Climatology of the extreme heavy precipitation events in Slovakia in the 1951–2020 period

Ladislav Markovič, P. Faško, J. Pecho
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引用次数: 1

Abstract

In this study, we investigate extreme heavy precipitation events in the Slovak Republic in the period 1951–2020 in terms of their spatial and temporal distribution with goal to create dynamic-climatological analysis of those patterns of the atmospheric circulation that can eventually lead to the occurrence of the extreme multi-day precipitation events. Heavy precipitation is defined as maximum precipitation total over five consecutive days (Rx5D) where a non-zero daily precipitation total must be recorded every day of selected 5-day period. Spatial and temporal distribution of multiday precipitation totals is affected by many factors, mainly by the processes taking place in the troposphere eventually represented by the synoptic scale atmospheric circulation and by the orographic diversity of the area, which together significantly affects distribution of precipitation in the selected area. Our study is therefore constructed as an analysis of relationships between localized tropospheric circulation defined by the Czechoslovak catalogue of the typified synoptic situations (Brádka, 1968), the predominant wind patterns and the spatiotemporal distribution of Rx5D.
1951-2020年斯洛伐克极端强降水事件的气候学分析
在这项研究中,我们调查了1951-2020年斯洛伐克共和国的极端强降水事件的时空分布,目的是对那些最终导致极端多日降水事件发生的大气环流模式进行动态气候学分析。强降水定义为连续5天的最大降水总量(Rx5D),在选定的5天周期内,每天必须记录非零的日降水总量。多日降水总量的时空分布受多种因素的影响,主要受最终以天气尺度大气环流为代表的对流层过程和地区地形多样性的影响,这些因素共同显著影响所选地区降水的分布。因此,我们的研究是建立在分析由捷克斯洛伐克典型天气情况目录(Brádka, 1968)定义的局部对流层环流、主要风型和Rx5D时空分布之间关系的基础上的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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