Number of the records: 1  

Hydrological balance and runoff from a montane peat bog traced by water temperature

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    SYSNO ASEP0582936
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleHydrological balance and runoff from a montane peat bog traced by water temperature
    Author(s) Falátková, Kristýna (UH-J) ORCID, RID, SAI
    Šípek, Václav (UH-J) SAI, ORCID, RID
    Vlček, Lukáš (UH-J) ORCID, RID, SAI
    Kocum, Jiří (UH-J) ORCID
    Pivokonský, Martin (UH-J) SAI, ORCID, RID
    Source TitleHydrological Sciences Journal. - : Taylor & Francis - ISSN 0262-6667
    Roč. 69, č. 4 (2024), s. 393-406
    Number of pages14 s.
    Publication formOnline - E
    Languageeng - English
    CountryGB - United Kingdom
    Keywordspeatlands ; runoff formation ; catchment hydrology ; water balance ; water temperature ; tracer
    Subject RIVDA - Hydrology ; Limnology
    OECD categoryHydrology
    R&D ProjectsGA22-12837S GA ČR - Czech Science Foundation (CSF)
    Method of publishingLimited access
    Institutional supportUH-J - RVO:67985874
    UT WOS001182636800001
    EID SCOPUS85187454207
    DOI10.1080/02626667.2024.2320392
    AnnotationPeatlands are hydrologically significant landscape units in mountain headwater catchments in Central Europe. In this study, the contribution of a peat bog to runoff and its annual water balance were analysed and compared with those of a forested mineral soil hillslope. A mixing model method using the water temperature as a tracer was applied, and the resulting ratio of peat bog water in streams was incorporated into a hydrological model. The mean peat bog contribution during baseflow ranged from 33.4% during the cold season to 48.9% during the warm season, while during runoff events, the contribution reached over 83%. The simulated water balance results showed a higher actual evapotranspiration on the mineral hillslope, which suggests a higher total runoff from the peat bog (1,523 versus 1,327 mm/y on the mineral hillslope). The results of this study enable more reliable modelling assessments of peatland reactions to climate change.
    WorkplaceInstitute of Hydrodynamics
    ContactSoňa Hnilicová, hnilicova@ih.cas.cz, Tel.: 233 109 003
    Year of Publishing2025
    Electronic addresshttps://www.tandfonline.com/doi/full/10.1080/02626667.2024.2320392
Number of the records: 1  

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