Trends of convective and stratiform precipitation in the Czech Republic, 1982?2010

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F14%3A00427909" target="_blank" >RIV/68378289:_____/14:00427909 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216208:11320/14:10334377

Výsledek na webu

<a href="http://dx.doi.org/10.1155/2014/647938" target="_blank" >http://dx.doi.org/10.1155/2014/647938</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1155/2014/647938" target="_blank" >10.1155/2014/647938</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Trends of convective and stratiform precipitation in the Czech Republic, 1982?2010

Popis výsledku v původním jazyce

The study examines trends in characteristics of convective and stratiform precipitation in the Czech Republic over 1982?2010. The spatially averaged trends in convective precipitation are rising for indices of mean precipitation, and the increases are significant in all seasons except for winter. For extremes, the trends are spatially much more variable and insignificant, but increases tend to prevail as well. The trends in convective precipitation are larger in the western part of the country where Atlantic influences are stronger. For characteristics of stratiform precipitation, the trends are usually smaller compared to those of convective precipitation, but increases prevail too. They are significant in autumn, especially for extremes, and larger in the eastern part of the country where Mediterranean cyclones play more important role. The trends in convective precipitation tend to be more pronounced at lowland than higher-elevated stations while an opposite pattern prevails for str

Název v anglickém jazyce

Trends of convective and stratiform precipitation in the Czech Republic, 1982?2010

Popis výsledku anglicky

The study examines trends in characteristics of convective and stratiform precipitation in the Czech Republic over 1982?2010. The spatially averaged trends in convective precipitation are rising for indices of mean precipitation, and the increases are significant in all seasons except for winter. For extremes, the trends are spatially much more variable and insignificant, but increases tend to prevail as well. The trends in convective precipitation are larger in the western part of the country where Atlantic influences are stronger. For characteristics of stratiform precipitation, the trends are usually smaller compared to those of convective precipitation, but increases prevail too. They are significant in autumn, especially for extremes, and larger in the eastern part of the country where Mediterranean cyclones play more important role. The trends in convective precipitation tend to be more pronounced at lowland than higher-elevated stations while an opposite pattern prevails for str

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DG - Vědy o atmosféře, meteorologie

OECD FORD obor

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Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2014

Kód důvěrnosti údajů

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

Název periodika

Advances in Meteorology

ISSN

1687-9309

e-ISSN

—

Svazek periodika

2014

Číslo periodika v rámci svazku

647938

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

11

Strana od-do

1-11

Kód UT WoS článku

000332880000001

EID výsledku v databázi Scopus

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