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| DOI | 10.1080/02626667.2024.2320392 |
| Hydrological balance and runoff from a montane peat bog traced by water temperature | |
| 发表日期 | 2024 |
| ISSN | 0262-6667 |
| EISSN | 2150-3435 |
| 起始页码 | 69 |
| 结束页码 | 4 |
| 卷号 | 69期号:4 |
| 英文摘要 | 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 (1523 versus 1327 mm/year on the mineral hillslope). The results of this study enable more reliable modelling assessments of peatland reactions to climate change. |
| 英文关键词 | peatlands; runoff formation; catchment hydrology; water balance; water temperature; tracer |
| 语种 | 英语 |
| WOS研究方向 | Water Resources |
| WOS类目 | Water Resources |
| WOS记录号 | WOS:001182636800001 |
| 来源期刊 | HYDROLOGICAL SCIENCES JOURNAL
 |
| 文献类型 | 期刊论文 |
| 条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/286930 |
| 作者单位 | Czech Academy of Sciences; Institute of Hydrodynamics of the Czech Academy of Sciences; Charles University Prague |
| 推荐引用方式 GB/T 7714 | . Hydrological balance and runoff from a montane peat bog traced by water temperature[J],2024,69(4). |
| APA | (2024).Hydrological balance and runoff from a montane peat bog traced by water temperature.HYDROLOGICAL SCIENCES JOURNAL,69(4). |
| MLA | "Hydrological balance and runoff from a montane peat bog traced by water temperature".HYDROLOGICAL SCIENCES JOURNAL 69.4(2024). |
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