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The basic climate of the UK annually is wet and cool in winter, spring, and autumn with frequent cloudy skies, and drier and cool to mild in summer. The climate in the United Kingdom is defined as a humid temperate oceanic climate , or Cfb on the Köppen climate classification system, a classification it shares with most of north-west Europe. [ 1 ]
Highest monthly total (UK national average) [11] 266 hours UK (national average) May 2020 Highest monthly total (England) [2] 383.9 hours Eastbourne, Sussex: July 1911 Highest monthly total (Northern Ireland) [2] 298 hours Mount Stewart, County Down: June 1940 Highest monthly total (Scotland) [2] 329.1 hours Tiree, Argyll & Bute: May 1975
In 2004-2006, a partial drought caused fires to break out throughout the south of Great Britain, and water restrictions were introduced in some areas. The drought problems were solved due to the unusually wet period between October 2006 and July 2007, which had higher than average rainfall. The year 2006 was an unusually warm one.
This was the wettest day at the observation site in 38 years. Typically, the entire month of J. Drenching thunderstorms soaked London on Monday, with parts of city seeing the region's heaviest ...
London on a snowy day in 2018. According to the Köppen climate classification, London has a temperate oceanic climate (Cfb). [1] This type of climate features cool winters with frequent cloudy skies and rain showers (and on occasion snow), and mild summers.
The months with the most rainfall are in autumn and winter. Monthly rainfall can be variable. On the coast, most months have recorded less than 20 millimetres (0.79 in) and, some months, less than 10 millimetres (0.39 in) at some point. The wettest station of the region, Princetown, has recorded 7 millimetres (0.28 in) of rain during May. [4]
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The wet season in lands bordering the Mediterranean lasts from October through March, with November and December typically the wettest months. Summer rainfall across the continent evaporates completely into the warm atmosphere, leaving winter precipitation to be the source of groundwater for Europe. [ 36 ]