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01640_supercomputer_infographic

Advance global resilience and security Better informed risk assessments for the UK’s resilience to flooding in the changing climate Improving efficiency in weather sensitive operations such as within utilities and aviation To inform climate and weather models and forecasts Amounting to billions of £s

jcliD1400808 7470..7488

: Physiographically sensitive mapping of climatological temperature and precipitation across the conterminous United States. Int. J. Climatol., 28, 2031–2064, doi:10.1002/joc.1688. Deser, C., R. Knutti, S. Solomon, and A. S. Phillips, 2012a: Communication of the role of natural variability in future

met-office_climate-change-impacts-for-ukraine_report_08dec2021_english.pdf

135 0000 Recommended citation: Wilson, L., New, S., Daron, J., Golding, N. (2021). Climate Change Impacts for Ukraine. Met Office. Image credits: Front cover The Southern Bridge across the Dnieper in Kiev, the capital of Ukraine. (Shutterstock 1178833933). Page 8 Kamenets-Podolsky, Ukraine-MAY 19

mounkaila15wafricacordexrainonsets.compressed.pdf

Theor Appl Climatol (2015) 119:255–272 DOI 10.1007/s00704-014-1104-4 ORIGINAL PAPER Assessing the capability of CORDEX models in simulating onset of rainfall in West Africa Moussa S. Mounkaila & Babatunde J. Abiodun& J. ‘Bayo Omotosho Received: 15 August 2013 /Accepted: 23 January 2014 /Published

UK climate extremes

19 July 2022 Cambridge, NIAB England SW 36.0 18 July 2022 Bude (Cornwall) Wales S 35.8 18 July 2022 Gogerddan (Ceredigion) England SE & Central S 40.2 19 July 2022 Heathrow (London) England SE & Central S 40.2 19 July 2022 St James's Park (London) Lowest daily minimum temperature records District

September 2011 Sea Ice Outlook

., Fereday, D., Camp, J., Scaife, A.A., Xavier, P., McLean, P., Colman, A., and Cusack, S, 2011: The GloSea4 ensemble prediction system for seasonal forecasting, MWR, DOI: 10.1175/2011MWR3615.1. To be published in June 2011 issue MWR, 139(6), pp. 1891-1910. Bowler, N.E., A. Arribas, S. Beare, K. Mylne and G

The Future is Small

– Differential fluxes of electrons and ions range 10 5 – 10 9 /cm2/sr/keV/s shall be able to be measured. – Time resolution for a complete measurement over all energies and both species shall be able to be commanded to less than 30s – Total mass of all sensors plus electronics shall be < 0.5kg L5 Consortium

Frank_Colberg_ppt

static members (interpolated from ORCA025 system) • 3-day cycle system Atmosphere • ERA5 atmospheric forcing Observations • SLA (remote, L2P) Sentinel-3A, Sentinel-3B, Cryosat-2, Jason-3, Saral (RADS); • SST (remote, L2P) VIIRS-NPP, VIIRS-N20 (NOAA), AMSR-2 (JAXA), AVHRR-MTA,AVHRR-MTB (NAVO) • T,S

uk_annual_mean_temperature_cmip6_attribution_v1.pdf

accounting for differences in model ensembles, method and emissions scenarios is beyond the scope of this report. © Crown copyright 2024, Met Office Page 9 of 10 References Christidis, N., P. A. Stott, A. Scaife, A. Arribas, G. S. Jones, D. Copsey, J. R. Knight, and W. J. Tennant, 2013: A new

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