Hydrological balance and runoff from a montane peat bog traced by water temperature
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985874%3A_____%2F24%3A00582936" target="_blank" >RIV/67985874:_____/24:00582936 - isvavai.cz</a>
Alternative codes found
RIV/00216208:11310/24:10478388
Result on the web
<a href="https://www.tandfonline.com/doi/full/10.1080/02626667.2024.2320392" target="_blank" >https://www.tandfonline.com/doi/full/10.1080/02626667.2024.2320392</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1080/02626667.2024.2320392" target="_blank" >10.1080/02626667.2024.2320392</a>
Alternative languages
Result language
angličtina
Original language name
Hydrological balance and runoff from a montane peat bog traced by water temperature
Original language description
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.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10501 - Hydrology
Result continuities
Project
<a href="/en/project/GA22-12837S" target="_blank" >GA22-12837S: Hydrological and hydrochemical response of montane peat bogs to climate change</a><br>
Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2024
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Hydrological Sciences Journal
ISSN
0262-6667
e-ISSN
2150-3435
Volume of the periodical
69
Issue of the periodical within the volume
4
Country of publishing house
GB - UNITED KINGDOM
Number of pages
14
Pages from-to
393-406
UT code for WoS article
001182636800001
EID of the result in the Scopus database
2-s2.0-85187454207