Tuyển tập các báo cáo nghiên cứu về lâm nghiệp được đăng trên tạp chí lâm nghiệp Original article đề tài: Heat and drought 2003 in Europe: a climate synthesis. | Ann. For. Sci. 63 2006 569-577 INRA EDP Sciences 2006 DOI forest 2006043 569 Review Heat and drought 2003 in Europe a climate synthesis Martine REBETEZa Helmut MAYERb Olivier DUPONTc Dirk SCHINDLERb Karl GARTNERd Jurgen P. KROPPe Anette MENZELf a WSL Swiss Federal Research Institute Lausanne Switzerland b Meteorological Institute University of Freiburg Germany c MeteoFrance Illkirch-Graffenstaden France d Federal Research and Training Centre for Forests Natural Hazards and Landscape Vienna Austria e Potsdam Institute for Climate Impact Research Potsdam Germany f Chair for Ecoclimatology Technical University of Munich Freising Germany Received 14 October 2005 accepted 17 March 2006 Abstract - Heat and drought were extreme in summer 2003 in Europe. Climatic data show that most extreme were maximum air temperatures in June and August maps of these two months show a striking similarity in geographical range. Over wide regions monthly mean temperatures were more than 4 C above the long term mean values. The heat lasted from May to September in large parts of western and central Europe. The lack of precipitation was most severe in summer 2003 but precipitation was generally below normal from February 2003 until June 2004 with the exception of two months . Sunshine duration was above normal particularly in regions which usually have rainy and cloudy episodes in summer and relative air humidity was below normal during the whole year of 2003. The drought experienced by the vegetation in summer 2003 was exacerbated by the length of the period with scarce precipitation and humidity by the heat during the summer and by long sunshine duration. climate change drought heat precipitation air temperature Résumé - La chaleur et la sécheresse 2003 une synthèse climatique. Temperatures et sécheresse ont été extremes en Europe durant l été 2003. Les valeurs les plus anormales ont été atteintes par les températures maximales en juin et en aout. La repartition spatiale des .
