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is not certain, but during the war weather echoes were regarded as a nuisance rather than of intrinsic value. Nevertheless, before the end of the war the Meteorological Office had established a radar research station at East Hill, some 30 miles north of London. For a time after the war, the Meteorological Office

level rise is not uniform across the UK. Sea level rise is less in the north and more in the south, this is mainly due to the movement of land, up and down. 4.2 For London, sea level rise by the end of the century (when compared to 1981-2000), for the low emission scenario is very likely 6

, up and down. 4.2 For London, sea level rise by the end of the century (when compared to 1981-2000), for the low emission scenario is very likely 6 to be in the range 0.29 m to 0.70 m.For a high emission scenario, the range is very likely to be 0.53 m to 1.15 m. 6 The IPCC use likelihood to provide

to 2100 under all emission pathways. 4.1 The pattern of sea level rise is not uniform across the UK. Sea level rise is less in the north and more in the south, this is mainly due to the movement of land, up and down. © Crown copyright 2019, Met Office Page 8 4.2 For London, sea level rise by the end

temperatures of 20.8 °C were recorded at St James’s Park (London) on the 23rd and Treknow (Cornwall) on the 25th. A minimum temperature of -9.1 °C was recorded at Aboyne (Aberdeenshire) on the 2nd. In the 24 hours ending at 0900 UTC on the 2nd, 51.6 mm of rain fell at White Barrow (Devon). A wind gust

in Northern Ireland and parts of western Scotland. The UK monthly extremes were as follows: A maximum temperature of 19.8 °C was recorded at Kew Gardens (Greater London) on the 26th. A minimum temperature of -6.9 °C was recorded at Aboyne (Aberdeenshire) on the 5th. In the 24 hours ending at 0900 GMT

especially parts of eastern England, with an overall figure of 107% of average. The UK monthly extremes were as follows: A maximum temperature of 23.4 °C was recorded at St James’s Park (London) on the 15th. A minimum temperature of -8.0 °C was recorded at Tulloch Bridge (Inverness-shire) on the 1st

on 19th at London, St James's Park (Greater London, 5mAMSL) 8.3°C on 21st at Tomintoul No 6 (Banffshire, 320mAMSL) 18.5°C on 7th at Swanage (Dorset, 10mAMSL) -5.0°C on 29th at Tomintoul No 6 (Banffshire, 320mAMSL) -6.6°C on 29th at Tomintoul No 6 (Banffshire, 320mAMSL) 87.8mm on 11th at Achnagart

the length of the Offas Dyke. During the first week, several low impact rain warnings were issued. Substantial rainfall fell across Cumbria in the opening days which may have contributed to a landslide that caused the derailment of a Glasgow to London service at Shap early on the 3rd. The next day came

of England there were reports of flooding on the 14th, affecting the A414 in Harlow, one road in Hinxton, and the entrance to Cambridge railway station, as well as property flooding in Kings Lynn. In London there were reports of flooding around Tower Bridge, and long delays on the Piccadilly line