Spatial and temporal evolution of drought conditions at various time scales in the Czech Republic during growing period

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41210%2F12%3A56242" target="_blank" >RIV/60460709:41210/12:56242 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67179843:_____/12:00388746 RIV/00020699:_____/12:#0000680

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Spatial and temporal evolution of drought conditions at various time scales in the Czech Republic during growing period

Popis výsledku v původním jazyce

This paper analyzes the characteristics of spatial evolution of the standardized precipitation evapotranspiration index (SPEI) at various time scales during the growing period (April-September) over the Czech Republic. The SPEI was calculated from monthly records of mean temperature and precipitation totals measured at a dense network of 184 climatological stations for the period 1961?2010. Using various lags, 1, 3, 6, 12, and 24 months. The drought at these time scales is relevant for agricultural, hydrological, and socio-economic impacts, respectively. The study refers to the warm season of the year (from April to September). The principal modes of variability of the SPEI calculated at these five time scales were identified by using the empirical orthogonal functions (EOF) analysis. The explained variance of the leading EOF ranges between 71 and 61% as the time scale for calculating the SPEI increases from 1 to 24 months. The explained variance of EOF2 and EOF3 ranges between 5 and 9

Název v anglickém jazyce

Spatial and temporal evolution of drought conditions at various time scales in the Czech Republic during growing period

Popis výsledku anglicky

This paper analyzes the characteristics of spatial evolution of the standardized precipitation evapotranspiration index (SPEI) at various time scales during the growing period (April-September) over the Czech Republic. The SPEI was calculated from monthly records of mean temperature and precipitation totals measured at a dense network of 184 climatological stations for the period 1961?2010. Using various lags, 1, 3, 6, 12, and 24 months. The drought at these time scales is relevant for agricultural, hydrological, and socio-economic impacts, respectively. The study refers to the warm season of the year (from April to September). The principal modes of variability of the SPEI calculated at these five time scales were identified by using the empirical orthogonal functions (EOF) analysis. The explained variance of the leading EOF ranges between 71 and 61% as the time scale for calculating the SPEI increases from 1 to 24 months. The explained variance of EOF2 and EOF3 ranges between 5 and 9

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

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2012

Kód důvěrnosti údajů

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

Název periodika

Idojaras

ISSN

0324-6329

e-ISSN

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Svazek periodika

116

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

15

Strana od-do

281-295

Kód UT WoS článku

000312155300003

EID výsledku v databázi Scopus

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