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Park - top right) and wind speed (anemogram for Shoeburyness - bottom). Daily weather extremes Highest Maximum Temperature 15.5 °C at Jeresey, St Helier (Channel Islands) Lowest Minimum Temperature 0.4 °C at Tummel Bridge (Tayside) Most Rainfall 69.5 mm at Trawstynydd (Gwynedd) Most Sunshine 8.1 hours

across Central and Southern England. Daily weather extremes Highest Maximum Temperature 16.7 °C at St Mary's (Isles of Scilly) Lowest Minimum Temperature -3.9 °C at Eskdalemuir (Dumfriesshire) Most Rainfall 17.8 mm at Stornoway Airport (Western Isles) Most Sunshine 10.3 hours at Chivenor (Devon

-35.625 o W, 3.75 o S-8.75 o S and is marked by the blue rectangle in Figure 1. Quintile category forecasts have been issued for this (or a very similar) region since 1987. Forecast probabilities for quintile categories of mean rainfall for SNEBR are shown in the table below. The near-normal and above

) on initiation. Can we perturb the soil moisture in a realistic way in some case(s) to investigate this? Analysis of climate runs inc. UKCP 2.2km ensemble, 2.2km over Europe and 4.5km over Africa. Event composites for different weather regimes. Analyse profiles of events and rainfall distributions

with New Year’s Day the warmest on record according to maximum temperature. 16.3C was recorded at St James’s Park, London and that mild theme was replicated through much of 2022 with more warmer than average days and fewer cooler than average days.   St James's Park was provisionally the warmest

the period 1996-2009. References M. J. Best, M. Pryor, D. B. Clark, G. G. Rooney, R .L. H. Essery, C. B. Ménard, J. M. Edwards, M. A. Hendry, A. Porson, N. Gedney, L. M. Mercado, S. Sitch, E. Blyth, O. Boucher, P. M. Cox, C. S. B. Grimmond, and R. J. Harding. The Joint UK Land Environment Simulator

areas in the north. Sheltered locations in the west and south remained nearer or above freezing, but all areas were exposed to the strong east wind, typically gusting at 20 to 30 Kt (23 to 35 mph); such conditions resulting in a ‘feels like’ temperature of around -10 °C. Even St Mary’s Airport, Isles

this signal has a particularly large spatial extent and a magnitude of >1.6 hPa s �1 in the ensemble mean by the 2080s/2090s. In north central Sahel both ensembles show smaller upward anomalies (approximately 0.8 hPa s �1 ) corresponding to the wet signal in Figure 1. These changes are amplified

Climatic Change (2013) 120:965–975 DOI 10.1007/s10584-013-0831-3 LETTER Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP) L. O. Mearns & S. Sain & L. R. Leung & M. S. Bukovsky & S. McGinnis & S. Biner & D. Caya & R. W. Arritt & W. Gutowski & E

, Institut Pierre Simon Laplace (IPSL) S. Flavoni: Sorbonne Universités, LOCEAN Laboratory, Institut Pierre Simon Laplace (IPSL) L. Hermanson: Met Office Hadley Centre N. Keenlyside: University of Bergen and Bjerknes Centre for Climate Research, Nansen Environmental and Remote Sensing Center