STORM ON JUNE 22, 2013 IN INDJIJA (SERBIA) – A CONSEQUENCE OF HEAT WAVE

In the period between 16 and 22 June 2013, Europe was hit by a heat wave. At the end of the period characterized by extremely high temperatures, the development of storm along with supercell HP convection cell took place in Serbia, producing tennis ball-sized hailstones and wind with speed exceedin...

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Main Author: Nada Pavlović Berdon
Format: Article
Language:English
Published: Geographical Institute "Jovan Cvijić" SASA 2015-12-01
Series:Zbornik Radova: Geografski institut "Jovan Cvijić"
Subjects:
Online Access:http://ojs.gi.sanu.ac.rs/index.php/zbornik/article/view/278
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spelling doaj-b11443f515fc45259deeca0195bf895d2021-05-28T01:51:54ZengGeographical Institute "Jovan Cvijić" SASAZbornik Radova: Geografski institut "Jovan Cvijić"0350-75991821-28082015-12-01653STORM ON JUNE 22, 2013 IN INDJIJA (SERBIA) – A CONSEQUENCE OF HEAT WAVENada Pavlović Berdon0Pensioner of Republic Hydrometeorological Servce of Serbia, Belgrade, Serbia In the period between 16 and 22 June 2013, Europe was hit by a heat wave. At the end of the period characterized by extremely high temperatures, the development of storm along with supercell HP convection cell took place in Serbia, producing tennis ball-sized hailstones and wind with speed exceeding 35 m/s. This paper analyzes the underlying conditions that led to development of this storm using synoptic charts, vertical atmosphere characteristics as well satellite and radar images. The development of strong convective clouds was enabled by exceptional thermal instability of the atmosphere above the Pannonian Plain and the Balkans and warm subtropical air. The analysis of the vertical structure of atmosphere indicates that the separate convective cells could produce large amounts of precipitation and hailstones up to 8 cm in diameter. Cloudy zone, of the supercell type in development, of 12–16 km width, reached to 20 km height (cloud penetrated tropopause) and indicating extremely great energy instability. Furthermore, this analysis is supplemented with results of nonhydrostatic mesoscale NMM model. Big hailstones from this storm took life of 31 persons in addition to great material damage it caused. http://ojs.gi.sanu.ac.rs/index.php/zbornik/article/view/278heat wave, HP supercell, CAPE, hail, stormy wind
collection DOAJ
language English
format Article
sources DOAJ
author Nada Pavlović Berdon
spellingShingle Nada Pavlović Berdon
STORM ON JUNE 22, 2013 IN INDJIJA (SERBIA) – A CONSEQUENCE OF HEAT WAVE
Zbornik Radova: Geografski institut "Jovan Cvijić"
heat wave, HP supercell, CAPE, hail, stormy wind
author_facet Nada Pavlović Berdon
author_sort Nada Pavlović Berdon
title STORM ON JUNE 22, 2013 IN INDJIJA (SERBIA) – A CONSEQUENCE OF HEAT WAVE
title_short STORM ON JUNE 22, 2013 IN INDJIJA (SERBIA) – A CONSEQUENCE OF HEAT WAVE
title_full STORM ON JUNE 22, 2013 IN INDJIJA (SERBIA) – A CONSEQUENCE OF HEAT WAVE
title_fullStr STORM ON JUNE 22, 2013 IN INDJIJA (SERBIA) – A CONSEQUENCE OF HEAT WAVE
title_full_unstemmed STORM ON JUNE 22, 2013 IN INDJIJA (SERBIA) – A CONSEQUENCE OF HEAT WAVE
title_sort storm on june 22, 2013 in indjija (serbia) – a consequence of heat wave
publisher Geographical Institute "Jovan Cvijić" SASA
series Zbornik Radova: Geografski institut "Jovan Cvijić"
issn 0350-7599
1821-2808
publishDate 2015-12-01
description In the period between 16 and 22 June 2013, Europe was hit by a heat wave. At the end of the period characterized by extremely high temperatures, the development of storm along with supercell HP convection cell took place in Serbia, producing tennis ball-sized hailstones and wind with speed exceeding 35 m/s. This paper analyzes the underlying conditions that led to development of this storm using synoptic charts, vertical atmosphere characteristics as well satellite and radar images. The development of strong convective clouds was enabled by exceptional thermal instability of the atmosphere above the Pannonian Plain and the Balkans and warm subtropical air. The analysis of the vertical structure of atmosphere indicates that the separate convective cells could produce large amounts of precipitation and hailstones up to 8 cm in diameter. Cloudy zone, of the supercell type in development, of 12–16 km width, reached to 20 km height (cloud penetrated tropopause) and indicating extremely great energy instability. Furthermore, this analysis is supplemented with results of nonhydrostatic mesoscale NMM model. Big hailstones from this storm took life of 31 persons in addition to great material damage it caused.
topic heat wave, HP supercell, CAPE, hail, stormy wind
url http://ojs.gi.sanu.ac.rs/index.php/zbornik/article/view/278
work_keys_str_mv AT nadapavlovicberdon stormonjune222013inindjijaserbiaaconsequenceofheatwave
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