CZEXWED: The unified Czech extreme weather database

被引:2
|
作者
Kaspar, Marek [1 ]
Muller, Miloslav [1 ,2 ]
Bliznak, Vojtech [1 ]
Valerianova, Anna [3 ]
机构
[1] Czech Acad Sci, Inst Atmospher Phys, Bocni 2 1401, Prague 14100, Czech Republic
[2] Charles Univ Prague, Fac Sci, Albertov 6, Prague 12843, Czech Republic
[3] Czech Hydrometeorol Inst, Sabatce 2050-17, Prague 14306, Czech Republic
来源
WEATHER AND CLIMATE EXTREMES | 2023年 / 39卷
关键词
Weather extreme; Weather extremity index; Meteorological database; RAINFALL EVENTS; WINDSTORMS; FLOODS; FREQUENCY; CATALOG;
D O I
10.1016/j.wace.2022.100540
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A crucial step in developing a strategy against natural hazards is the analysis of weather extremes in the past. Due to the multiplication of their impacts when occurring in a larger area, we strongly recommend not evaluating the extremes only at individual sites but assessing regional extreme weather events. The presented Czech Extreme Weather Database (CZEXWED) comprises six types of extreme events, namely, heat waves, cold waves, air temperature drops, windstorms, heavy precipitation events, and heavy snowfalls. To date, it covers the period 1961-2020. To minimize methodological differences in the process of evaluating various types of extreme weather events including compound events, we employed the weather extremity index (WEI), a universal in-dicator based on the evaluation of return periods of relevant variables. Each event is characterized not only by the WEI value but also by its spatial extent and duration.Heat and cold waves in Czechia generally reach higher WEI values than other types of extreme weather because they usually affect larger areas. The number and extremity of heat waves are increasing significantly, while the opposite may be true for cold waves and windstorms. Air temperature drops defined by declines in daily maximum air temperature are frequent in the warm half-year, but three of four top events occurred in January. Windstorms and heavy precipitation events prevailed in the cold and warm half-years, respectively, but weaker events of these types also occurred during the opposite season. A comparison of CZEXWED with event lists from the wider Central European region shows that Czech and Central European extreme events correspond well with each other.
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页数:11
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