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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

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

  • Czech description

Classification

  • Type

    O - Miscellaneous

  • CEP classification

  • OECD FORD branch

    10501 - Hydrology

Result continuities

  • Project

  • 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