Modelling the impact of changes in seasonal snowpack on annual runoff and summer low flows
The result's identifiers
Result code in 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>
Result on the web
<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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Alternative languages
Result language
angličtina
Original language name
Modelling the impact of changes in seasonal snowpack on annual runoff and summer low flows
Original language description
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.
Czech name
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Czech description
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Classification
Type
O - Miscellaneous
CEP classification
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OECD FORD branch
10501 - Hydrology
Result continuities
Project
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Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2019
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů