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

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>

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

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Type

J_imp - Article in a specialist periodical, which is included in the Web of Science database

CEP classification

—

OECD FORD branch

10501 - Hydrology

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

Publication year

2021

Confidentiality

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

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