Regional effects of synoptic situations on soil drought in the Czech Republic
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43210%2F20%3A43918041" target="_blank" >RIV/62156489:43210/20:43918041 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/86652079:_____/20:00531326 RIV/00216224:14310/20:00114168 RIV/00020699:_____/21:N0000008
Výsledek na webu
<a href="https://doi.org/10.1007/s00704-020-03275-4" target="_blank" >https://doi.org/10.1007/s00704-020-03275-4</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s00704-020-03275-4" target="_blank" >10.1007/s00704-020-03275-4</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Regional effects of synoptic situations on soil drought in the Czech Republic
Popis výsledku v původním jazyce
Soil drought has an important influence on plant development. The SoilClim model was used to investigate episodes of soil drought at the 0-100-cm profile during the 1961-2017 period for four selected regions of the Czech Republic (North-western Bohemia, Southern Bohemia, North-eastern Moravia, and Southern Moravia). It emerged that the frequency of soil drought significantly increases in the summer half-year (SHY) and exhibits insignificant trends in the winter half-year (WHY). The dynamic climatology of soil drought is based herein upon synoptic situations as classified by the Czech Hydrometeorological Institute, in terms of which changes in the occurrence and precipitation intensity of drought episodes in the four individual regions were studied. Drought episodes are generally related to decreases in the frequency of precipitation-rich situations and in their precipitation intensity. This is particularly true for situations C (central cyclone over central Europe), B (trough over central Europe), and Bp (travelling trough). Situations B and Bp, together with south-west cyclonic situations SWc1-3, appeared as the most relevant to regional differences in drought episodes during SHY in the four regions studied, while western cyclonic situations (Wc and Wcs) emerged as particularly important in WHY. Regional differences are clearly marked between the Bohemian and Moravian regions, especially in SHY. Discussion of the results obtained concentrates on the uncertainty of soil drought data, differences between SHY and WHY, the effects of synoptic situations, and the broader context of soil droughts.
Název v anglickém jazyce
Regional effects of synoptic situations on soil drought in the Czech Republic
Popis výsledku anglicky
Soil drought has an important influence on plant development. The SoilClim model was used to investigate episodes of soil drought at the 0-100-cm profile during the 1961-2017 period for four selected regions of the Czech Republic (North-western Bohemia, Southern Bohemia, North-eastern Moravia, and Southern Moravia). It emerged that the frequency of soil drought significantly increases in the summer half-year (SHY) and exhibits insignificant trends in the winter half-year (WHY). The dynamic climatology of soil drought is based herein upon synoptic situations as classified by the Czech Hydrometeorological Institute, in terms of which changes in the occurrence and precipitation intensity of drought episodes in the four individual regions were studied. Drought episodes are generally related to decreases in the frequency of precipitation-rich situations and in their precipitation intensity. This is particularly true for situations C (central cyclone over central Europe), B (trough over central Europe), and Bp (travelling trough). Situations B and Bp, together with south-west cyclonic situations SWc1-3, appeared as the most relevant to regional differences in drought episodes during SHY in the four regions studied, while western cyclonic situations (Wc and Wcs) emerged as particularly important in WHY. Regional differences are clearly marked between the Bohemian and Moravian regions, especially in SHY. Discussion of the results obtained concentrates on the uncertainty of soil drought data, differences between SHY and WHY, the effects of synoptic situations, and the broader context of soil droughts.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
40104 - Soil science
Návaznosti výsledku
Projekt
Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2020
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Theoretical and Applied Climatology
ISSN
0177-798X
e-ISSN
—
Svazek periodika
141
Číslo periodika v rámci svazku
3-4
Stát vydavatele periodika
AT - Rakouská republika
Počet stran výsledku
18
Strana od-do
1383-1400
Kód UT WoS článku
000538348300001
EID výsledku v databázi Scopus
2-s2.0-85086101235