding within the area may be influenced by interactions between surface water,
sewer and fluvial processes.
Consequently, whilst the updated SEPA mapping indicates a reduced level of surface water flood risk compared
to the previous dataset, the combined evidence from hydraulic modelling, historical flooding records, sewer
flooding records and SEPA flood mapping suggests that flood risk at Low Crescent is influenced by the interaction
of surface water, sewer and fluvial mechanisms, with sewer flooding remaining a significant contributor to the
overall risk. 
Figure 4-36 - Integrated model predicted flooding compared to SEPA pluvial flood maps (200 year RP)

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4.3.3.7 Dumbarton Road
The integrated modelling indicates that flooding on Dumbarton Road is limited and primarily confined to localised
areas around the low point near the junction with French Street. The model predicts only shallow flooding in
isolated locations, with the majority of runoff conveyed towards the adjacent watercourse. The results suggest
that neither pluvial runoff nor sewer network exceedance are significant flood mechanisms at this location and
that impacts to properties and infrastructure are likely to be limited.
During the initial SWMP assessment, there was a notable disparity between the integrated model results and the
SEPA surface water flood maps available at the time, which identified a much greater extent of flood risk affecting
surrounding properties, the school and sections of the A814. As discussed in Section 4.2, subsequent review
indicated that the original SEPA mapping was likely influenced by limitations within the underlying terrain model.
In particular, the Duntocher Burn passes beneath both Dumbarton Road and the Forth and Clyde Canal via
culvert and bridge structures that are not fully represented within the digital terrain model. This creates artificial
barriers, or "false blockages", within mapped flow paths, resulting in unrealistic ponding and exaggerated surface
water flood extents.
The release of the 2025 SEPA Flood Maps has significantly reduced the mapped flood risk at this location and
is now much more closely aligned with the integrated model predictions. Both datasets indicate that pluvial flood
risk is limited and that there is little evidence of significant sewer flooding within the hotspot. Consequently, the
available evidence from the updated SEPA mapping, hydraulic modelling and site observations supports the
conclusion that flood risk at this location is substantially lower than indicated by the original SEPA dataset and
that the previously identified hotspot was largely influenced by terrain-model artefacts associated with the
representation of the Duntocher Burn crossings. 
Figure 4-37 - Integrated model predicted flooding compared to SEPA pluvial flood maps (200 year RP)

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4.3.3.8 Dunedin Terrace
The integrated modelling indicates that flooding within the Dunedin Terrace hotspot is limited and largely confined
to isolated low points along North Douglas Street and Dunedin Terrace. The model predicts only shallow flooding,
with very little flooding exceeding 0.3 m in depth, suggesting limited potential for significant impacts to properties
or infrastructure.
These findings are consistent with the conclusions of the desktop root cause analysis. As discussed in Section
4.2, the updated 2025 SEPA Flood Maps indicate a notable reduction in the extent and severity of surface water
flooding at this location compared to the previous dataset, with fewer properties shown to be at risk and only
limited areas of deeper flooding identified. The integrated model results are therefore more closely aligned with
the updated SEPA mapping than with the previous flood maps.
In addition, no historical flooding records were identified from WDC or other available sources to support the
existence of a significant flood risk at this location. Consequently, whilst the modelling indicates that localised
ponding may occur during intense rainfall events, the combined evidence from the updated SEPA mapping,
hydraulic modelling and available flood records suggests that the overall level of flood risk at Dunedin Terrace is
relatively limited compared to the other hotspots assessed within the study area. 
Figure 4-38 - Integrated model predicted flooding compared to SEPA pluvial flood maps (200 year RP)

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4.3.3.9 Kilbowie Road
The integrated modelling indicates that flooding within the Kilbowie Road hotspot is concentrated along
Coldstream Road, with overland flow conveyed from higher ground to the east, including the wider Livingstone
Street area. Additional localised ponding is also predicted within parts of the Clyde Shopping Centre area. The
model results indicate flooding depths that could result in disruption to the local road network and access routes
during intense rainfall events.
The integrated model results show good agreement with both the original and updated SEPA surface water flood
maps, which consistently identify this location as being susceptible to flooding. Although the 2025 SEPA Flood
Maps indicate a modest reduction in the extent of flood risk compared to the previous dataset, significant areas
of flooding remain evident within both the SEPA mapping and the integrated model predictions.
As discussed in the desktop root cause analysis, whilst no historical flooding records were identified from WDC,
media reports and information from ScW indicate a history of flooding and drainage-related issues within the
wider area. In particular, the proximity of sewer flooding records at Cambridge Avenue suggests that sewer
network performance may also influence flooding mechanisms locally.
Consequently, the available evidence indicates that Kilbowie Road remains an area of flood susceptibility, with
flood risk influenced primarily by surface water runoff, whilst sewer network constraints may also contribute to
flooding within the wider catchment. 
Figure 4-39 - Integrated model predicted flooding compared to SEPA pluvial flood maps (200 year RP)
4.3.3.10 Station Road
Due to limitations on the extent of network model, this hotspot was not assessed in the pluvial model.

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4.3.3.11 Dumbarton Road (west)
Due to limitations on the extent of network model, this hotspot was not assessed in the pluvial model.
4.3.4 Model Limitations
At all times, reasonable skill and care has been used to ensure that the model was updated to best represent the
physical nature and hydraulic performance of the catchment, within the confines of the Client Brief and Client
Budget. It is highlighted that models only represent aspects of systems which we can both understand and
quantify, and running simulations in a model environment carries limitations associated with required
simplification and uncertainties including, but not limited to, the point outlined below.  
 A number of key flooding mechanisms identified during the desktop review and stakeholder engagement
are not fully represented within the hydraulic model. These include the unnamed watercourse at
Duntocher Road, which is currently being investigated by ScW due to its potential interaction with the
combined sewer network, and historic drainage features within the Livingstone Street/Linnvale area that
may influence sewer performance. As a result, the contribution of these systems to observed flooding
remains uncertain.
 The calibration of this model is based on a combination of historical anecdotal evidence (the RP’s of
historical events are not known), and SEPA surface water depth flood maps. As no measured data or
evidence of depths of flooding at flooding hotspots has been provided to calibrate the model against, the
exercise is considered an assessment of the predicted flows which may reach each hotspot based on
the data provided.  
 While the Dalmuir ScW models were used as a basis for the SWMP, following updates to the surfaces
to more accurately understand pluvial flooding, some impact on previous flow survey verification has
occurred. Sense checks have been undertaken on flows in the ScW sewer system, and no reverification
has been undertaken using historic flow survey data. Therefore, the model is considered to underpredict
the flows that enter the sewer system, however, it is considered conservative for assessment of surface
flows for the purpose of the LA SWMP. 
 Gullies are typically designed to operate up to a 1 in 5-year RP event, and so their impact is considered
limited for the larger RP’s used to assess flooding in this model. The losses into the sewer system that
would occur from their representation therefore means that potential flows into the piped system are
more limited than in reality. 1D subcatchments, typically used to generate runoff in a sewer model (as
per the ScW baseline) route runoff directly into the piped network. This can be conservative for flows
more than the design of gullies in terms of out-of-sewer flooding in the 1D model.
 All simulations represent current climate conditions. In other words, future design horizons were not
represented (increases in population, impacts of climate change, etc), so options developed will not
consider the future performance of the catchment.
 The model should be used with caution when assessing out-of-sewer flooding and the effectiveness of
proposed mitigation measures. Since completion of the original SWMP, additional information has
become available through the updated 2025 SEPA Flood Maps, stakeholder engagement and ongoing
ScW investigations. These investigations have identified uncertainties regarding sewer connectivity and
flooding mechanisms at a number of hotspots. Any future use of the model to support option development
or detailed design should therefore be preceded by further model review, updating and reverification
where appropriate.
4.3.5 Future Flood Risk
A multitude of factors influence flood hazard and flood risk. The main factors are:
 Climate
 Land use (urban creep can greatly influence surface water flooding)
 Demographics

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It is important to understand how these factors will influence flood risk in the future so that holistic judgement
can be made, and appropriate actions can be taken to sustainably manage flood risk now and in the future. Key
information that helps to make this holistic judgement is:
 Understanding where significant flood risks may arise in the future and which areas are more
susceptible to change.
 Understanding and deciding which actions can be taken now to mitigate changes in the future.
 Consider the longevity of actions to ensure that actions taken now are resilient and adaptable to future
change.
 Prioritise actions – actions in an area that is highly sensitive to climate change should be given greater
importance.

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5. Set Objectives
In line with the Scottish Government’s SWMP guidance, the indicators used for the flood risk objectives were
the ‘at-risk’ receptors. 
Objectives were prioritised to help clarify which factors should be addressed first (i.e., in the short term) and
which factors can be addressed in the medium to longer term.
The category used to help prioritise were:
 Surface water flood risk (using information on flooding impact)
 Surface water flood risk to priority receptor groups (e.g., homes at risk in more socially vulnerable
areas).
 Locations with a history of flooding
 Areas where there is no history of flooding, but which are predicted to flood and should be treated with
caution (particularly where more detailed modelling is not available).
 Locations where there are opportunities for joint working (for example, making management more cost-
effective and delivering multiple benefits).
The hotspot areas are summarised in Table 5-1 below with each hotspot classified in terms of priority. It should
be noted that this assessment was undertaken as part of the initial SWMP submission in April 2024 and does not
take into account the updates discussed associated with the change in flood risk attributed to the 2025 SEPA
flood maps
Table 5-1 Objectives
Location /
Hotspot
History of
flooding
confidence in
data
Initial Objective Initial
Priority
Homes (1
in 30
year)
Loss in
Economic
Activity
Safety
Concerns
Second
Avenue /
Ramsay
Street
SEPA pluvial flood
maps and historic
flood data. Sewer
flooding.
Improve understanding of
surface water flooding in
area.
High 12  Roads
impacted 
Western
Isles Road
SEPA pluvial
Flood Maps and
historic flood data
Improve understanding of
surface water flooding in
area.
High 31  
Duntocher
Road
SEPA pluvial flood
maps and historic
flood data. Sewer
flooding.
Improve understanding of
surface water flooding in
area.
High 0 
1m deep
flooding
on roads

Livingstone
Street
SEPA pluvial flood
maps and historic
flood data. Sewer
flooding.
Improve understanding of
surface water flooding in
area.
High 14 Road 
Melbourne
Avenue
SEPA pluvial flood
maps and historic
flood data
Improve understanding of
surface water flooding in
area.
High 0 
0.9m deep
flooding
on roads

Low
Crescent
SEPA pluvial &
fluvial flood maps
and historic flood
Improve understanding of
surface water flooding in
area.
Med 52

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data. Sewer
flooding.
Dumbarton
Road
SEPA pluvial flood
maps and historic
flood data
Improve understanding of
surface water flooding in
area.
Med 0  
Dunedin
Terrace
SEPA pluvial flood
maps 
Improve understanding of
surface water flooding in
area.
Med
Large
block of
flats
Road 
Kilbowie
Road
SEPA pluvial flood
maps and historic
flood data
Improve understanding of
surface water flooding in
area.
Med 0  
Station
Road*
SEPA pluvial flood
maps and historic
flood data
Improve understanding of
surface water flooding in
area.
High* 0  
Dumbarton
Road (west)
SEPA pluvial flood
maps and historic
flood data
Improve understanding of
surface water flooding in
area.
Med 0  
*WDC requested that the Station Road hotspot be included as a high priority hotspot following the initial
submission of this report, due to this, Station Road was not included in the initial options appraisal.

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6. Option Appraisal
6.1 Scoping Option Appraisal
The options appraisal and development of preferred measures presented in this section were undertaken as part
of the initial SWMP submission and were based on the best available information at that time, including historical
flood records, stakeholder information, hydraulic modelling outputs and the SEPA Flood Maps then available. A
detailed appraisal was undertaken for the identified high-priority hotspots, whilst medium and lower priority
locations were assessed at a higher level to identify potential future actions and investigations.
Following completion of the initial assessment, additional information became available through the December
2025 stakeholder workshop involving WDC, ScW, Network Rail and Scottish Canals, together with subsequent
stakeholder engagement and the publication of the updated 2025 SEPA Flood Maps. This information provided
further insight into flood mechanisms, interactions between surface water, sewer, watercourse, canal and railway
drainage systems, and highlighted data gaps and ongoing investigations that influence the understanding of flood
risk at several locations. In some cases, the updated SEPA mapping also resulted in changes to the extent and
significance of previously identified hotspots.
The options appraisal presented in the following sections should therefore be viewed within the context of the
information available at the time it was undertaken. While the assessment remains valuable in identifying potential
flood risk management opportunities, the findings should be reviewed alongside the updated hotspot
assessments, stakeholder feedback and the outcomes of ongoing investigations before progressing any
preferred options. In particular, collaboration with ScW is recommended for the Dalmuir System Plan, in which
they are looking understand where local authority needs/investment is planned and how that can possibly link to
their own investment. The prioritisation adopted for the original options appraisal is outlined in Table 6-1
Table 6-1 Prioritisation of hotspots for Option Appraisal.
Location
History of
flooding /
confidence in
data (2024)
Initial Objective Initial
Priority
Include in
Option
Appraisal
(2024)
2026 update
Second
Avenue /
Ramsay Street
SEPA pluvial
flood maps and
historic flood data
Sewer flooding.
Reduce surface
water flooding High Yes
Collaboration
with ScW to
reduce surface
water and out
of sewer
flooding
Western Isles
Road
SEPA pluvial
Flood Maps and
historic flood data
Reduce surface
water flooding High Yes
Collaboration
with ScW to
reduce surface
water and out
of sewer
flooding
Duntocher
Road
SEPA pluvial
flood maps and
historic flood data
Sewer flooding.
Reduce surface
water flooding High Yes
Collaboration
with ScW to
reduce surface
water and out
of sewer
flooding
Livingstone
Street
SEPA pluvial
flood maps and
historic flood data
Sewer flooding.
Reduce surface
water flooding High Yes
Collaboration
with ScW to
reduce surface
water and out

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of sewer
flooding
Melbourne
Avenue
SEPA pluvial
flood maps and
historic flood data
Reduce surface
water flooding High Yes
Collaboration
with ScW to
reduce surface
water and out
of sewer
flooding
Low Crescent
SEPA pluvial &
fluvial flood maps
and historic flood
data Sewer
flooding.
Reduce surface
water flooding Medium
Not at this time
– action can be
for future option
appraisal
Pluvial
flooding no
longer main
driver based
on updated
dataset. 
Dumbarton
Road
SEPA pluvial
flood maps and
historic flood data
Reduce surface
water flooding Medium
Not at this time
– action can be
for future option
appraisal
Pluvial
flooding no
longer main
driver based
on updated
dataset.
Dunedin
Terrace
SEPA pluvial
flood maps 
Reduce surface
water flooding Medium
Not at this time
– action can be
for future option
appraisal
Pluvial
flooding no
longer main
driver based
on updated
dataset.
Kilbowie Road
SEPA pluvial
flood maps and
historic flood data
Reduce surface
water flooding Medium
Not at this time
– action can be
for future option
appraisal
Not at this time
– action can
be for future
option
appraisal
Station Road*
SEPA pluvial
flood maps and
historic flood data
Reduce surface
water flooding High*
Not at this time
– action can be
for future option
appraisal
Added as a
high priority
hotspot
following the
previous
submission
Dumbarton
Road (west)
SEPA pluvial
flood maps and
historic flood data
Reduce surface
water flooding Medium
Not at this time
– action can be
for future option
appraisal
Not at this time
– action can
be for future
option
appraisal
*WDC requested that the Station Road hotspot be included as a high priority hotspot following the initial
submission of this report, due to this, Station Road was not included in the initial options appraisal.

