2015
Drivers of soil drying in the Czech Republic between 1961 and 2012
TRNKA, Miroslav, Rudolf BRÁZDIL, J. BALEK, D. SEMERADOVA, P. HLAVINKA et. al.Základní údaje
Originální název
Drivers of soil drying in the Czech Republic between 1961 and 2012
Autoři
TRNKA, Miroslav (203 Česká republika, garant), Rudolf BRÁZDIL (203 Česká republika, domácí), J. BALEK (203 Česká republika), D. SEMERADOVA (203 Česká republika), P. HLAVINKA (203 Česká republika), M. MOŽNÝ (203 Česká republika), Petr ŠTĚPÁNEK (203 Česká republika), Petr DOBROVOLNÝ (203 Česká republika, domácí), Pavel ZAHRADNÍČEK (203 Česká republika), M. DUBROVSKY (203 Česká republika), Josef EITZINGER (40 Rakousko), B. FUCHS (203 Česká republika), M. SVOBODA (203 Česká republika), M. HAYES (840 Spojené státy) a Zdeněk ŽALUD (203 Česká republika)
Vydání
International Journal of Climatology, HOBOKEN, Wiley, 2015, 0899-8418
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10500 1.5. Earth and related environmental sciences
Stát vydavatele
Spojené státy
Utajení
není předmětem státního či obchodního tajemství
Impakt faktor
Impact factor: 3.609
Kód RIV
RIV/00216224:14310/15:00081170
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000357894100034
Klíčová slova anglicky
pan evaporation; soil moisture; reference evapotranspiration; drought climatology; water balance; observed climate change
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 5. 4. 2016 16:07, Ing. Andrea Mikešková
Anotace
V originále
Soil moisture dynamics and their temporal trends in the Czech Republic are forced by various drivers. The methodology of applying remotely sensed data with both high temporal and spatial resolutions provides detailed insight and objective quantification of the causes of changes in soil moisture patterns. Our analysis of temporal trends indicates that shifts in drought severity between 1961 and 2012 (especially in the April, May, and June period, which displayed a 50% increase in drought probability between 1961-1980 and 2001-2012) are alarming. We found that increased global radiation and air temperature together with decreased relative humidity (all statistically significant at the 0.05 level) led to increases in the reference evapotranspiration in all months of the growing season; this trend was particularly evident in April, May, and August, when more than 80% of the territory displayed an increased demand for soil water. This finding was shown to be consistent with the measured pan evaporation (1968-2012) that was characterized by increasing trends, particularly during the April-June period. These changes, in combination with the earlier end of snow cover and the earlier start of growing season (up to 20days in some regions), led to an increased actual evapotranspiration at the start of growing season that tends to deplete the soil moisture earlier, leaving the soil more exposed to the impacts of rainfall variability. These results support concerns related to the potentially increased severity of drought events in Central Europe. The reported trend patterns are of particular importance with respect to the expected climate change, given the robustness and consistency of the trends shown and the fact that they can be aligned with the existing climate model projections.
Návaznosti
GAP209/11/0956, projekt VaV |
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GA13-04291S, projekt VaV |
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