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Future changes in snowpack will impact seasonal runoff and low flows in Czechia
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SYSNO ASEP 0545028 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Future changes in snowpack will impact seasonal runoff and low flows in Czechia Author(s) Jeníček, M. (CZ)
Hnilica, Jan (UH-J) SAI, ORCID, RID
Nedělčev, O. (CZ)
Šípek, Václav (UH-J) SAI, ORCID, RIDArticle number 100899 Source Title Journal of Hydrology: Regional Studies. - : Elsevier
Roč. 37, October (2021)Number of pages 16 s. Publication form Online - E Language eng - English Country NL - Netherlands Keywords climate change ; snow ; snowmelt runoff ; seasonal runoff ; low flows Subject RIV DA - Hydrology ; Limnology OECD category Hydrology R&D Projects 8I20001 GA MŠMT - Ministry of Education, Youth and Sports (MEYS) Method of publishing Open access Institutional support UH-J - RVO:67985874 UT WOS 000708973000005 EID SCOPUS 85113673750 DOI 10.1016/j.ejrh.2021.100899 Annotation Mountains are referred to as “water towers” because they substantially affect the hydrology of downstream areas. However, snow storages will decrease in the future due to the increase in air temperature which will affect streamflow regime. Main objectives of this study were 1) to simulate the future changes in snow for a large set of mountain catchments in Czechia, reflecting a wide range of climate projections and 2) to analyse how the snow changes will affect groundwater recharge, streamflow seasonality and low flows in the future. Workplace Institute of Hydrodynamics Contact Soňa Hnilicová, hnilicova@ih.cas.cz, Tel.: 233 109 003 Year of Publishing 2022 Electronic address https://www.sciencedirect.com/science/article/pii/S2214581821001282
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