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, G. & KERN, A. 2009a. What Climate Can We Expect in Central/Eastern Europe by 2071-2100? BARTHOLY, J., PONGRACZ, R., PIECZKA, I., KARDOS, P. & HUNYADY, A. 2009b. Computational Analysis of Expected Climate Change in the Carpathian Basin Using a Dynamical Climate Model. In: MARGENOV, S., VULKOV, L. G
Order Rank ordered statistics Year ordered statistics Region Choose a region UK England Wales Scotland Northern Ireland England & Wales England N England S Scotland N Scotland E Scotland W England E & NE England NW/Wales N Midlands East Anglia England SW/Wales S England SE/Central S Parameter
Dec 2025 Height (m) Wind Speed mean/gusts (mph) Wind Direction (blowing from) 00:00 03:00 06:00 09:00 12:00 15:00 18:00 21:00 00:00 1300 39/48 S 50/62 S 50/63 SW 49/61 SW 49/61 SW 45/57 SW 38/48 SW 32/40 SW 31/38 S 900 28/37 SW 35/47 S 37/49 SW 35/47 SW 35/46 SW 32/43 SW 28/37 SW 25/34 SW 23/30 S
observations. Over the UK most commercial aircraft are continuously broadcasting information for air traffic management; this information is defined by the Mode-Selective (Mode-S) Enhanced Surveillance (EHS) and Automatic Dependent Surveillance Broadcast (ADS-B) standards. ADS-B data is continuously broadcast
-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
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
was certainly faster during this period and significant increases took place, the large changes implied by the linear trend are probably misleading as the trend in mean temperature is clearly not linear and there was a drop in temperature coinciding with the start of the 1960’s. To present a more
., Sutton, M. A., Ambus, P., Raivonen, M., Duyzer, J., Simpson, D., Fagerli, H., Fuzzi, S., Schjoerring, J. K., Granier, C., Neftel, A., Isaksen, I. S. A., Laj, P., Maione, M., Monks, P. S., Burkhardt, J., Daemmgen, U., Neirynck, J., Personne, E., Wichink-Kruit, R., Butterbach-Bahl, K., Flechard, C
of the loan in accordance with the terms of the Exhibition Loan Agreement. 4.3 Procedure for loan request Please note that for all loan requests, we would expect the preliminary research, identification and selection of the object(s) to be undertaken by the borrower or representatives working
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
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