Select Committee on Environment, Food and Rural Affairs Written Evidence


Memorandum submitted by David Jones (FL 51)

REGARDING FLOODING IN ENGLAND AND WALES.

  I am a retired Chartered Civil Engineer and was affected by the recent floods in Gloucester. I worked for Gloucestershire County Council Highways Department between 1964 and 1989 and as an independent consultant thereafter until last year. During my time at the County, I worked inter alia on Development of Tewkesbury and Gloucester when Planning Policies were generated allowing building to 10.4 O.D. Some arguments for a 14.5 O.D. were overruled. Whilst an articled pupil in West London I had experience in dealing with a number of drainage matters including flood relief work along The Thames as a result of the 1947 floods. I believe there are a number of issues causing severe flooding along the Lower Severn in July 2007:

1.  Geography of The Severn Valley

  Generally the River Severn flows in a south-westerly direction against the prevailing wind.Thus a typical Atlantic Storm blows up The Severn as flood waters travel down it. This is a completely different situation to river estuaries flowing eastwards to The North Sea such as the Humber where the south-westerly air stream flows more or less with the river current. There are also differences in geology all of which may lead to individual policies for each flood plain.

2.  Building on the Flood Plain

  This is dealt with adequately under existing terms of reference of The Environment Agency but advice to Local Planning Authorities on planning applications is not mandatory.

3.  Building on areas above flood plains where rain water can be retained

  This should not be confused with (2) above. Here the ground acts as a sponge allowing slow release of surface water reducing the possibility of sudden flooding. EA comments on planning applications do not appear to deal with this matter.

4.  River and Watercourse Management

  The bed of the River Severn above Gloucester is rising possibly due to the Victorian Weirs at Gloucester which allow mud to flow up stream on a flood tide but deposits mud on an ebb tide. After the July 2007 storm the water ran off from areas above the 50 m contour very quickly. My house is in this area and there were very few problems. The nearby Gloucester Trading Estate is being developed at the present time and provision has been made to contain water already in water courses such as the Wotton Brook in a balancing tank. Inspection showed that 2 days after the flood the balancing tank was empty.

  I believe the following measures should be introduced:

    1.  The EA should have powers of direction for planning purposes.

    2.  The EA should develop policies on land for water retention above general flood levels.

    3.  Management of water courses and water flow control systems should be undertaken more vigorously.

D R Jones CEng MICE

August 2007





 
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