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

0582936 - ÚH 2025 RIV GB eng J - Článek v odborném periodiku
Falátková, Kristýna - Šípek, Václav - Vlček, Lukáš - Kocum, Jiří - Pivokonský, Martin
Hydrological balance and runoff from a montane peat bog traced by water temperature.
Hydrological Sciences Journal. Roč. 69, č. 4 (2024), s. 393-406. ISSN 0262-6667. E-ISSN 2150-3435
Grant CEP: GA ČR(CZ) GA22-12837S
Grant ostatní: AV ČR(CZ) StrategieAV21/20
Program: StrategieAV
Institucionální podpora: RVO:67985874
Klíčová slova: peatlands * runoff formation * catchment hydrology * water balance * water temperature * tracer
Obor OECD: Hydrology
Impakt faktor: 3.5, rok: 2022
Způsob publikování: Omezený přístup
https://www.tandfonline.com/doi/full/10.1080/02626667.2024.2320392

Peatlands 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.
Trvalý link: https://hdl.handle.net/11104/0350980