Modelling the impact of changes in seasonal snowpack on annual runoff and summer low flows
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00020699%3A_____%2F19%3AN0000147" target="_blank" >RIV/00020699:_____/19:N0000147 - isvavai.cz</a>
Výsledek na webu
<a href="https://meetingorganizer.copernicus.org/EGU2019/EGU2019-9879.pdf" target="_blank" >https://meetingorganizer.copernicus.org/EGU2019/EGU2019-9879.pdf</a>
DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Modelling the impact of changes in seasonal snowpack on annual runoff and summer low flows
Popis výsledku v původním jazyce
In fact, this is an abstract related to the poster presentation exhibited during the EGU2019 General Assembly. Using the HBV (i.e. HBV-light) model and various hydrometeorological time series representing 60 selected mountain catchments from Czechia and the period 1980-2014, it was found that, besides summer precipitation, the previous snowpack has a crucial effect on the generation of summer runoff. As a consequence, snow and the timing of spring snowmelt have also an important effect on the occurrence of summer runoff minima, which are expected to be shifted in the future, depending on the climate change patterns.
Název v anglickém jazyce
Modelling the impact of changes in seasonal snowpack on annual runoff and summer low flows
Popis výsledku anglicky
In fact, this is an abstract related to the poster presentation exhibited during the EGU2019 General Assembly. Using the HBV (i.e. HBV-light) model and various hydrometeorological time series representing 60 selected mountain catchments from Czechia and the period 1980-2014, it was found that, besides summer precipitation, the previous snowpack has a crucial effect on the generation of summer runoff. As a consequence, snow and the timing of spring snowmelt have also an important effect on the occurrence of summer runoff minima, which are expected to be shifted in the future, depending on the climate change patterns.
Klasifikace
Druh
O - Ostatní výsledky
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
2019
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů