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Scoping Study into the Cost of Flooding Using the August 2004 event as a case study Final Report

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2 Impacts of flooding in August 2004

Information on flooding or severe weather is held by a number of organisations and in a number of locations. Our study collected formal reports and assessed news reportage to provide a picture of the impact of flooding in August.

2.1 Formal reporting

A statutory means for the formal collection of flooding data under the Flood Prevention and Land Drainage (Scotland) Act 1997 is through the biennial reports published by Local Authorities and a review of these biennial flood reports was reported to the SEPA Conference on the 30th of September 2004 by Professor Alan Werritty 5. Scottish Executive asked the councils for information on flooding in their area and received a summary of information. This is kept in a paper file by Scottish Executive. Information is received in the biennial reports which vary substantially in format and content. Some are published documents, some web pages and some short paper reports.

The biennial reports can be of limited use in assessment of severe flood events as they only produced every two years. There can therefore be some delay in collation of flood data for an immediate assessment of a flood's impact. When severe weather events take place the SE seeks 'live' information from Local Authorities for Ministerial briefing and this information is collated in a file. It is assumed that this is then also used in the biennial reports.

2.2 Press coverage

This assessment of incidents of flooding involved a search through internet resources including local and national news and newspaper websites, SEPA flood warning website and news and through data collected by Scottish Executive during the period. This data search identified two distinct events, one in early August (9 to 13 August) and the second later on in August (18 to 22 August), a full list of flooding incidents found during this search are detailed in Appendix A and are shown in Figure 2-1 overleaf. Landslides were prevalent during both of the periods, receiving most press coverage was the landslide blocking the A9 on the 12 of August and two landslides blocking the A85 at Glen Ogle.

Table 2-1: Glen Ogle landslip after repairs pictured in early September 2004

Landslip A82 from old railway from north west

Landslip A82 from old railway from north west

Landslip on A82 from old railway from south west showing new gabions

Landslip on A82 from old railway from south west showing new gabions

The two floods had distinct distributions (Figure 2-1). Flood reports in early August were over higher areas either side of the central belt, whereas later in August the events were predominantly in the north east apart from the landslides in Glen Ogle.

During our assessment of areas flooding there was substantial reportage of roads flooding. Of note is that in the two areas where a substantial number of houses were flooded to depth there was little or no news coverage. The two sites were at Menstrie, a Clackmannanshire hillfoots settlement at the foot of the Ochils, where 30 properties flooded to depths of nearly 0.5 m, and at Pebbles on the River Tweed, where properties within an existing scheme flooded to a depth of between 0.3 and 0.6 m. At Menstrie 4 houses were flooded the day after they had been handed over by a developer and this could be considered to be reasonably newsworthy.

Table 2-2 : Location of flooding in Menstrie

Floodwater passed along Burnside Road flooding houses on the left

Floodwater passed along Burnside Road flooding houses on the left

Bridge damaged in flood, note a footbridge upstream was washed down onto this bridge

Bridge damaged in flood, note a footbridge upstream was washed down onto this bridge

Following collation of the flood incident data the following catchments were designated as target catchments in terms of SEPA hydrometric data analysis to determine the severity of the event.

  • The Don (Aberdeenshire)
  • The Tweed (Borders)
  • The Tay (Perthshire)
  • The Teith (Stirlingshire)

The greatest press coverage of flooding incidents and landslides occurred in the upland Tay and Teith catchments, but unfortunately due to time constraints prevailing on this project data was only received for the for the Don and Tweed catchments and one 15 minute instantaneous rain gauge close to the Teith catchment, hence data analyses during this study can only be based on the Don and Tweed catchments.