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6.2 Options Assessed
A wide range of measures were considered for potential use in the hotspot areas to reduce surface water flooding.
Both non-structural and structural measures were considered.
6.2.1 Non-Structural
The non-structural and structural measures that were investigated are outlined in Table 6-2.
Table 6-2 Table outlining non-structural intervention measures to reduce surface water flooding, as
outlined in the Flood Risk Management (Scotland) Act 2009: Surface Water Management Planning
Guidance. 
Action Action Description Notes 
Land use planning
policy – adhere to
existing
New development should not be at
risk of surface water flooding and
does not increase flooding
elsewhere. To achieve this, surface
water (drainage and flooding) should
be managed sustainably above-
ground and should integrate with and
enhance the urban landscape.
This requirement will continue
to apply. It is considered
difficult to implement more
stringent policies because of
WDC’s competing ‘One Plan
One Place’ objective. 
Land use planning
policy – implement
more stringent
policies 
New developments may have the
potential to reduce existing flood
risks. Where this is possible local
policies (e.g., In supplementary
planning guidance) to implement this
should be put in place for
development planning and
development management. 
Clarify
responsibilities for
new surface water
management
infrastructure 
Clarify ownership and vesting
processes for all surface water
management and infrastructure in
new developments (drainage and
flooding up to 1 in 200-year rainfall
event) and set out how they will work
with the land use planning system to
meet required planning policies. 
Clarify
responsibilities for
existing surface
water management
infrastructure
Clarify and agree ownership for
maintaining existing surface water
management infrastructure (including
SuDS) 
Emergency
response plans
Use information about surface water
flood risk to improve emergency
response plans

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Study – improve
understanding
Carry out modelling and other
assessments to improve knowledge
of flood hazards and risk (adverse
impact)
Currently underway 
Study – option
appraisal and
design
Further study to appraise
management options in more detail
or take a preferred option to detailed
design.
Currently underway 
Study – improve
information on
surface water flood
events
Improve data collection on surface
water flood events when they occur,
to improve knowledge of surface
water flood risk and improve
confidence in surface water flood
models.
It is recommended that WDC
improve their data collection
and recording of flooding
events. 
Self-help –
community flood
action groups and
resilient community
plans   
Self-help –-property-
level protection
Increase the resilience of individuals
and businesses through self-help
actions, helping to ensure that
people, communities, and
businesses are prepared for flooding,
knowing what action they can take
and can recover quickly afterwards.
Door flood door or barrier
(manually fitted), air brick
cover, install non-return valves
on drainage outlets, pointing or
waterproofing brickwork, raise
vulnerable features such as
electrical sockets above floor
level, submersible pump. 
Self-help –-property-
level resilience
(retrofit)   
Flood forecasting
and warning
Develop surface water flood
forecasting, alerts, and warning
systems. SEPA issues surface water
flood forecasting and alerts but does
not currently provide surface water
flood warnings. Other authorities may
contact SEPA for advice on installing
local schemes. 
Asset management
and maintenance
Review and change existing systems
for inspecting and maintaining
surface water management
infrastructure e.g., culverts, SUDS,
sewers, and road drainage. 
Watercourse
management and
maintenance
Review and change existing systems
for inspecting and maintaining urban
burns.

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Relocation Relocate properties or infrastructure
away from flood risk areas. 
6.2.2 Structural
The structural measures that were investigated are outlined in Table 6-3.
Table 6-3 – Table outlining structural above ground intervention measures to reduce surface water
flooding, as outlined in the Flood Risk Management (Scotland) Act 2009: Surface Water Management
Planning Guidance.
Action Action Description Notes 
Restoring urban
watercourses
Restore urban watercourse (e.g.,
restoring floodplains and
deculverting) to reduce flooding
from watercourse itself and
provide more opportunities to
convey surface water into the
natural environment. 
Urban water
engineering
Storage (online or offline storage),
embankments, walls, or flood
diversion channel in urban burns. 
Runoff reduction
strategy
Develop a long-term plan for
making whole urban areas greener
and more permeable and reducing
grey surfaces. 
Green infrastructure allows more
rain to infiltrate the ground and
encourages evapotranspiration in
the atmosphere, reducing runoff
rates and volumes. This can help
manage frequent rainfall events,
mitigate urban creep and adapt
to climate change. 
Reducing surface water
in sewer
Identify opportunities to reduce
surface water in sewers. ScW is
responsible for the sewer network
and should be contacted regarding
any proposals. WDC may see
opportunities when managing
surface water flooding or where
sewer network overflows may be
contributing to surface water
flooding problems. ScW and WDC
should coordinate work to realise
multiple benefits. 
Land management -
NFM
Implement land management
actions that reduce the rate and
volume of runoff. Runoff from more
rural land can flood homes,
businesses, and infrastructure

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directly and, by significantly
increasing flows to urban areas,
drainage systems and watercourse
can raise flood risk further
downstream. 
Underground storage
Divert surface water to storage
tanks or by providing storage in
the existing drainage / flood
management network. 
Underground
conveyance
Increase capacity or build new
underground pipes for surface
water 
Modification of
culverted watercourses
Increase the capacity of culverted
watercourses or divert culverted
watercourses 
The importance of the sustainable management of water is becoming increasingly evident because of the ever-
increasing pressures placed on natural resources because of various factors such as: increasing population and
increasing food demands, (trend towards wetter winters and drier summers).
Therefore, it is no surprise that the sustainable management of water is a catalyst for economic growth, social
change, improved public health (both physical and mental) and improved resilience to adapt to the constantly
changing climate because of climate change impacts and the uncertainties associated with climate change. WDC
strongly recognise this and prefer above ground sustainable solutions where feasible and cost-effective.
6.2.3 Property Level Protection
Flood water can enter a property through a variety of mechanisms. For example:
 Entry at air bricks
 Entry through party walls from property next door if it is flooded.
 Entry through cracks in brickwork
 Seepage through ground entering through the floors of basements and cellars.
 Backflow through overloaded drainage/sewer system blocked by flooding.
 Entry at the damp-proof course
 Entry through permeable brickwork and weathered or damaged mortar.
 Entry at gaps and cracks in joint sealant around doors and windows
 Entry through gaps around pipes and cable pass throughs in walls and floors

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Figure 6-1 – Different mechanisms of flood water entry into properties.
6.2.4 SuDS Types
The SuDS types investigated in the options appraisal are summarised in Table 6-4.
Table 6-4 Table outlining SuDS measures considered.
SuDS
Measure Brief description of all 15 types  
Green roofs (1) Planted roof suitable for large flat
roofed buildings

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Water butts
(2) Private solutions for storing water
installed on residential buildings by
diverting existing rainwater downpipes
into water butts 
Various
permeable
pavings and
soakaways 
(3) Permeable paving: Permeable surface
with underground gravel or plastic
boxes storage space 
(4) Gravel paving:  Gravel surface
providing some storage suitable for
car parks etc. 
(5) Filter drains:  Trench filled with gravel
allowing some storage 
(6) Soakaways: Excavation filled with
gravel or plastic boxes (to allow water
infiltration into the ground) and
covered with soil 
(7) Disconnecting downpipes:
Disconnected rainwater downpipes
from large buildings into underground
storage usually beneath permeable
pavements  
Raingardens 
(8) Bioretention: Includes pocket
infiltration, bioretention and multiple
tree pits. The same set up as rain
gardens (surface) but separated in
assessment as they are supposed to
take runoff from roads whilst surface
rain gardens only from residential
roofs. 
(9) Single tree pits with storage beneath 
Raingardens either: 
(10) Rain garden (box) 1m high boxes with
voids for water storage and surface
planting

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(11) Raingardens (surface): Residential
solution consisting of surface planting
with limited storage capacity to direct
runoff from roof or hardstanding into
these raingardens, or 
(12) Attenuating rain gardens: Raingardens
with additional storage beneath in a
form of gravel or plastic boxes storage
more suitable for larger public spaces 
Large
nature-based
solutions 
(13) Swales: Large grassed channels,
includes wet and dry, linear and round
solutions 
(14) Ponds: Suitable in large natural
spaces only 
(15) Wetlands: Shallow features suitable
only in large natural spaces

