Exmoor rises to 520m - annual average rainfall is over 2,000mm (UK average - 920mm)
prevailing westerly winds from the Atlantic bring higher than average precipitation
geology characteristics
80% of rocks in basin are impermable
geology of catchment spans 400million years
soil characteristics
dominant soils are permable and loamy soils (48% of land area)
soils have iron pan - means water can't infiltrate through them
reducing percolation and increasing river discharge
land use characteristics
main areas of urban development are south of catchment due to flatter land
urban areas include Tiverton (not at risk of flooding)
agriculture grassland use
67% - sheep and cattle compact soil , reducing infiltration
woodland land use
13%
peat bogs land use
3%
hydrography for the river exe
flashy hydrograph
high runoff
rainfall high in rainfall season - winter
river regime
the annual variation of flow of a river
water balance for the river exe
precipitation = 1295mm
evaporation + soil water storage = 451
runoff = 844
reasons for 65% water balance
impermable nature of bedrock reduces percolation and base flow
drainage ditches is on Exmoor reduced the amount of soil water storage
plant water availability
evapotranspiration rates exceed rainfall inputs in lowland Devon during April - September
this can lead to periods of water stress on less water retentive loamy soil e.g heathlands of East Devon
what is peat?
Decomposed plant material. Accumlates faster than it decomposes due to lack of oxygen in waterlogged plants
what is Peatland restoration?
drainage ditches have been dug in peat bogs of Exmoor to make it more sustainable for farming - increases speed of water flow to River Exe , potential water surplus
what is the Exmoor Mires Project?
the project works to restore peat bogs by blocking drainage ditches with peatbogs or moorland bales.
aims of the Exmoor Mires Project
to restore 2000ha of Exmoor to boggy conditions that would be naturally present in order to help retain carbon within the peat.
pros of the Exmoor Mires Project
more water storage in upper catchment - ensures steady supply of water all year round
improved water quality - slower throughflow means that less sediment is carried back to river. Reduce channel storage , increased groundwater store
improved biodiversity - 31% has been restored to OG ecohydrological function
carbon storage , research (Uni of Exeter) , Bogstacle course
cost of Exmoor Mires Project
cost £4.5 million
2015 - 1000ha of Peat Moorland had been restored
reduction in daily surface runoff due to peatland restoration
66%
what is Wimbleball Reservoir?
in 1979 , an upland tributary of the River Exe (the River Haddeo) was dammed to create Wimbleball reservoir
surface area of Wimbleball reservoir
150ha
a reservoir is an artificial lake
pros of Wimbleball reservoir
important water store - reduces water stress in summer months
crucial impact on this part of catchment - regulates flow
reduces likelyhood of flooding - 1960 , 2500 homes flooded and in 1992 - 2,000 flooded
cons of wimbleball reservoir
in 2022 after extreme heatwaves - reservoir was 45% full
could have resulted in increased water stress and the water flow would be disrupted - risk of drought