Figure 2-1: Instances of Flooding Scotland August 2004

Figure 2-1: Instances of Flooding Scotland August 2004

2.3 SEPA

SEPA maintain the hydrometric network and issue flood warnings as floodline and they are also responsible for producing the new flood maps for Scotland driven by Scottish Planning Policy 7 6 ( SPP7). SEPA have collated a number of historical flood maps and maintain this as a GIS dataset. Occasionally flood outlines and levels are surveyed and for the January 2005 event in some of the areas affected in August 2004 is being collected to increase the understanding of flooding. This will include flood levels on the Tweed through Peebles but not levels on the Burn that caused substantial localised flooding. Most of the flood outlines are on larger catchments and tend not to be on smaller urban catchments.

2.4 Scottish Water

Scottish Water maintains a database or register of flooding and logs calls made to its customer service line. Scottish water reported over 3000 calls in August over a normal monthly total of 500. Twice as many "incident alerts" as in any other month have also been recorded 7. This information would contribute substantially to understanding flooding particularly in urban areas. Scottish Water is predominantly focused on flooding from its own sewer network. Scottish Water is currently undertaking a detailed analysis of the flood event and a report is due in March 2005. This report is a comparison of phone logs and reports with their flooding register and will produce a measle map (incident plan with locations similar to Figure 2-1). This information will be a valuable resource in determining flooding areas.

2.5 Fire Service

Tayside Fire Brigades log for both events in August revealed there were a number of incidents across Tayside, including substantial flooding in Dundee, Bankfoot, landslides on the A9 and other flooding across the whole region in 2 events on the 11 & 16 August 8. The Fire service logs have valuable information on location but would require investigating beyond the scope of this work to ascertain the flooding details.

2.6 Observational

Substantial attention and resources was focused on the landslides on the A85, on the eastern slopes of the Glen Ogle Valley. There was also risk to local property on Lochearnhead with material blocking the bridge on the A85 at Auchraw, and threatening local houses. There were also a number of landslides on the western side of the valley which blocked and closed the new Sustrans National cycle route. The route was still being repaired in September 2004, a month after the event.

2.7 Insurers

No insurers were approached as part of this study. The insurance industry does hold information on households and businesses insured at the time of flooding. In addition at least one insurance company had its own flood map of parts of Scotland at the time of flooding and is currently extending this cover for the rest of Scotland.

2.8 RECAP Flooding Forum November Tayside

The RECAP flooding Forum Meeting Monday 29 November 2004, Council Chambers Perth and Kinross Council Perth, brought together interested parties who played an active role in the flooding incidents in August, and presentations were made by the following services:-

  • Tayside Police
  • Tayside Fire Brigade
  • Angus Council
  • Dundee City Council
  • Perth Council
  • Scottish Executive ( RNM) and BEAR
  • Scottish Water

Each party was able to clearly state their own interpretation of their role. All referred to a difficulty in communication and the co-ordination. All parties identified gaps in responsibility for flooding and that there was no body that had overall responsibility for handling the situation which arises in an extreme weather event and where widespread flooding is recorded.

2.9 Agricultural impacts

The saturated soils and wet conditions delayed harvesting and damaged crops in some areas, Figure 2-2 below shows flattened grass and sediment deposition on pasture in Glen Ogle down valley from the landslides (see Section 2.2). Despite searches made through the NFU Scotland web news archive 9 there was no apparent readily available record or sources of primary/ secondary data which would enable the agricultural inputs to be quantified geographically and quantified financially were found.

Agricultural statistics are collated by Scottish Executive where a census is undertaken each June; therefore in the case of this study no information is available as to the output from such a census on agricultural output or harvested crops until the June 2005 census.

Figure 2-2: Pasture showing flattened grass and sediment deposition

Figure 2-2: Pasture showing flattened grass and sediment deposition

2.10 Chronology of British Flood Events

The British Hydrological Society maintains a website 10 of hydrological events with data being held at the University of Dundee. This database was launched in July 1998, with the ultimate aim of bringing together all hydrological circumstances including flooding, drought and heavy rainfall.

This is an extremely useful tool and all hydrological users (from consultants, local authorities, government through to the public are encouraged to maintain input into the database.

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Page updated: Tuesday, May 17, 2005