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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

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

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

displayed, which is reflective of the region seeing temperatures that are rarely experienced.” Contrary to some misleading online commentary, temperatures quoted in Met Office forecasts are air temperatures. This means it’s a reading of the temperatures at a height of 1.25m above the ground inside

including modelling the fallout from Chernobyl for my PhD. I was keen to tell Jim about the unforgettable moment in March 1996 when I first met John Mitchell, then the organisation’s chief climate modeller, at the Met Office college in Reading.   I reached the second interview at the Met Office, where

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

the game again. You can move the messages around until it works. If you are stuck, the solutions are in the solutions document. Software engineers spend lots of time reading code to figure out how it works, so don’t worry about using the solution to help get it right. www.metoffice.gov.uk/schools 6

through the floodplain to the river, rainfall from November to February can be used to predict the risk of flooding in the following May to July period. The project, led by Dr Amulya Chevuturi, whilst at the University of Reading, in collaboration with Brazilian scientists from various partner

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

, • Chilbolton, Lyneham, Wardon Hill • 25+ Days scanning Radiosonde •Larkhill, Chilbolton, Ash Farm, Spire View, Reading. •Extras: Camborne, Herstmonceux, Aberporth •>350 in total. WxUAS •Breach Hill, Heytesbury, Chilbolton, Wherwell Forest. •~120 flight hours. •~700 flights. •First 2 km BVLOS