From 1-31 March, rainfall across the Thames catchment was 183% of the 134 year historic monthly average, with 95.7mm.
Rainfall in the last year
The graph below shows the rainfall over the last year and percentage increase and decrease against the monthly average.
Where our water comes from
Across our region, we take about 65 per cent of our source water from rivers, in a process called abstraction. We then store this in large, open reservoirs (known as surface reservoirs) before putting it through our treatment process to turn it into drinking water.
The remaining 35 per cent comes from natural underground reservoirs called aquifers, from which we pump water using boreholes. This water has originally fallen as rain and sunk down into the ground in a process called recharge. These supplies from aquifers are referred to as groundwater.
Reservoir and water levels
The diagram below shows the rainfall and levels of water in the rivers, aquifers and reservoirs in our area, for the last month.
Water situation summary
On 31st March 2018, the Thames Regional Soil Moisture Deficit (SMD) total was 1mm which is lower (i.e. wetter) than expected for the time of year.
At the end of March, groundwater levels are generally Below Normal to Normal, except an area of the Cotswolds which is Exceptionally High.
River flows were generally above their long term averages in March. The Teddington Target Flow was maintained at 800 megalitres/day during March in agreement with the Environment Agency.
Reservoir storage on the 31st March 2018 for London as a whole was 96% (Thames Valley 98% & Lee Valley 89%) and Farmoor storage was 96%.