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. P. Bierkens, P. Ciais, D. B. Clark, D. Deryng, P. Döll, P. Falloon, B. Fekete, C. Folberth, A. D. Friend, C. Gellhorn, S. N. Gosling, I. Haddeland, N. Khabarov, M. Lomas, Y. Masaki, K. Nishina, K. Neumann, T. Oki, R. Pavlick, A. C. Ruane, E. Schmid, C. Schmitz, T. Stacke, E. Stehfest, Q. Tang, D

from) 06:00 09:00 12:00 15:00 18:00 21:00 00:00 1300 5/7 NE 6/7 SE 7/9 E 9/12 S 13/16 SE 19/22 SE 21/25 SE 900 5/6 E 9/12 SE 7/10 S 9/13 S 11/15 SE 14/17 SE 15/19 S 600 9/11 NE 5/7 E 6/9 E 6/9 SW 10/14 S 10/13 SE 11/14 S 300 3/8 NE 2/5 N 5/7 NE 4/7 S 4/8 S 7/12 SE 5/8 S Glen 2/6 N 1/6 E 2/5 E 3/5 SW 4

, 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

/6 SE 4/7 SE 4/7 SE 7/11 S 13/16 SW 17/21 S 20/25 S 900 8/11 W 8/12 W 5/7 SE 4/6 SE 3/7 SE 7/11 S 11/14 SW 15/19 S 18/23 S 600 4/7 SW 4/7 SW 3/5 SE 3/6 SE 3/6 SE 6/10 SW 5/8 SW 9/13 S 11/16 S 300 2/8 W 3/9 N 1/6 NE 1/4 E 1/6 SE 2/8 S 1/7 SW 1/9 S 2/11 S Glen 2/4 W 3/4 N 3/5 NE 2/4 E 2/5 W 2/5 W 1/3

-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

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

, we construct a data blending framework based on Generalised Additive Models (GAMs, e.g. Hastie & Tibshirani, 1990; Wood, 2017, 2020) to undertake extreme value analysis of RX1day JJAS block-maxima a extreme precipitation , modelled as a Generalised Extreme Value (GEV) distribution: Y s,t,m ∼ GEV(μ