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6.3 Develop Preferred Option / Screening
The long list of options presented in this section were developed as part of the previous SWMP submission in
April 2024, based on the understanding of flood risk and flooding mechanisms available at that time. The options
were informed by the root cause analysis, hydraulic modelling and stakeholder information available during the
original assessment and were intended to identify potential opportunities to manage flood risk at each hotspot.
The long list of options was developed taking cognisance of:
 Meeting the objectives outlined in Section 5;
 Promoting a sustainable approach to flood risk management; and
 Working collaboratively with stakeholders.
As previously noted, since completion of the original options appraisal, additional information has become
available through the December 2025 stakeholder workshop, subsequent stakeholder engagement, ongoing
investigations and publication of the 2025 SEPA Flood Maps. This information has improved understanding of
the interactions between surface water flooding, sewer systems, watercourses, transport infrastructure and other
stakeholder assets across the catchment. It has also identified a number of data gaps and highlighted the
interconnected nature of flooding mechanisms within Clydebank.
As a result, the options identified within the original appraisal should be reviewed in the context of this updated
understanding of flood risk. In particular, the workshop discussions highlighted the need for a more strategic and
collaborative catchment-wide approach, recognising that opportunities associated with ScW, Network Rail,
Scottish Canals, WDC and other stakeholders' assets may provide greater benefits than individual hotspot-
specific interventions delivered in isolation. It should be noted that the existing sewer system is understood to
have little or no spare capacity for additional flows. However, Scottish Canals have advised that they would be
open to considering this, and the potential for doing so can be investigated further. The options presented in the
following sections should therefore be considered as an initial evidence base that can inform future strategic
option development and partnership working across the wider catchment.
6.3.1 Second Avenue / Ramsay Street
The Second Avenue / Ramsey Street hotspot was identified during the initial SWMP assessment due to historical
flooding records, significant road flooding and evidence of sewer network exceedance. The long list of options
identified for Second Avenue / Ramsay Street is outlined in Table 6-5 and illustrated in Figure 6-2. 
Table 6-5 - Options outlined for Second Avenue
No Location Option
1a Park Road Park Avenue junction with B814 – remove redundant bus only arm and
replace with attenuation basin 
1b Park Road Park Avenue junction with B814 – remove redundant bus only arm and
replace with underground storage tank
2a
Second Avenue (stretch
between Park Road and St
Stephen’s Primary School)
Install a new additional sewer to convey flow to St Stephen’s Primary
School and attenuate within the school (rain garden or swale to convey
flow) – road width to be reduced by 1.5m 
2b
Second Avenue (stretch
between Park Road and St
Stephen’s Primary School)
Install a new additional sewer to convey flow to St Stephen’s Primary
School and attenuate within the school (engineered channel) – road width
to be reduced by 1.5m
3 Duntocher Road Install a rain garden or shallow swale and reduce road width along
Duntocher road by 2-3m
4 Duntocher Road (Option 1 in
the Duntocher Road Hotspot) SuDs Basin

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Figure 6-2 - Options outlined for Second Avenue
As discussed in the root cause analysis, the flooding mechanism at Second Avenue / Ramsay Street is influenced
by a combination of surface water runoff and sewer flooding, and is hydraulically linked to the wider catchment
upstream at the Duntocher Road hotspot (see Section 6.3.3 for a summary of options at this hotspot). The root
cause analysis identified that runoff conveyed through the catchment has the potential to influence flooding at
both locations. ScW is currently undertaking investigations to improve understanding of the interactions between
the sewer network, storm drainage systems and the unnamed watercourse within the wider area, and the
outcomes of these investigations are expected to provide important information regarding the sources of flooding
and performance of the drainage system.
Consequently, the options identified for Second Avenue / Ramsay Street should be reviewed in light of the
findings of the ongoing ScW investigations before being progressed further. In particular, due to the hydraulic
linkages, options proposed at Duntocher Road may provide benefits to the downstream Second Avenue /
Ramsay Street hotspot through attenuation of runoff and reduction of flows conveyed through the catchment.
However, the uncertainties associated with the current understanding of flooding mechanisms, including the role
of the unnamed watercourse and sewer network interactions, should be taken into account when assessing the
likely effectiveness of these measures.
Given the significant contribution from sewer flooding at this location, a collaborative approach between WDC
and ScW will be required to identify the most appropriate long-term solution. If a detention basin or similar surface
water storage feature is progressed in isolation of a wider strategic approach, consideration should be given to
the potential presence of out-of-sewer flooding within stored floodwaters. In such circumstances, appropriate
water quality and biological treatment measures may be required to manage risks associated with contaminated
floodwaters and ensure compliance with relevant environmental and public health requirements.

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6.3.2 Western Isles Road
The Western Isles Road hotspot was identified during the initial SWMP assessment due to historical flooding
records, reported sewer surcharging, evidence of sewer network exceedance and the low-lying topography
surrounding Durban Avenue, which contributes to localised ponding during heavy rainfall events. The root cause
analysis identified a combination of surface water runoff and sewer flooding, with sewer capacity constraints
considered a significant contributor to flood risk at this location. The long list of options identified for Dunbarton
Road is outlined in Table 6-6 and illustrated in Error! Reference source not found..
Table 6-6 Options outlined for Western Isles Road.
No Location Option
1a Western Isles Road (junction
with Dumbarton Road)
Kerb inlets within south arm of the roundabout to collect surface water in
centre of roundabout, attenuate and convey to playpark between
Dumbarton Road and Durban Avenue (SuDS basin)
1b Western Isles Road (junction
with Dumbarton Road)
Kerb inlets within north arm of the roundabout to collect surface water in
centre of roundabout, attenuate and convey to playpark between
Dumbarton Road and Durban Avenue (underground storage tank)
2
Western Isle Road
(Greenspace between
Western Isles Road and
Dumbarton Road
SuDS basin or SuDS Pond to attenuate runoff and discharge at greenfield
rate into sewer
3 Western Isle Road  Roadside swales to convey and attenuate surface water and store in the
park  
4 Iona Place Speed bump where Iona Place meets Western Isle Road to prevent
additional flow entering Iona Place

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Figure 6-3 - Options outlined Western Isles Road
6.3.3 Duntocher Road
The Duntocher Road hotspot was identified during the initial SWMP assessment due to historical flooding
records, significant road flooding and evidence of sewer network exceedance. The long list of options identified
for Duntocher Road is outlined in Table 6-7 and illustrated in Figure 6-4.
Table 6-7 Options outlined for Duntocher Road.
No Location Option
1
In grassy area immediately west of the
Kilbowie Roundabout (between the
A82 and Duntocher Road)
SuDS basin providing surface water attenuation prior to
discharge into the sewer network
2
In the grassy verge between the A82
east and west bound roads (north-west
of the Kilbowie Roundabout)
Roadside swale providing conveyance and attenuation of
surface water prior to discharge into the sewer network
3
In grassy area immediately north of the
Kilbowie Roundabout (between the
A82 and Kilbowie Road)
SuDS basin providing surface water attenuation prior to
discharge into the sewer network
4 Centre of the Kilbowie Roundabout SuDS basin providing localised surface water attenuation prior to
discharge into the sewer network
5 Green space south of the A82 (south-
east of the Kilbowie Roundabout)
SuDS basin providing surface water attenuation prior to
discharge into the sewer network
6 Kilbowie Park and Ride Permeable paving to reduce runoff rates and volumes
discharged to the sewer network

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Figure 6-4 - Options outlined Duntocher Road
As discussed in the root cause analysis, the flooding mechanism at Duntocher Road is not yet fully understood
due to uncertainties surrounding the interaction between the sewer network, the storm drainage system and the
unnamed watercourse running parallel to the road. ScW is currently undertaking investigations to better
understand these interactions, including the potential connectivity between the unnamed watercourse and the
combined sewer network. The outcomes of these investigations are expected to provide important information
regarding the sources of flooding and the performance of the drainage system at this location.
Consequently, the options identified for Duntocher Road should be reviewed in light of the findings of the ongoing
ScW investigations before being progressed further. In particular, any future option development should consider
the potential influence of the unnamed watercourse, the storm drainage outfalls to the adjacent parkland and any
identified sewer network constraints to ensure that measures do not create downstream detriment or
inadvertently increase flood risk elsewhere within the catchment.
Given the complex and interconnected nature of the flooding mechanisms at this site, together with the significant
contribution from sewer flooding, a collaborative approach between WDC and ScW will be required to identify
the most appropriate long-term flood risk management solution. If a detention basin or similar surface water
storage feature is progressed at this location in isolation of a wider strategic solution, consideration should be
given to the potential presence of out-of-sewer flooding within the stored floodwaters. In such circumstances,
appropriate water quality and biological treatment measures may be required to manage the risk associated with
contaminated floodwaters and to ensure compliance with relevant environmental and public health requirements.

