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gc-seamless-workshop-agenda.pdf

for DYAMOND-3 at convection-permitting resolution GC's regional sister at km-scale: towards an RC configuration James Bassford Richard W Jones Juan Castillo 10:40 Coffee break + Poster Session 4&5 University of Leeds Met Office Met Office 11:00 The ParaChute Programme Alison Stirling Met Office 11:20 11

gc-seamless-workshop-agenda-3.pdf

configuration Annelize Van Niekerk James Bassford Richard W Jones Juan Castillo 10:40 Coffee break + Poster Session 4&5 ECMWF University of Leeds Met Office Met Office 11:00 The ParaChute Programme Alison Stirling Met Office 11:20 11:40 Modifying CoMorph-A for kilometre-scale resolutions. Interaction

trd---climate-risk-report-for-sea---v2-final.pdf

geographical regions (zones) which were determined using the following criteria: • Similar climate characteristics e.g., timing of rainy seasons or similar seasonal temperatures (see TRD Section C for further detail on Köppen-Geiger climate classifications). • Zone size was tailored to the resolution

western-scotland_-climate-met-office.pdf

of Stirling) on 12 July 1911. The variation of mean daily maximum and minimum temperatures month by month, together with the highest and lowest temperatures recorded, is shown for Paisley and Tiree. An 'air frost' occurs when the temperature at 1.25 metres above the ground falls below 0 °C, whereas

trd---climate-risk-report-for-csa---v4-final.pdf

risks. Climate has been analysed for distinct geographical regions which were determined using the following criteria: • Similar climate characteristics e.g., timing of rainy seasons or similar seasonal temperatures (please see TRD Section E for more detail on Köppen-Geiger climate classifications

metoffice_sipn_2018_june_arctic.pdf

. Vosper, H. Wells, K. Williams, N. Wood, T. Allen, A. Bushell, D. Copsey, P. Earnshaw, J. Edwards, M. Gross, S. Hardiman, C. Harris, J. Heming, N. Klingaman, R. Levine, J. Manners, G. Martin, S. Milton, M. Mittermaier, C. Morcrette, T. Riddick, M. Roberts, C. Sanchez, P. Selwood, A. Stirling, C

williams15victoriabasinrcmperformance.pdf

parametrisations struggle with the diurnal cycle of precipitation (Stephens et al. 2010; Stratton et al. 2012; Stirling and Stratton 2012). Model tropical convection over land tends to initiate too early in the day and peak in the early afternoon, rather than in late afternoon/early evening

uk_monthly_climate_summary_201802.pdf

) and a maximum of 12.8 °C at Drumnadrochit (Inverness) and Grangemouth (Stirling), with patchy rain and drizzle in the east slowly clearing during the a ernoon; more rain and drizzle moved into the west in the a ernoon. Dry and mostly sunny on the 20th with showers for the north and west. 21st to 28th Dry

uk_monthly_climate_summary_201906.pdf

to lightning strikes. The worst hit areas were the Craigavon and Newry areas. Road, rail, tram and airport services were disrupted in Edinburgh. In Stirling, a number of roads were closed due to flooding, including the M9. Power outages were reported across Tayside, Aberdeen and Dundee

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