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Attributing the effects of climate change and forest disturbance on runoff using distributed modeling and indicators of hydrological alteration in Central European montane basins

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F25%3A10491337" target="_blank" >RIV/00216208:11310/25:10491337 - isvavai.cz</a>

  • Výsledek na webu

    <a href="https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=D2KTH2ZrvY" target="_blank" >https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=D2KTH2ZrvY</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.ejrh.2024.102101" target="_blank" >10.1016/j.ejrh.2024.102101</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Attributing the effects of climate change and forest disturbance on runoff using distributed modeling and indicators of hydrological alteration in Central European montane basins

  • Popis výsledku v původním jazyce

    This study examines the impacts of climate warming and forest disturbances on hydrological alterations in montane headwater basins. Using the MIKE SHE distributed hydrological model, scenario-based simulations assessed changes in runoff seasonality, evapotranspiration, streamflow, and variability. Hydrological alteration indicators were applied to disentangle the contributions of these drivers and their interactions under varying environmental conditions. The study is focused on eight unregulated basins in the headwaters of five mid-latitude mountain ranges in Czechia. The results demonstrated that the climate warming is the primary driver of hydrological change, causing shifts in runoff seasonality, increased evapotranspiration, and reduced streamflow. Forest disturbances amplify these effects during dry conditions, intensifying runoff variability, increasing low-flow frequency, and modifying peak flows. Regional differences show greater sensitivity in steeper eastern basins due to limited snow accumulation and higher runoff variability. This study highlights the interconnected impacts of climate warming and forest disturbances, with warming driving systemic shifts and disturbances acting as amplifiers in extreme conditions. Methodologically, the study provide a framework for disentangling the effects of climate and landcover changes on hydrology, and thus offering insights for managing sensitive montane ecosystems and water resources under changing environmental conditions.

  • Název v anglickém jazyce

    Attributing the effects of climate change and forest disturbance on runoff using distributed modeling and indicators of hydrological alteration in Central European montane basins

  • Popis výsledku anglicky

    This study examines the impacts of climate warming and forest disturbances on hydrological alterations in montane headwater basins. Using the MIKE SHE distributed hydrological model, scenario-based simulations assessed changes in runoff seasonality, evapotranspiration, streamflow, and variability. Hydrological alteration indicators were applied to disentangle the contributions of these drivers and their interactions under varying environmental conditions. The study is focused on eight unregulated basins in the headwaters of five mid-latitude mountain ranges in Czechia. The results demonstrated that the climate warming is the primary driver of hydrological change, causing shifts in runoff seasonality, increased evapotranspiration, and reduced streamflow. Forest disturbances amplify these effects during dry conditions, intensifying runoff variability, increasing low-flow frequency, and modifying peak flows. Regional differences show greater sensitivity in steeper eastern basins due to limited snow accumulation and higher runoff variability. This study highlights the interconnected impacts of climate warming and forest disturbances, with warming driving systemic shifts and disturbances acting as amplifiers in extreme conditions. Methodologically, the study provide a framework for disentangling the effects of climate and landcover changes on hydrology, and thus offering insights for managing sensitive montane ecosystems and water resources under changing environmental conditions.

Klasifikace

  • Druh

    J<sub>imp</sub> - Článek v periodiku v databázi Web of Science

  • CEP obor

  • OECD FORD obor

    10508 - Physical geography

Návaznosti výsledku

  • Projekt

    Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

  • Návaznosti

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Ostatní

  • Rok uplatnění

    2025

  • Kód důvěrnosti údajů

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

Údaje specifické pro druh výsledku

  • Název periodika

    Journal of Hydrology: Regional Studies

  • ISSN

    2214-5818

  • e-ISSN

    2214-5818

  • Svazek periodika

    57

  • Číslo periodika v rámci svazku

    February

  • Stát vydavatele periodika

    NL - Nizozemsko

  • Počet stran výsledku

    22

  • Strana od-do

    102101

  • Kód UT WoS článku

    001385167100001

  • EID výsledku v databázi Scopus

    2-s2.0-85211231870