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• May 2026 temperature records verified

  -by-minute analysis of the figures reported and a meteorological summary of the day’s conditions to check alignment in what was meteorologically possible and what was observed. In addition, data is compared with nearby readings to ensure its feasibility and that it is representative of what occurred

• Microsoft Word - high-impact-low-likelihood-scenarios-for-the-uk-summary_final

  High-impact lowlikelihood climate scenarios for the UK Summary N.W. Arnell 1 , E. Hawkins 2 , T.G. Shepherd 1 , I.D. Haigh 3 , B. Harvey 2 , L. Wilcox 2 , L. Shaffrey 2 & A.G. Turner 1,2 1 Department of Meteorology, University of Reading 2 National Centre for Atmospheric Sciences, University

• uk_synop_station_list_-_cdl_climate_data_logger_numbered_stations_jul24pdf

  PATELEY BRIDGE, RAVENS NEST 259 54.07041 -1.77147 ENG 2000 99178 NORMANBY HALL 47 53.63689 -0.65941 ENG 1993 99179 NANTWICH, REASEHEATH HALL 40 53.08618 -2.52602 ENG 1895 99180 EDINBURGH, ROYAL BOTANIC GARDEN NO 2 28 55.96656 -3.21234 SCO 1926 99182 FRITTENDEN 38 51.14177 0.5957 ENG 2011 99183 READING

• Mini heatwave or is snow on the way? Weather headline review

  about how snow is forecast in the UK. Find out how to assess the forecast you’re reading in online news. Find a forecast for your area via the Met Office online now. Or explore more in-depth meteorological analysis on Met Office YouTube. More by Press Office Connecting climate science to local

• PowerPoint Presentation

  and Their Impact on Malaysian Rainfall during Northeast Monsoon: A Climatology Study, Fadilla et. Al, RMetS, 17 August 2019 https://doi.org/10.1002/met.1836 • Visit by MET Malaysia’s Officer Mr. Diong)National Centre for Atmospheric Science (NCAS) at the University of Reading from 11 – 28 February 2019. • Two

• Evolution for Met Office colour scales

  .   As always, temperatures that appear in public Met Office forecasts are air temperatures. This is the reading of a temperature inside a Stevenson screen at a height of 1.25m above the surface.  More by Met Office How accurate was the Met Office during winter’s weather? ‘AI enables collaboration

• richard-jones---k-scale-year-long-global-um-simulations-for-dyamond-3-at-convection-permitting-resolution.pdf

  n1280 GAL9 n1280 CoMA9_TBv1p2 n1280 GAL9 n1280 CoMA9_TBv1p2 n2560 RAL3 OBS OBS n2560 RAL3 CTC 4.4 km CTC 4.4 km Pier Luigi Vidale (NCAS, Uni of Reading) First looks from WCRP global km-scale hackathon RAL3.3 n2560 241K brightness T tracked MCS centroid GAL9 n1280 Shading is the difference between

• ESWW2018_talk_DJ

  state •Window = 27 days. Simple linear model (NWP = 6 hrs). What about for an MHD model? Matt Lang (Paris), Matt Owens (Reading) A Whole Atmosphere model • One model from the Earth’s surface to exobase • Important role of lower level driving in thermos / ionospheric state Extend UM from 85 km up

• richard-jones---k-scale-year-long-global-um-simulations-for-dyamond-3-at-convection-permitting-resolutionpdf

  n1280 GAL9 n1280 CoMA9_TBv1p2 n1280 GAL9 n1280 CoMA9_TBv1p2 n2560 RAL3 OBS OBS n2560 RAL3 CTC 4.4 km CTC 4.4 km Pier Luigi Vidale (NCAS, Uni of Reading) First looks from WCRP global km-scale hackathon RAL3.3 n2560 241K brightness T tracked MCS centroid GAL9 n1280 Shading is the difference between

• PowerPoint Presentation

  a 50hPa deep layer is used. • Turbulence Severity is provided as an Eddy Dissipation Rate • Extra reading: https://doi.org/10.1175/BAMS- D-17-0117.1 • EDR is the official ICAO and WMO atmospheric turbulence intensity metric • Values will range between 0 and 1. • On this map some high EDR values can