Drivers of soil drying in the Czech Republic between 1961 and 2012

Logo poskytovatele
Logo poskytovatele

Varování

Publikace nespadá pod Ústav výpočetní techniky, ale pod Přírodovědeckou fakultu. Oficiální stránka publikace je na webu muni.cz.
Autoři

TRNKA Miroslav BRÁZDIL Rudolf BALEK J. SEMERADOVA D. HLAVINKA P. MOŽNÝ M. ŠTĚPÁNEK Petr DOBROVOLNÝ Petr ZAHRADNÍČEK Pavel DUBROVSKY M. EITZINGER Josef FUCHS B. SVOBODA M. HAYES M. ŽALUD Zdeněk

Rok publikování 2015
Druh Článek v odborném periodiku
Časopis / Zdroj International Journal of Climatology
Fakulta / Pracoviště MU

Přírodovědecká fakulta

Citace
Doi http://dx.doi.org/10.1002/joc.4167
Obor Vědy o atmosféře, meteorologie
Klíčová slova pan evaporation; soil moisture; reference evapotranspiration; drought climatology; water balance; observed climate change
Popis 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.
Související projekty:

Používáte starou verzi internetového prohlížeče. Doporučujeme aktualizovat Váš prohlížeč na nejnovější verzi.

Další info