Number of the records: 1

Severe storm in Bavaria, the Czech Republic and Poland on 12–13 July 1984: A statistic- and model-based analysis

SYSNO ASEP	0327260
Document Type	J - Journal Article
R&D Document Type	Journal Article
Subsidiary J	Článek ve WOS
Title	Severe storm in Bavaria, the Czech Republic and Poland on 12–13 July 1984: A statistic- and model-based analysis
Title	Silná bouře v Bavorsku, České republice a Polsku 12.-13. července 1984: statistická a modelová analýza
Author(s)	Kašpar, Marek (UFA-U)_{RID, ORCID} Müller, Miloslav (UFA-U)_{RID, ORCID} Kakos, Vilibald (UFA-U) Řezáčová, Daniela (UFA-U)_{RID, ORCID} Sokol, Zbyněk (UFA-U)_{RID, ORCID}
Number of authors	5
Source Title	Atmospheric Research. - : Elsevier - ISSN 0169-8095 Roč. 93, 1-3 (2009), s. 99-110
Number of pages	12 s.
Publication form	web - web
Action	European Conference on Severe Storms /4./
Event date	10.09.2007-14.09.2007
VEvent location	Miramare -Trieste
Country	IT - Italy
Event type	EUR
Language	eng - English
Country	NL - Netherlands
Keywords	convective storm ; synoptic anomaly ; mesoscale condition ; forecast verification ; gust front
Subject RIV	DG - Athmosphere Sciences, Meteorology
R&D Projects	GA205/07/0905 GA ČR - Czech Science Foundation (CSF)
	KJB300420701 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
	KJB300420802 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
CEZ	AV0Z30420517 - UFA-U, BC-A (2005-2011)
UT WOS	000267743900012
DOI	10.1016/j.atmosres.2008.10.004
Annotation	We analyze synoptic and sub-synoptic meteorological conditions which occurred before and during a selected historic event with organized convection in Central Europe. The re-analyses ERA-40 are used to investigate the fields of dynamic and thermodynamic variables at the synoptic scale. It is demonstrated that some variables may reach abnormal values not only in a case of heavy steady rains, but also in a case of severe convection. The non-hydrostatic limited-area NWP model COSMO is employed to reforecast the event at the sub-synoptic scale. The verification of model results indicates the simulated convection environment does not differ significantly from the real conditions. The subsequent analysis reveals vertical shear and stability conditions favorable for the intensification of convective processes ahead of propagating gust fronts.
Workplace	Institute of Atmospheric Physics
Contact	Kateřina Adamovičová, adamovicova@ufa.cas.cz, Tel.: 272 016 012 ; Kateřina Potužníková, kaca@ufa.cas.cz, Tel.: 272 016 019
Year of Publishing	2010

Number of the records: 1