Analysis of small forest catchments evapotranspiration determined by precipitation/runoff measurements, remote sensing model DisALEXI and water balance model SoilClim
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43210%2F21%3A43921844" target="_blank" >RIV/62156489:43210/21:43921844 - isvavai.cz</a>
Výsledek na webu
<a href="https://mendelnet.cz/media/mnet_2021_full.pdf" target="_blank" >https://mendelnet.cz/media/mnet_2021_full.pdf</a>
DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Analysis of small forest catchments evapotranspiration determined by precipitation/runoff measurements, remote sensing model DisALEXI and water balance model SoilClim
Popis výsledku v původním jazyce
The below-average precipitation combined with above-average temperature during the period 2015-2019 showed high susceptibility of the Czech landscape to drought stress. This particular drought caused significant economics losses in the forestry, agcicultural and water management sectors. Because the climate models predict recurrence of drought period with increasing intensity and frequency, accurate knowledge of individual ecosystems evapotranspiration is needed to develop suitable adaptation to climate change. This contribution detects the evapotranspiration determined by precipitation/runoff measurements, diagnostic remote sensing model DisALEXI and semi-empirical model SoilClim in small forest (mostly Norway spruce) catchments areas (GEOMON network). Based on altitudinal gradient analysis (470-942 m), two of the three applied methods (DisALEXI and SoilClim models) confirm the previously accepted hypothesis, that at low elevation the evapotranspiration is limited by precipitation while at higher altitudes by available energy. Moreover, these two models identify the break point where evapotranspiration reaches maximum values and the altitude where evapotranspiration begins to be limited by a lack of available energy (DisALEXI at 758 m, SoilClim at 685 m). However, the DisALEXI model as the only one that best captures the relationship between evapotranspiration, precipitation and altitude. This analysis can by useful for detection suitable conditions for sustainable spruce forest management.
Název v anglickém jazyce
Analysis of small forest catchments evapotranspiration determined by precipitation/runoff measurements, remote sensing model DisALEXI and water balance model SoilClim
Popis výsledku anglicky
The below-average precipitation combined with above-average temperature during the period 2015-2019 showed high susceptibility of the Czech landscape to drought stress. This particular drought caused significant economics losses in the forestry, agcicultural and water management sectors. Because the climate models predict recurrence of drought period with increasing intensity and frequency, accurate knowledge of individual ecosystems evapotranspiration is needed to develop suitable adaptation to climate change. This contribution detects the evapotranspiration determined by precipitation/runoff measurements, diagnostic remote sensing model DisALEXI and semi-empirical model SoilClim in small forest (mostly Norway spruce) catchments areas (GEOMON network). Based on altitudinal gradient analysis (470-942 m), two of the three applied methods (DisALEXI and SoilClim models) confirm the previously accepted hypothesis, that at low elevation the evapotranspiration is limited by precipitation while at higher altitudes by available energy. Moreover, these two models identify the break point where evapotranspiration reaches maximum values and the altitude where evapotranspiration begins to be limited by a lack of available energy (DisALEXI at 758 m, SoilClim at 685 m). However, the DisALEXI model as the only one that best captures the relationship between evapotranspiration, precipitation and altitude. This analysis can by useful for detection suitable conditions for sustainable spruce forest management.
Klasifikace
Druh
D - Stať ve sborníku
CEP obor
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OECD FORD obor
10501 - Hydrology
Návaznosti výsledku
Projekt
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Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2021
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název statě ve sborníku
MendelNet 2021: Proceedings of International PhD Students Conference
ISBN
978-80-7509-821-4
ISSN
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e-ISSN
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Počet stran výsledku
6
Strana od-do
242-247
Název nakladatele
Mendelova univerzita v Brně
Místo vydání
Brno
Místo konání akce
Brno
Datum konání akce
10. 11. 2021
Typ akce podle státní příslušnosti
EUR - Evropská akce
Kód UT WoS článku
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