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The Climatology of Significant Tornadoes in the Czech Republic

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BRÁZDIL Rudolf CHROMÁ Kateřina PÚČIK Tomáš ČERNOCH Zbyněk DOBROVOLNÝ Petr DOLÁK Lukáš KOTYZA Oldřich ŘEZNÍČKOVÁ Ladislava TASZAREK Mateusz

Rok publikování 2020
Druh Článek v odborném periodiku
Časopis / Zdroj Atmosphere
Fakulta / Pracoviště MU

Přírodovědecká fakulta

Citace
www https://www.mdpi.com/2073-4433/11/7/689
Doi http://dx.doi.org/10.3390/atmos11070689
Klíčová slova tornado; documentary data; tornado intensity; tornado damage; tornado fatality; spatiotemporal variability; dynamic climatology; environmental conditions; Czech Republic
Popis In the Czech Republic, tornadoes may reach an intensity of F2 and F3 on the Fujita scale, causing "considerable" to "severe" damage. Documentary evidence is sufficient to allow the creation of a chronology of such events, from the earliest recorded occurrence in 1119 CE (Common Era) to 2019, including a total of 108 proven or probable significant tornadoes on 90 separate days. Since only 11 significant tornadoes were documented before 1800, this basic analysis centers around the 1811–2019 period, during which 97 tornadoes were recorded. Their frequency of occurrence was at its highest in the 1921–1930, 1931–1940, and 2001–2010 decades. In terms of annual variations, they took place most frequently in July, June, and August (in order of frequency), while daily variation favored the afternoon and early evening hours. Conservative estimates of human casualties mention 8 fatalities and over 95 people injured. The most frequent types of damage were related to buildings, individual trees, and forests. Tornadoes of F2–F3 intensity were particularly associated with synoptic types characterized by airflow from the western quadrant together with troughs of low pressure extending or advancing over central Europe. Based on parameters calculated from the ERA-5 re-analysis for the period of 1979–2018, most of these tornadoes occurred over a wide range of Convective Available Potential Energy (CAPE) values and moderate-to-strong vertical wind shear. The discussion herein also addresses uncertainties in tornado selection from documentary data, the broader context of Czech significant tornadoes, and the environmental conditions surrounding their origins.