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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

at 0900 UTC 30.1°C on 1st at Cambridge, Botanic Garden (Cambridgeshire, 13mAMSL) 7.3°C on 27th at Balmoral (Aberdeenshire, 283mAMSL) 18.8°C on 2nd at London, St James's Park (Greater London, 5mAMSL) -3.0°C on 25th at Tyndrum No 3 (Perthshire (in Central Region), 168mAMSL) and Braemar No 2

Minimum Lowest Minimum Lowest Grass Minimum Most Rainfall Most Sunshine Highest Gust Highest Gust (mountain*) Greatest Snow Depth at 0900 UTC 30.1°C on 1st at Cambridge, Botanic Garden (Cambridgeshire, 13mAMSL) 7.3°C on 27th at Balmoral (Aberdeenshire, 283mAMSL) 18.8°C on 2nd at London, St James's

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

University, Stockholm, Sweden. Dept. of Environmental and Geographical Science, University of Cape Town, Cape Town, South Africa. Downing College Cambridge, Cambridge, UK. Earth Sciences Division, NASA GSFC, Greenbelt, MD, USA. Earth Sciences, University College London, London, UK. Environment

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 reports of several road closures in west Cumbria due to surface water flooding. Parts of Wales were also notably wet during

at 0900 UTC 30.1°C on 1st at Cambridge, Botanic Garden (Cambridgeshire, 13mAMSL) 7.3°C on 27th at Balmoral (Aberdeenshire, 283mAMSL) 18.8°C on 2nd at London, St James's Park (Greater London, 5mAMSL) -3.0°C on 25th at Tyndrum No 3 (Perthshire (in Central Region), 168mAMSL) and Braemar No 2

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

of 114% of average. The UK monthly extremes were as follows: A maximum temperature of 22.9 °C was recorded at Kew Gardens (Greater London) on the 29th. A minimum temperature of -3.8 °C was recorded at Aboyne (Aberdeenshire) on the 15th. In the 24 hours ending 0900 UTC on the 5th, 102.6 mm of rain fell

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