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6.3.4 Livingstone Street
The Livingstone Street hotspot was identified during the initial SWMP assessment due to historical flooding
records, the strategic importance of the road as the sole vehicular access route into Linnvale, and evidence of
sewer network exceedance. The long list of options identified for Livingstone Street is outlined in Table 6-8 and
illustrated in Figure 6-5.
Table 6-8 Options outlined for Livingstone Street.
No Location Option
1 Grassy verge south of
Livingstone Street SuDS Basin
2 Clyde Retail Park Disconnect large commercial roof downpipes and store in underground
storage below the parking areas.
3 Linnvale Primary School Disconnect roof downpipes from the school into rain gardens, SuDS, or
underground storage 
4 Linnvale Primary School Minimise extent of impermeable surfacing in the playground area to
reduce runoff generated from the school grounds.
5 North of Shinwell Avenue
and railway
Take into account investigations by ScW whether there is an upstream
watercourse contributing flow into the combined sewer through a drainage
survey in this location. If an upstream connection is found a short-term
flow survey may help to verify flows experience here and understand how
much this is contributing to flooding in the Livingstone Street area. 
Figure 6-5 - Options outlined for Livingstone Street
As discussed in the root cause analysis, the flooding mechanism at Livingstone Street is influenced by
interactions between surface water runoff and the sewer network. However, the updated 2025 SEPA Flood Maps
indicate a substantial reduction in predicted pluvial flood risk compared to the mapping used during the initial
SWMP assessment, suggesting that widespread surface water flooding is less significant than originally

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anticipated. Ongoing ScW investigations, including consideration of the potential interaction between historic
drainage features and the combined sewer network, are expected to further improve understanding of the flooding
mechanism at this location.
Consequently, the options identified for Livingstone Street should be reviewed in light of the updated flood
mapping and the outcomes of the ongoing ScW investigations before being progressed further. While the original
options were developed primarily to manage surface water runoff, they may still provide benefits by reducing
inflows to the sewer network and helping to alleviate sewer exceedance during heavy rainfall events.
Given the evidence that sewer flooding may be a primary contributor to flood risk at this location, a collaborative
approach between WDC and ScW will be required to identify appropriate long-term solutions. Future option
development should therefore focus on opportunities that provide integrated benefits to both surface water and
sewer systems and should be considered within the context of wider strategic investigations being undertaken
across the catchment.
6.3.5 Melbourne Avenue
The Melbourne Avenue hotspot was identified during the initial SWMP assessment due to historical flooding
records, recurring drainage issues and evidence of sewer network exceedance. The root cause analysis found
that flooding is concentrated around the low point on Melbourne Avenue and is associated with a combination of
surface water runoff, blocked drainage infrastructure and surcharge from the combined sewer network. Avenue,
indicating that sewer capacity constraints are a significant contributor to the observed flood risk. 
The long list of options identified for Melbourne Avenue is outlined in Table 6-9 and illustrated in 
Figure 6-6.
Table 6-9 Options outlined for Melbourne Avenue.
No Location Option
1 Melbourne Avenue Swale to west of Melbourne Avenue across from the bus shelter
2 Melbourne Avenue Swale and geocellular crate below to the west of Melbourne Avenue
across from the bus shelter
3 Melbourne Avenue
New over-sized surface water sewer system that connects back into the
combined system just north-west of the existing play park area but could
have a separate outfall in the future (designed to have an overland flow
path down Salisbury Place).

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Figure 6-6 - Options outlined for Melbourne Avenue

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6.4 Prioritising Options
The long list of solutions has been screened using a multi-criteria assessment to reduce the number of potential measures taken forward for further
consideration. The purpose of this process is to focus subsequent appraisal on those options that are considered most likely to provide a viable means of
managing flood risk. The multi-criteria analysis is based on a high-level assessment of relative cost, feasibility and effectiveness at reducing flood volume. This
prioritisation does not represent a detailed cost benefit analysis, nor does it account for all site-specific constraints, planning considerations or potential
stakeholder input. The feasibility and effectiveness of the options should be reviewed further at design stage when data from more detailed investigations is
available. Accordingly, this prioritisation should be treated as indicative. In addition, the feasibility and effectiveness of potential measures should be reviewed
in consultation with WDC, ScW and other relevant stakeholders to ensure that wider drainage system interactions, ongoing investigations and catchment-wide
objectives are appropriately considered. Options highlighted in green scored the highest. In certain instances, multiple options have been shortlisted for
consideration together, reflecting their complementary strengths.
The four key criteria used for screening unfeasible actions were:
 Sustainability (environmental, economic and social sustainability);
 Technical feasibility;
 Legal and planning considerations; and
 Effectiveness in reducing flood risk.
Table 6-10 shows the scoring criteria that was applied when performing the multi-criteria assessment.
Table 6-10 - Multi-Criteria Assessment Scoring Criteria
Public or Private Planned Resurfacing Volume Attenuated Relative Cost Technical Feasibility
Effectiveness at
removing flow
volumes –
considers flow
passing through
and proximity to
main flooding
Total Score
1 (private) - 5 (public)
1 (no planned
resurfacing) – 5
(planned resurfacing)
1 (limited attenuation
capacity) – 5 (greater
attenuation capacity)
1 (higher cost
implications)
– 5 (lower cost
implications)
1 (complex) – 5 (limited
perceived constraints)
1 (minimum
effectiveness) – 10
(maximum
effectiveness)

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6.4.1 Second Avenue / Ramsay Street
The multi-criteria assessment for Second Avenue / Ramsay Street is outlined in Table 6-11. 
Table 6-11 - Multi-Criteria Assessment for Second Avenue / Ramsay Street
ID Option Location Public or
Private
Planned
Resurfacing
Volume
Attenuated Relative Cost Technical
Feasibility
Effectiveness
at removing
flow volumes
Total Score
1a Attenuation basin Park Road 5 1 3 3 3 6 21
1b Underground storage
tank Park Road 5 1 4 2 2 5 19
2a
New storm sewer and
attenuation with
raingarden or swale
Second Avenue (stretch
between Park Road and St
Stephen’s Primary School)
5 1 2 3 3 4 18
2b
New storm system
and attenuation with
engineered channel
Second Avenue (stretch
between Park Road and St
Stephen’s Primary School)
5 1 4 2 3 6 21
3 Raingarden and
swale Duntocher Road 5 1 2 2 2 2 14
4 SuDs basin 
Duntocher Road Basin
(Duntocher Road Hotspot Option
1)
5 1 5 3 4 8 26

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6.4.2 Western Isles Road
The multi-criteria assessment for Western Isles Road is outlined in Table 6-12.
Table 6-12 - Multi-Criteria Assessment for Western Isles Road
ID Option Location Public or
Private
Planned
Resurfacing
Volume
Attenuated Relative cost Technical
Feasibility
Effectiveness
at Removing
flow Volumes
Total
1 SuDS basin
Western Isles Road
(junction with Dumbarton
Road)
5 1 2 4 3 4 19
1b Underground storage tank
Western Isles Road
(junction with Dumbarton
Road)
5 1 3 2 3 5 19
2 SuDS basin
Western Isle Road
(Greenspace between
Western Isles Road and
Dumbarton Road
5 1 4 3 3 5 21
3 Swale and attenuation in
park   Western Isles Road  5 1 4 4 4 6 24
4 Speed bump to divert flows Iona Place 5 1 1 3 4 1 15

