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-spread application of the models. Key aims To develop high quality globally applicable regional climate models (s). To understand and demonstrate how to apply s to derive regional climate information. To demonstrate the quality of s and their applicability for studying extreme events and projected

is open to UK operating and registered organisations only. Call Reference: Expression of Interest for: Grant Funds for the Period: WCSSP South Africa FY25/25 Grant Funding Opportunities (DN699573) WCSSP South Africa 1 st May 2024 – 31 st March 2025 Funding is initially available to cover a 1-year

ICON – TOWARDS (VERTICALLY) INTEGRATED EARTH SYSTEM MODEL FOR NUMERICAL WEATHER FORECAST, CLIMATE PREDICTIONS AND PROJECTIONS WA Müller, R Potthast (DWD), B Früh (DWD), P Korn 2nd J u n e 2 0 2 5 , S e a m l e s s GCM , B r i s t o l VERTICAL INTEGRATION • ICON (Icosahedral Nonhydrostatic) • All

in military planning, from the timing of D-Day to the movement of troops and supplies. As such, forecasts became top secret. Dr Catherine Ross, library and archive manager at the Met Office, said: “Forecasting stopped at the announcement of the outbreak of war because your weather observations are really

on climate model parameters Developing the next standard configuration for standalone JULES using a benchmarking system based on ModelEvaluation.org Towards a seamless cloud fraction scheme for Unified Physics 17:00 Close Catherine Hardacre Kunal Ghosh Heather Rumbold Paul Barrett University

for standalone JULES using a benchmarking system based on ModelEvaluation.org Towards a seamless cloud fraction scheme for Unified Physics Catherine Hardacre Kunal Ghosh Heather Rumbold Paul Barrett University of Canterbury University of Leeds Met Office Met Office Agenda - Seamless Global Modelling

After a warm week in which we saw the hottest April day since 1949 with 29.1°C recorded at St James’s Park in London, the warm conditions are forecast to stretch into the weekend, albeit at not quite the same intensity. There were a number of weather station records set stretching from Yorkshire

) the “rainfall accumulation from convection” must be added to this to get the total rainfall accumulation. Pa 1 None m s-1 1e-09 None m s-1 1e-09 None m s-1 1e-09 None m s-1 1e-09 None m s-1 1e-09 None m 1e-06 None rainfall_ accumulation- PT03H rainfall_ accumulation- PT06H precipitation_ accumulation-PT01H

deposited on the surface in the previous hour. For the Global models (which run a convection scheme) the “rainfall accumulation from convection” must be added to this to get the total rainfall accumulation. Pa 1 None m s-1 1e-09 None m s-1 1e-09 None m s-1 1e-09 None m s-1 1e-09 None m s-1 1e-09 None m

3dp 1dp 1dp 1dp 1dp Wspd 'Instantaneous' (10min mean) 10m Wind Speed m/s 1dp Wdir Gust MxGust 'Instantaneous' (10min mean) 10m Wind Direction 'Instantaneous' (Max 3s mean in 10min) 10m Wind Gust Maximum Gust (Max 3s mean) in previous hour Wx Predominant Weather Symbol or Type Code Int Vis