Portsmouth Water has no large raw water storage reservoirs. It relies almost entirely upon groundwater reserves in the chalk aquifers of the South Downs and abstracts its raw water from wells, boreholes and springs. It has one river abstraction at Gaters Mill on the River Itchen, a chalk river with a groundwater baseflow.
Those reserves rise and fall with the seasons and so Portsmouth Water pays particular attention to the local hydrogeological data by monitoring rainfall at its Havant Offices, groundwater levels in the chalk at Idsworth on the Hampshire/Sussex border, as well as the total yield from the natural springs at Havant and Bedhampton.
These resources are monitored on a daily basis and reported upon on a monthly basis. The information here is therefore at times one month behind the most current situation.
The information gathered is reproduced here for information purposes; no guarantee is given as to its accuracy.
The Rainfall Records at the Company’s Head Office at Havant date back to 1886.
The month of January saw rainfall levels the same as the long term average rain for the month. Rain fell on 67% of the days, with the maximum daily rainfall approximately 15mm on Sunday 14 January 2018.
Total rainfall for the month was 88mm, the same as the 30 year long term average.
The Company has groundwater records from the Idsworth Estate Well, north of Rowlands Castle, which date back to 1931. Water levels in the Well, which is entirely unaffected by abstraction, give an accurate indication of the groundwater reserves of the South Downs. In the winter, levels usually rise in response to rainfall, whilst during the summer, levels recede as any summer rainfall either evaporates or is taken up by trees and plants before reaching the aquifer below. Levels can fluctuate by as much as 20m.
The Groundwater level is usually recorded in metres AOD (Above Ordnance Datum), Ordnance Datum principally being equivalent to sea level.
Despite the dry winter of 2016/17, ground water remained within the “normal” levels for the spring of 2017. During the summer, levels fell to a “low” level, but recovered to “normal” levels by the end of August 2017.
It is normal to see ground water levels recover in the autumn as rainfall increases. September and December rainfall was above average and October and November below with January being the same as the LTA. Cumulative rainfall for the five months being approximately 83% of the long term average which has seen levels increase, but remaining 1.0m below the long term average at the end of January and remaining within “normal” levels.
So long as rainfall remains close to average for the remaining winter and spring, we do not see the need for drought control measures for the summer of 2018, such as temporary use bans. We would encourage all customers to continue to use water wisely.
The graph below shows the change in groundwater level over the last twenty four months compared to the Long Term Average (last 30 years).