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6.4.3 Duntocher Road
The multi-criteria assessment for Duntocher Road is outlined in Table 6-13.
Table 6-13 - Multi-Criteria Assessment for Duntocher Road
ID Option Location Public or
private
Planned
resurfacing
Volume
Attenuated Relative Cost Technical
Feasibility
Effectiveness
at removing
flow volumes
Total
1 SuDS Basin 
In grassy area immediately
west of the Kilbowie
Roundabout (between the
A82 and Duntocher Road)
5 1 5 3 4 8 26
2 Swale 
In the grassy verge
between the A82 east and
west bound roads (north-
west of the Kilbowie
Roundabout)
5 1 3 3 4 6 22
3 SuDS Basin 
In grassy area immediately
north of the Kilbowie
Roundabout (between the
A82 and Kilbowie Road)
5 1 5 3 4 6 24
4 SuDS Basin Centre of the Kilbowie
Roundabout 5 1 3 3 3 5 20
5 SuDS Basin
Green space south of the
A82 (south-east of the
Kilbowie Roundabout)
5 1 3 3 4 4 20
6 Permeable Paving Kilbowie Park and Ride 1 1 2 2 2 3 11

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6.4.4 Livingstone Street
The multi-criteria assessment for Livingstone Street is outlined in Table 6-14.
Table 6-14 - Multi-Criteria Assessment for Livingstone Street.
ID Option Location Public or
private
Planned
resurfacing
Volume
Attenuated
Relative
Cost
Technical
Feasibility
Effectiveness at
removing flow
volumes
Total
1 SuDS Basin Grassy verge south of
Livingstone Street 5 1 4 3 4 6 23
2
Commercial roof
disconnection and
attenuation
Clyde Retail Park 1 1 2 1 3 3 11
3 School roof disconnection
and attenuation 
Linnvale Primary
School 1 1 2 1 3 3 11
4 De-paving in school Linnvale Primary
School 1 1 2 2 3 3 12
5
Upstream inflow
investigation Shinwell Avenue N/A N/A N/A N/A N/A N/A -

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6.4.5 Melbourne Avenue
The multi-criteria assessment for Livingstone Street is outlined in Table 6-15.
Table 6-15 - Multi-Criteria Assessment for Livingstone Street.
ID Option Location Public or
private
Planned
resurfacing Volume Relative
Cost
Technical
Feasibility
(Effectiveness at
removing flow volumes) Total
1 Roadside swale Melbourne Avenue 5 1 3 4 5 4 22
2 Swale and geocellular
storage Melbourne Avenue 5 1 4 3 4 6 23
3 Oversized surface water
sewer Melbourne Avenue 5 1 3 2 3 4 18

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6.5 Baseline: ‘Do minimum’
The baseline scenario against which the impacts and cost of other options can be compared against is the ‘do
minimum’ option. The ‘do-minimum’ scenario was selected as the most appropriate baseline for surface water
management. This is because there is a statutory requirement imposed on WDC to continue some surface water
management activities. 
The ‘do-minimum’ scenario is the minimum existing actions carried forward to ensure adherence to statutory
duties and responsibilities. For example: 
 adherence to Scottish Planning Policy, 
 duties for emergency response planning, 
 agreement between responsible authorities as a matter of policy and, 
 continuing asset management 
The ‘do-minimum’ scenario assumes that the baseline model drainage capacity (1 in 5-year drainage capacity if
using SEPA pluvial modelling) is maintained. This means that an effective schedule of clearance and repair or
inspection and maintenance regime of drainage infrastructure is performed by WDC. Moreover, once an existing
structure reaches the end of its design life, it is assumed that it will be replaced.
6.6 Options: ‘Do something’
The ‘do something’ options were developed by combining the refined actions identified for each hotspot and
were modelled as part of the initial SWMP submission using the information, flood mapping and hydraulic models
available at that time.
Since completion of the original assessment, additional information has become available through the December
2025 stakeholder workshop, publication of the 2025 SEPA Flood Maps, and ongoing ScW investigations across
the Dalmuir catchment. As discussed throughout this report, this information has improved understanding of
flooding mechanisms, identified a number of data gaps and uncertainties, and highlighted the significant
interaction between surface water flooding, sewer network performance, watercourses and wider drainage
infrastructure.
Consequently, whilst the original option modelling provides a useful indication of the potential benefits of runoff
reduction measures, the results and associated option performance assessments should now be considered
superseded by the improved understanding of flood risk. The options developed during the initial assessment
were largely hotspot-specific interventions, whereas the updated evidence demonstrates that flooding at many
locations is strongly influenced by wider catchment processes, sewer network constraints and significant volumes
of out-of-sewer flooding.
It is therefore recommended that the previously developed options are not progressed on the basis of the original
modelling alone and are instead reassessed as part of a more strategic and collaborative catchment-wide
approach involving WDC, ScW and other key stakeholders. This reassessment should take account of the
outcomes of ongoing investigations, updated flood risk information and links to the Dalmuir System Plan. Even
where local runoff management measures remain appropriate, close collaboration with ScW will be required to
ensure that residual sewer flood risk is adequately addressed and that interventions provide benefits at both the
hotspot and wider catchment scale. Table 6-16 summarises the ‘Do Something’ standalone options identified in
the multi criteria analysis.
Table 6-16 – Summary of ‘Do Something’ options
Hotspot
Name No Location Option
1a Park Road Attenuation basin at junction

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Second
Avenue/
Ramsey
Street
2b
Second Avenue (stretch
between Park Road and St
Stephen’s Primary School)
Attenuation at school
4 Duntocher Road (Option 1 in
the Duntocher Road Hotspot) SuDs Basin
Western
Isles Road 3 Western Isles Road Roadside swales  
Duntocher
Road 1
In grassy area immediately
west of the Kilbowie
Roundabout (between the
A82 and Duntocher Road)
SuDs Basin
Livingstone
Street 1 Grassy verge south of
Livingstone Street SuDs Basin
Melbourne
Avenue 2 Melbourne Avenue Swale and geocellular storage

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7. Develop preferred option: confirm
funding
Sources of funding available for options within the Clydebank area were considered and these primarily sit with
WDC because of the nature of the flooding (surface water) and how the responsibilities for implementation current
sit.
It should be recognised that these are other sources of funding available which may include:
 ScW maintenance
 ScW capital via quality and standard process
 Private funding (developer contributions)
 Other sources of funding
ScW were engaged in the process and as it stands, they only have funding within their capital funding works for
internal flooding up to the 10% Annual Exceedance Probability event (1 in 10 Year Return Period Event).
Table 7-1 Actions
Location Existing Action New Action (2026 update) Future Action 
Second
Avenue /
Ramsay Street
Road gully
maintenance
Flood incident
records
Update emergency response
planning with new pluvial flood
information
Continue coordination with ScW
and ongoing investigations; review
flood mechanism and links with
Duntocher Road hotspot; continue
runoff reduction and blue-green
infrastructure opportunities where
appropriate.
Review hotspot following ScW
investigations and catchment
studies; consider integrated
catchment-scale options rather
than standalone schemes.
Western Isle
Road
Road gully
maintenance
Flood incident
records
Update emergency response
planning with new pluvial flood
information
Continue coordination with ScW
regarding sewer flooding; maintain
flood incident records and review
any future flooding occurrences;
continue runoff reduction strategy
where opportunities arise.
No further hotspot-specific
option appraisal currently
recommended. Review
following outcomes of ScW
investigations and links to the
Dalmuir System Plan. 
Duntocher
Road
Road gully
maintenance
Flood incident
records
Update emergency response
planning with new pluvial flood
information
Support ongoing ScW
investigations into the unnamed
Review strategic opportunities
once ScW investigations are
complete; reassess hotspot-
specific options in the context
of wider catchment

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watercourse, sewer connectivity
and drainage interactions; continue
runoff reduction strategy and
stakeholder collaboration.
management and sewer
constraints.
Livingstone
Street 
Road gully
maintenance
Flood incident
records
Update emergency response
planning with new pluvial flood
information
Continue coordination with ScW
investigations into historic drainage
features and sewer interactions;
maintain records of flooding and
access disruption; continue runoff
reduction strategy where
appropriate.
Review previous options
alongside ScW investigation
outcomes. Prioritise measures
delivering sewer and surface
water benefits through a
collaborative catchment
approach.
Melbourne
Avenue
Road gully
maintenance
Flood incident
records
Update emergency response
planning with new pluvial flood
information
Continue coordination with ScW
due to significant sewer flooding
mechanism; improve maintenance
of local drainage assets; continue
runoff reduction strategy where
appropriate.
Review existing options in
conjunction with ScW
investigations and wider sewer
catchment constraints before
progression.
Low Crescent Road gully
maintenance
Flood incident
records
Update emergency response
planning with new pluvial flood
information
Continue monitoring of flooding
incidents; review interaction of
sewer, pluvial and fluvial
mechanisms; coordinate with ScW
regarding sewer flooding records. 
Future option appraisal if
deemed appropriate based on
model validation against real
life data.
Dumbarton
Road
Road gully
maintenance
Flood incident
records
Update emergency response
planning with new pluvial flood
information
Continue routine maintenance and
monitor future flood incidents. 
No further hotspot-specific
option appraisal currently
recommended unless future
evidence indicates a significant
flood risk.

