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Temperature, Mean (tas) °C 4 4 4 4 hourly 4 Temperature, minimum (tasmin) °C 4 4 4 4 Water Balance variables 4 4 Wind gusts (wsgmax10m) m/s 4 hourly Wind speed (sfcWind) m/s 4 4 4 hourly 4 Wind speed eastwards/ northwards (uas/vas) m/s 4 4 4 4 Time steps Data set dependent Monthly Seasonal Annual
, S Proud, FV Thom. SS Arakaka: SL Portass, PWH Short, RHR Wrighton. Figure 19. The steamer SS Arakaka, torpedoed on 22 June 1941 with the loss of all hands. 4 The number of ocean weather stations maintained by the US and the UK did increase but only very slowly. By the end of May 1945 there were 16
on historical investigations of cloud seeding during the early 1950's. Q- Reports/studies on geo-engineering. A- The list below includes publications that Met Office researchers have led and those that Met Office researchers have contributed to as co-authors. Our contribution to this research
at the equator). Precipitation information was taken from the CHIRPS (Climate Hazards Group InfraRed Precipitation with Station data) dataset (Funk et al., 2015) which is available to download from: http://chg.geog.ucsb.edu/data/chirps/. The data spans 50°S to 50°N in a band around the equator
February 1967 to 17 March 1969. Extremes of wind Wind: the (horizontal) movement of air relative to the rotating surface of the Earth. The Met Office measures the wind speed in knots. The knot is defined as a speed of one nautical mile per hour. 1 knot = 0.51444 m s -1 = 1.15078 mile h -1 = 1.853 km
members are also members of the Executive Board and are Met Office employees: • R. Varley, Chief Executive • J. Slingo, Chief Scientist (until 31 December 2016) • S. Belcher, Chief Scientist (from 1 January 2017) • N. Jobling, Chief Financial Officer • S. Noyes, Deputy Chief Executive (previously
requests due acknowledgement and a copy of the publication. For online use, we ask readers to link to the original resource on the ODI website. The views presented in this paper are those of the author(s) and do not necessarily represent the views of ODI. © Overseas Development Institute 2018. This work
morphology • Vertical velocities within updrafts • Cold pool representation Colours show radar reflectivity, dashed contours are w > 4m/s (courtesy Liam Till, Thorwald Stein). CoMorph properties for scale-aware behaviour Mike Whitall • Implicit detrainment term gives smooth timestep behaviour
contexts. Support to WISER Fund Management, to build on learning from WISER 2’s Partner Learning Event to focus on: • Development and use of a Sustainability Toolkit to enable WISER to better understand whether the outcomes and key results of Phase 1 projects and the national project in Uganda
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