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Assess hydrological responses to a warming climate at the Lysina Critical Zone Observatory in Central Europe

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00020699%3A_____%2F21%3AN0000040" target="_blank" >RIV/00020699:_____/21:N0000040 - isvavai.cz</a>

  • Alternative codes found

    RIV/86652079:_____/21:00544848 RIV/86652079:_____/21:00547394 RIV/00025798:_____/21:00000129

  • Result on the web

    <a href="https://onlinelibrary.wiley.com/doi/epdf/10.1002/hyp.14281" target="_blank" >https://onlinelibrary.wiley.com/doi/epdf/10.1002/hyp.14281</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/ 10.1002/hyp.14281" target="_blank" > 10.1002/hyp.14281</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Assess hydrological responses to a warming climate at the Lysina Critical Zone Observatory in Central Europe

  • Original language description

    Climate warming is having profound effects on the hydrological cycle by increasing atmospheric demand, changing water availability, and snow seasonality. Europe suffered three distinct heat waves in 2019, and 11 of the 12 hottest years ever recorded took place in the past two decades, which will potentially change seasonal streamflow patterns and long-term trends. Central Europe exhibited six dry years in a row since 2014. This study uses data from a well-documented headwater catchment in Central Europe (Lysina) to explore hydrological responses to a warming climate. We applied a lumped parameter hydrologic model Brook90 and a distributed model Penn State Integrated Hydrologic Model (PIHM) to simulate long-term hydrological change under future climate scenarios. Both models performed well on historic streamflow and in agreement with each other according to the catchment water budget. In addition, PIHM was able to simulate lateral groundwater redistribution within the catchment validated by the groundwater table dynamics. The long-term trends in runoff and low flow were captured by PIHM only. We applied different EUROCORDEX models with two emission scenarios (Representative Concentration Pathways RCP 4.5, 8.5) and found significant impacts on runoff and evapotranspiration (ET) for the period of 2071–2100. Results from both models suggested reduced runoff and increased ET, while the monthly distribution of runoff was different. We used this catchment study to understand the importance of subsurface processes in projection of hydrologic response to a warming climate

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10501 - Hydrology

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2021

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Hydrological processes

  • ISSN

    0885-6087

  • e-ISSN

    1099-1085

  • Volume of the periodical

    35

  • Issue of the periodical within the volume

    9

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    17

  • Pages from-to

    1-17

  • UT code for WoS article

    000700789300019

  • EID of the result in the Scopus database

    2-s2.0-85113615755