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Dunedin
Terrace
Road gully
maintenance
Flood incident
records
Update emergency response
planning with new pluvial flood
information
Continue routine maintenance and
monitor future flood incidents.
No further hotspot-specific
option appraisal currently
recommended given the
limited flood risk identified in
updated mapping and
modelling.
Kilbowie Road Road gully
maintenance
Flood incident
records
Update emergency response
planning with new pluvial flood
information
Continue monitoring of flooding
incidents; coordinate with ScW
regarding sewer network
performance within the wider
catchment; continue runoff
reduction strategy.
Review opportunities through
wider catchment studies and
links to the Dalmuir System
Plan before progressing
hotspot-specific measures.
Station Road Road gully
maintenance
Flood incident
records
Update emergency response
planning with new pluvial flood
information
Maintain drainage assets and
monitor interactions with adjacent
watercourse and agricultural runoff;
review emergency response
procedures given strategic
transport impacts.
Consider future appraisal of
options focused on protecting
access and transport resilience
if flooding continues to affect
the route.
Dumbarton
Road (west)
Road gully
maintenance
Flood incident
records
Update emergency response
planning with new pluvial flood
information
Continue routine maintenance and
monitoring of flood incidents.
Review only if additional
evidence of flooding becomes
available.

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8. Conclusions
AtkinsRéalis was commissioned by WDC to develop a Surface Water Management Plan (SWMP) for Clydebank
in accordance with the Flood Risk Management (Scotland) Act 2009 and the objectives of the Clyde and Loch
Lomond Flood Risk Management Plan. The initial SWMP was completed and submitted in April 2024 based on
the best available information at that time, including SEPA Flood Maps, historical flood records, stakeholder
information and hydraulic modelling outputs. Since completion of the original assessment, additional information
has become available through the publication of the 2025 SEPA Flood Maps, the December 2025 stakeholder
workshop, subsequent engagement with key stakeholders and ongoing ScW investigations. This report has
therefore revisited the original SWMP findings to review how this new information influences the understanding
of flood risk, flooding mechanisms, hotspot prioritisation and future flood risk management recommendations
across the Clydebank catchment.
The review has demonstrated that the updated 2025 SEPA Flood Maps have reduced the extent of predicted
surface water flood risk at several locations across Clydebank. As a result, a number of hotspots identified during
the original assessment would no longer satisfy the original hotspot screening criteria if assessed using the
updated mapping alone. However, the review has also demonstrated the importance of considering historical
flooding records, stakeholder information and hydraulic model outputs alongside flood mapping when assessing
flood risk and prioritising investment. A comprehensive review of the 2025 SEPA Flood Maps to identify any new
flood risk hotspots has not been undertaken as part of this study. Future work should consider whether additional
hotspots are warranted, taking into account the updated mapping and any reported flooding incidents since
completion of the original SWMP.
The desktop assessments, hydraulic modelling and stakeholder engagement have shown that flood risk within
Clydebank is strongly influenced by the interaction between surface water runoff, sewer network exceedance,
watercourses and other drainage infrastructure. Whilst pluvial flooding remains an important component of flood
risk at some locations, the updated assessment indicates that sewer flooding is a significant contributor to flood
risk at many of the priority hotspots, including Second Avenue / Ramsay Street, Western Isles Road, Duntocher
Road, Livingstone Street, Melbourne Avenue and Low Crescent. In several locations, substantial volumes of out-
of-sewer flooding were predicted, indicating that constraints within the Dalmuir sewer catchment are a key
influence on the overall flooding mechanism.
Table 8-1 summarises the outcome of the hotspot reassessment, including consideration of the 2025 SEPA Flood
Maps, the principal flooding mechanisms identified at each location, and any discrete mitigation options identified
through the initial Surface Water Management Plan (SWMP). The review has been undertaken in the context of
the strategic approach to flood risk management recommended for the study area, recognising that while
individual options may provide localised benefits, their effectiveness should be considered alongside wider
catchment-scale interventions and opportunities across the drainage network.
Table 8-1 – Summary of hotpots
Hotspot
Name   
2025 SEPA Flood
Map Reassessment
Root Cause
Summary No Location Option
Second
Avenue/
Ramsey
Street
Continues to meet
criteria for surface
water flood risk
Combined sewer
flooding resulting
from limited sewer
capacity,
exacerbated by
surface water runoff
from the surrounding
catchment.
1a Park Road
Attenuation
basin at
junction 
2b
Second Avenue
(stretch between Park
Road and St
Stephen’s Primary
School)
Attenuation
at school
4 Duntocher Road
(Option 1 in the SuDs Basin

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Duntocher Road
Hotspot)
Western
Isles Road
Continues to meet
criteria based on
impact on roads
although no
properties impacted
Flooding is
understood to be
primarily driven by
surface water runoff
exceeding local
drainage capacity.
3 Western Isles Road Roadside
swales  
Duntocher
Road
Continues to meet
criteria based on
impact on roads
although no
properties impacted
Sewer flooding
associated with
capacity exceedance
in the drainage
network,
exacerbated by
surface water runoff
from the upstream
catchment.
1
In grassy area
immediately west of
the Kilbowie
Roundabout (between
the A82 and
Duntocher Road)
SuDs Basin
Livingstone
Street
No longer meets
hotspot criteria, being
investigated by ScW
Sewer flooding
resulting from
capacity exceedance
within the combined
network, with
contributions from
surface water runoff
and a potential fluvial
inflow into sewer
network being
investigated.
1 Grassy verge south of
Livingstone Street SuDs Basin
Melbourne
Avenue
Continues to meet
criteria based on
impact on roads
although no
properties impacted
Sewer flooding
associated with
limited drainage
capacity,
exacerbated by
surface water runoff
conveyed along local
overland flow routes. 
2
Melbourne Avenue 
Swale and
geocellular
storage  
Low
Crescent
No longer meets
hotspot criteria 
Sewer flooding
associated with
limited drainage
capacity, some
surface water and
fluvial influence
Not selected for options appraisal
Dumbarton
Road
No longer meets
hotspot criteria
No longer perceived
to be at risk based
on information
available
Not selected for options appraisal

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Dunedin
Terrace
No longer meets
hotspot criteria
No longer perceived
to be at risk based
on information
available
Not selected for options appraisal
Kilbowie
Road
Continues to meet
criteria due to impact
on commercial
properties
Surface water
flooding primary
driver, with potential
sewer flooding
upstream of hotspot
Not selected for options appraisal
Station
Road
Continues to meet
criteria based on
impact on critical
roads although no
properties impacted
Surface water with
potential rural
upstream influence
Not selected for options appraisal
Dumbarton
Road
(west)
Continues to meet
criteria based on
impact on critical
roads although no
properties impacted
Surface water with
potential rural
upstream influence
Not selected for options appraisal
The stakeholder workshop and subsequent discussions with ScW highlighted several uncertainties relating to
drainage connectivity, sewer performance and the interaction between historic watercourses and the combined
sewer network. In particular, ongoing investigations at Duntocher Road and Livingstone Street have identified
important data gaps that may influence the understanding of flood mechanisms and the relative contribution of
sewer flooding at these locations. Consequently, the findings of the hydraulic modelling should be interpreted
alongside the identified model limitations and reviewed as the outcomes of ongoing investigations become
available.
The review also highlighted that many of the flood management options developed as part of the original SWMP
were based on a more limited understanding of flood risk and were assessed as discrete hotspot-specific
interventions. Since completion of that work, the improved understanding of flood mechanisms, together with
ongoing investigations within the Dalmuir sewer catchment, has demonstrated that many flooding issues are
linked through wider catchment processes and sewer network constraints. As a result, the original options and
associated modelled benefits should be treated with caution and are considered to have been superseded by the
improved understanding of flood risk now available.
Overall, the findings of this SWMP indicate that many flood risk issues within Clydebank cannot be resolved
through isolated local interventions alone. A coordinated and collaborative catchment-wide approach is therefore
recommended, bringing together WDC, ScW, SEPA, Network Rail, Scottish Canals and other stakeholders to
develop integrated solutions that address both surface water and sewer flooding mechanisms and deliver
sustainable long-term flood risk management outcomes.
8.1 Recommendations
This section summarises Further Actions and Stakeholders Engagement stage of SWMP. 
Given the ongoing investigations being undertaken by ScW and the improved understanding of flood mechanisms
developed through this review, it is recommended that the findings of this study are used as a strategic evidence
base to support future partnership working and development of integrated flood risk management solutions
across Clydebank. The following recommendations are proposed:
 Continue engagement with ScW, SEPA, Network Rail and Scottish Canals to maintain the collaborative
approach established through the December 2025 workshop.

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 Review the 2025 SEPA Flood Maps to identify any additional flood risk hotspots, taking account of
reported flooding incidents.
 Consider the findings of ongoing ScW investigations and links to the Dalmuir System Plan before
progressing hotspot-specific flood alleviation measures, particularly where sewer flooding has been
identified as a significant contributor to flood risk.
 Develop a catchment-wide flood risk management strategy that considers interactions between surface
water runoff, sewer systems, watercourses, highway drainage and other infrastructure rather than
addressing hotspots in isolation.
 Review and update hydraulic models as further information becomes available regarding sewer
connectivity, historic watercourses and drainage system interactions.
 Reassess the flood management options developed as part of the initial SWMP in light of the updated
understanding of flood risk, ongoing investigations and wider stakeholder initiatives before progressing
to detailed appraisal or design.
 Undertake targeted surveys and investigations at locations where significant uncertainties remain
regarding drainage connectivity, watercourse interactions and sewer network performance.
 Continue to improve flood incident recording, GIS management and data sharing between organisations
to support model verification, future flood studies and evidence-based decision making.
 Identify opportunities to reduce flows entering the combined sewer network through retrofit SuDS,
surface water separation, blue-green infrastructure and wider runoff reduction measures.
 Update emergency planning and operational procedures using the improved understanding of flood
pathways, critical access routes and infrastructure dependencies developed through this study.
 Review the SWMP following completion of key stakeholder investigations and publication of updated
strategic studies to ensure future investment decisions are based on the most up-to-date understanding
of flood risk.
Subject to continued collaboration between stakeholders and progression of ongoing investigations, the
Clydebank SWMP provides a robust evidence base for developing a coordinated programme of flood risk
management measures that improves resilience to both surface water and sewer flooding, while supporting long-
term adaptation to future pressures including climate change

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APPENDICES

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Appendix A. Objectives
Objective 1  Action
Reference
Action Status Responsibility Implementation
Date
Avoid an increase in
surface water flood risk
in Clydebank
1A
Make sure all future development within the Clydebank area
meets planning guidance (unless special regeneration areas or
exempt areas which have been robustly justified)
Existing WDC Ongoing
Improve resilience to
flooding 1B Update emergency response planning with new pluvial flood
information New WDC 2026*
Objective 2
Improve understanding
of surface water flood
risk in Clydebank
2A
Continue to maintain and improve flood incident records and
compare observed flooding with model predictions to support
future model validation and refinement.
Existing /
Improved WDC 2024 onwards
2B
Continue collaborative working with ScW, SEPA, Network Rail
and Scottish Canals to improve understanding of flood
mechanisms and identify opportunities for joint investment, in
particular with links to the Dalmuir System Plan.
Existing /
Improved WDC 2024 onwards
2C
Support and review the outcomes of ongoing ScW investigations
into sewer flooding, drainage connectivity, historic watercourses
and flooding mechanisms across the Dalmuir catchment.
Existing WDC and ScW 2024 onwards
2D
Review and update hydraulic models as additional information
becomes available through ScW investigations, flood incidents
and future studies.
New WDC and ScW 2024 onwards
2E
Continue to improve management and sharing of GIS datasets,
including flood records, drainage assets, watercourse information
and completed improvement works.
New WDC and ScW 2024 onwards
Develop a strategic
understanding of sewer 3A Align future flood risk management activities and investment
decisions with the Dalmuir System Plan. New WDC and ScW 2026 onwards

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and surface water
interactions 3B
Investigate opportunities to reduce runoff entering the combined
sewer network through retrofit SuDS, blue-green infrastructure,
source control and surface water separation projects.  New WDC and ScW 2026 onwards
Improve understanding
of flood risk at Second
Avenue / Ramsay Street
4A
Coordinate with ScW to share information to help develop an
improved understanding of flood risk at Second Avenue and the
best solution to pursue. 
New WDC / ScW 2024 onwards
Reduce Surface Water
flood risk at Second
Avenue
4B Collaborate with ScW to realise any potential shared interests and
funding opportunities. New WDC 2024 onwards*
Improve understanding
of flood risk at Western
Isles Road
5A
Coordinate with ScW to share information to help develop an
improved understanding of flood risk at Western Isles Road and
the best solution to pursue. The existing sewer system appears to
be undersized so this should be considered.
New WDC / ScW 2024 onwards
Reduce Surface Water
flood risk at Western
Isles Road
5B Collaborate with ScW to realise any potential shared interests and
funding opportunities. New WDC 2024 onwards*
Improve understanding
of flood risk at Duntocher
Road
6A
Review flood risk and potential interventions following completion
of ScW investigations into the unnamed watercourse, sewer
connectivity and wider drainage interactions.
New WDC / ScW 2024 onwards
Reduce Surface Water
flood risk at Duntocher
Road
6B Collaborate with ScW to realise any potential shared interests and
funding opportunities. New WDC 2024 onwards*
Improve understanding
of flood risk at
Livingstone Street
7A
Review flood mechanisms and potential interventions following
completion of ScW investigations into historic watercourse
interactions and sewer network performance.
New WDC / ScW 2024 onwards
Reduce Surface Water
flood risk at Livingstone
Street
7B Collaborate with ScW to realise any potential shared interests and
funding opportunities. New WDC 2024 onwards*
Improved understanding
of flood risk at
Melbourne Avenue
8A
Continue collaboration with ScW to improve understanding of
sewer exceedance and identify opportunities to reduce flood risk
through integrated drainage management.
New WDC / ScW 2024 onwards

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Reduce Surface Water
flood risk at Melbourne
Avenue
8B Collaborate with ScW to realise any potential shared interests and
funding opportunities. New WDC 2024 onwards*
Reduce stress on
existing combined sewer
where possible when
considering new
development proposals,
retrofit schemes,
resurfacing works etc. 
9A
To support the Dalmuir System Plan, find ways to increase
capacity in the existing combined sewer in the Clydebank area by
removing surface water from this system. For example, retrofitting
SuDS, underground storage areas or creating a separated surface
water pipe system. This will have a greater impact where closer to
the flooding area. 
New WDC 2024 onwards*
Continue working with
ScW to manage internal
and external sewer
flooding
10A
Make sure all incidents of external and internal flooding of
properties and infrastructure are reported. This will keep record up
to date and help understand future flooding. New WDC 2024 onwards
10B Make sure that following an incident of sewer flooding (internal or
external) that an appropriate clean-up is undertaken. New WDC / ScW 2024 onwards*
10C
Make sure that a thorough investigation into the likely causes of
sewer flooding (both internal and external) take place.
Homeowners and business owners should be informed
New WDC / ScW 2024 onwards*
Future option
development 
11A
Reassess the options developed as part of the original SWMP
following completion of key stakeholder investigations and any
future model updates
New WDC / ScW 2026 onwards
11B Develop future options as part of a collaborative catchment-wide
strategy rather than isolated hotspot-specific schemes. New WDC / ScW 2026 onwards
*Subject to funding availability

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