Cold-ring shaped storms in Central Europe

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00020699%3A_____%2F08%3A%230000625" target="_blank" >RIV/00020699:_____/08:#0000625 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Cold-ring shaped storms in Central Europe

Popis výsledku v původním jazyce

This paper addresses satellite observations of Central European convective storms which exhibit a cloud-top feature resembling a cold ring in the IR-window bands, surrounding a distinct central warm spot (CWS). The storms from 25 June 2006 above the Czech Republic and Austria are extraordinary examples of storms with such features ? not only by the magnitude and duration of the cold ring and CWS couplets, but namely by storm cloud-top heights as determined from radar observations. While the cold-ring shaped storms in general are not rare, their duration is usually much shorter and the magnitude is typically smaller as compared to this case. The paper documents this case on the basis of MSG observations, combined with radar data. Further, it discusses the potential of the satellite-observed cold-ring feature as one of the indicators of storm severity. Finally, the paper briefly notes the possible impacts of this feature on some cloud-top related products derived from satellite imagery.

Název v anglickém jazyce

Cold-ring shaped storms in Central Europe

Popis výsledku anglicky

This paper addresses satellite observations of Central European convective storms which exhibit a cloud-top feature resembling a cold ring in the IR-window bands, surrounding a distinct central warm spot (CWS). The storms from 25 June 2006 above the Czech Republic and Austria are extraordinary examples of storms with such features ? not only by the magnitude and duration of the cold ring and CWS couplets, but namely by storm cloud-top heights as determined from radar observations. While the cold-ring shaped storms in general are not rare, their duration is usually much shorter and the magnitude is typically smaller as compared to this case. The paper documents this case on the basis of MSG observations, combined with radar data. Further, it discusses the potential of the satellite-observed cold-ring feature as one of the indicators of storm severity. Finally, the paper briefly notes the possible impacts of this feature on some cloud-top related products derived from satellite imagery.

Druh

D - Stať ve sborníku

CEP obor

DG - Vědy o atmosféře, meteorologie

OECD FORD obor

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Projekt

<a href="/cs/project/GA205%2F07%2F0905" target="_blank" >GA205/07/0905: Využití distančních měření při modelování a monitorování silných konvektivních bouří</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2008

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název statě ve sborníku

2008 EUMETSAT Meteorological Satellite Conference. Proceedings

ISBN

978-92-9110-082-8

ISSN

1011-3932

e-ISSN

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Počet stran výsledku

10

Strana od-do

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Název nakladatele

EUMETSAT

Místo vydání

Darmstadt

Místo konání akce

Darmstadt

Datum konání akce

8. 9. 2008

Typ akce podle státní příslušnosti

EUR - Evropská akce

Kód UT WoS článku

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