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DOI | 10.1016/j.jhydrol.2021.126314 |
Spatial-temporal trends of hydrological transitions in thermokarst lakes on Northeast Qinghai-Tibet Plateau based on stable isotopes | |
Yang, Yuzhong; Wu, Qingbai![]() | |
发表日期 | 2021 |
ISSN | 0022-1694 |
EISSN | 1879-2707 |
卷号 | 597 |
英文摘要 | Regarded as the water towers of numerous large rivers in Asia, the Source Area of Yellow River (SAYR) on Northeast Qinghai-Tibet Plateau (QTP) contains substantial thermokarst lakes, which have exerted significant roles on the regional hydrology and water resources under permafrost degradation. To address the potential impact of climate- and permafrost-induced changes in surface hydrological processes in the SAYR, the hydrological transitions and water balance of thermokarst lakes were characterized on large scales during three years using stable isotope method. Spatial and seasonal deviations in hydrological processes of thermokarst lakes were remarkable. Calculations of evaporation-to-inflow (E/I) ratios based on an isotope-mass balance model revealed substantial evaporation for all thermokarst lakes during June due to the control of climate conditions and limited input water. Substantial feeds from summer/fall rain and permafrost meltwater resulted in lower evaporation and positive water balance of lakes during July, August, September, and October. Based on the relationship between lake-specific input water isotope compositions (delta(I)) and annual average isotope value of precipitation (delta(P)), the recharge patterns of thermokarst lakes in the SAYR were classified: supra-permafrost water/rainfall-dominated lakes were mainly concentrated during June and October regardless of spatial divergences, and summer precipitation/permafrost thaw-dominated lakes are popular during July and August. Qualitatively, seasonal diversities in the water balance of thermokarst lakes are combinatively controlled by air temperature, precipitation regimes, permafrost degradation in the SAYR. Lastly, the future hydrological trajectories of thermokarst lakes are expected under climatic warming and permafrost degradation. This study serves as an important contribution for understanding future hydrological changes and allocation of water resources on the QTP, as well as an indication of permafrost degradation under climate warming. |
英文关键词 | Thermokarst lakes; Source Area of Yellow River (SAYR); Stable isotopes; Ground ice; Permafrost degradation; Water balance |
语种 | 英语 |
WOS研究方向 | Engineering ; Geology ; Water Resources |
WOS类目 | Engineering, Civil ; Geosciences, Multidisciplinary ; Water Resources |
WOS关键词 | ACTIVE-LAYER HYDROLOGY ; BAYAN HAR MOUNTAINS ; OLD CROW FLATS ; WATER-BALANCE ; YELLOW-RIVER ; THERMAL REGIME ; MASS-BALANCE ; SOURCE AREA ; DISCONTINUOUS PERMAFROST ; ARCTIC LAKES |
WOS记录号 | WOS:000652835600100 |
来源期刊 | JOURNAL OF HYDROLOGY
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来源机构 | 中国科学院西北生态环境资源研究院 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/240239 |
作者单位 | [Yang, Yuzhong; Wu, Qingbai; Jin, Huijun] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Frozen Soil Engn, Lanzhou 730000, Peoples R China; [Yang, Yuzhong; Liu, Fengjing] Michigan Technol Univ, Sch Forest Resources & Environm Sci, Houghton, MI USA; [Yang, Yuzhong; Wu, Qingbai] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Beiluhe Observat Stn Frozen Soil Environm & Engn, Lanzhou, Peoples R China |
推荐引用方式 GB/T 7714 | Yang, Yuzhong,Wu, Qingbai,Liu, Fengjing,et al. Spatial-temporal trends of hydrological transitions in thermokarst lakes on Northeast Qinghai-Tibet Plateau based on stable isotopes[J]. 中国科学院西北生态环境资源研究院,2021,597. |
APA | Yang, Yuzhong,Wu, Qingbai,Liu, Fengjing,&Jin, Huijun.(2021).Spatial-temporal trends of hydrological transitions in thermokarst lakes on Northeast Qinghai-Tibet Plateau based on stable isotopes.JOURNAL OF HYDROLOGY,597. |
MLA | Yang, Yuzhong,et al."Spatial-temporal trends of hydrological transitions in thermokarst lakes on Northeast Qinghai-Tibet Plateau based on stable isotopes".JOURNAL OF HYDROLOGY 597(2021). |
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