The River Thames is now 5 miles shorter as its supply dries up as a result of drought.
The Thames Head close to Cirencester, Gloucestershire has dried up what’s believed to be the primary time ever as drought circumstances and excessive weather proceed to impression elements of the UK.
On Thursday, the Met Office confirmed that temperatures are forecasted to rise within the coming week with little rain anticipated.
Dr Rob Collins, director of coverage and science on the Rivers Belief, mentioned the supply of the river has now shifted downstream from Cirencester to Somerford Keynes, Gloucestershire.
“Following the extended dry climate, the supply of the Thames in Gloucestershire has dried up, with a weak circulation now solely nearly discernible greater than 5 miles downstream,” Dr Collins informed The Guardian.
“Beneath our altering local weather we will anticipate the frequency and severity of such durations of drought and water shortage to accentuate, with growing competitors for a dwindling useful resource and devastating impacts on aquatic life.”
This comes as Thames Water warns of a hosepipe ban for patrons within the coming weeks, because the provider says their demand has reached its highest ranges in 25 years as a result of extraordinarily dry climate.
Different water suppliers, equivalent to South East Water, have already launched a hosepipe and sprinkler ban from 12 August for patrons in Kent and Sussex.
Southern Water additionally introduced a ban final week for patrons within the Isle of Wight and Hampshire.
Met Workplace chief forecaster, Steve Willington, warned of extra excessive climate circumstances within the coming week.
He mentioned: “We may see elements of the UK getting into heatwave circumstances if the above-average temperatures final for 3 days or extra.
“Because the excessive strain builds there’s little or no significant rain within the forecast, particularly in these areas within the south of England, which skilled very dry circumstances final month,” he added.
“Elsewhere within the UK, equivalent to in northern England, Scotland and Northern Eire, rain-bearing climate fronts will make restricted headway towards the excessive strain, bringing some rain to northwestern elements of the UK.”