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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

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

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

and in central and eastern Scotland. The UK monthly extremes were as follows: A maximum temperature of 33.4 °C was recorded at Heathrow (London) on the 25th. A minimum temperature of -1.9 °C was recorded at Tulloch Bridge (Inverness-shire) on the 8th. In the 24 hours ending at 0900 GMT on the 29th, 212.8

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

, 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

observations of the weather in the London area and is credited with having first discovered the concept of the urban heat island, where night time temperatures in the cities do not fall as low as those in the countryside. He attributed this to the numbers of coal fires burning in close proximity

Increase in tropical cyclone risk to coastal regions Also known as hurricanes in the North Atlantic and typhoons in the northwest Pacific, tropical cyclones have maximum wind speeds of at least 74 miles per hour and can be up to 1000 kilometres in diameter. Research by Imperial College London as part

, Liverpool, UK 2 King’s College, London, UK 3 University of Southampton, UK www.metoffice.gov.uk Contents Summary ������������������������������������������������������������������������������������������������������������������������������������������������������������������������������������ 3 1.1