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• wafc-sigwx-verification-v1.0.pdf

  a frequency bias <1) would indicate too few objects were forecast. The top right hand corner indicates a perfect forecast (the highest possible Critical Success Index). Figure 5 shows that the new WAFS SIGWX icing forecasts are well matched to the observations. There is a slight under-forecast of lower

• factsheet_9_weather_extremes_october2025pdf

  June 1957 July 40.3 °C Coningsby (Lincolnshire) 19 July 2022 August 38.5 °C Faversham (Kent) 10 August 2003 September 35.6 °C Bawtry – Hesley Hall (South Yorkshire) 2 September 1906 October 29.9 °C Gravesend (Kent) 1 October 2011 November 21.1 °C Chelmsford (Essex) Clacton (Essex) Cambridge

• mwr_2025_01_for_print_v1.pdf

  variation, with some areas experiencing much heavier rainfall. England, and in particular southern England, saw over 100% of the average rainfall, while Scotland and Northern Ireland saw around half the average rainfall. Nottinghamshire and South Yorkshire recorded nearly 150% of the average rainfall

• mwr_2025_01_for_print_v1pdf

  variation, with some areas experiencing much heavier rainfall. England, and in particular southern England, saw over 100% of the average rainfall, while Scotland and Northern Ireland saw around half the average rainfall. Nottinghamshire and South Yorkshire recorded nearly 150% of the average rainfall

• ukcp18--marine-report--march-2019-update.pdf

  “jigsaw puzzle” including the various components that are represented in the UKCP18 sea level projections. The schematic summarises the major contributors to changes in: global time-mean sea level (left-hand column); regional sea level (middle column); and local sea level and extremes (right-hand column

• ukcp18--marine-report--march-2019-updatepdf

  “jigsaw puzzle” including the various components that are represented in the UKCP18 sea level projections. The schematic summarises the major contributors to changes in: global time-mean sea level (left-hand column); regional sea level (middle column); and local sea level and extremes (right-hand column

• wiser0243_environmental_psychology_working_paper.pdf

  (temporal distance) and remote locations (spatial distance). Literature from the global north has often documented climate change as a psychologically distant threat. In turn, the psychological distance of climate change is often cited as a reason that people do not act on climate change (Lorenzoni

• ukcp18-factsheet-local-2.2km.pdf

  and flash flooding Influence of North Atlantic Oscillation (NAO) Daily precipitation extremes in winter Severe convective wind gusts Positive (NAO) LOW HIGH Influence of North Atlantic Storm Track Urban changes Figure 1 Schematic of the spatial resolution of UKCP18 climate models and the implications

• corporate_brochure.pdf

  area 14 area 15 area 16 area 17 01.53 GMT: MetOp-A, Europe’s first polar-orbiting meteorological satellite, is 850 km above the North Atlantic and travelling at 7 kilometres per second. Making around 14 circuits over the next 24 hours, it will view each part of the Earth at the same local time each

• remember_world-war-one-and-two_2023.pdf

  the Gallipoli Front, Macedonia Front, Italian Front, North Russian Front, Independent Force RAF and a Home Unit with its headquarters on Salisbury Plain to meet the requirements of the Army. In 1918 all of these sections were brought under the title of the Army Meteorological Service. At the end