Quantifying lake heat storage's impacts on lake evaporation for an alpine deep lake lacking water-temperature-profile observation
文献类型:期刊论文
作者 | Zhang, Fang1,2; Zhang, Xueqin2 |
刊名 | JOURNAL OF HYDROLOGY
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出版日期 | 2025-06-01 |
卷号 | 653页码:132791 |
关键词 | Lake heat storage Energy non-closure problem Eddy Covariance Water temperature profile Lake evaporation Yamzhog Yumco |
ISSN号 | 0022-1694 |
DOI | 10.1016/j.jhydrol.2025.132791 |
产权排序 | 1 |
文献子类 | Article |
英文摘要 | Lake heat storage is essential in regulating lake evaporation's magnitude and seasonal variation. However, its impacts on lake evaporation are inadequately investigated, mainly due to the limited lake-water-temperature- profile observations used to calculate lake heat storage, challenging the accurate quantification of lake evaporation. Hence, we integrate multiple-source observations and multiple-model simulations to quantify lake heat storage and its impacts on lake evaporation in the ice-free period for Yamzhog Yumco, an alpine deep lake in the southern Tibetan Plateau. We first calculate lake heat storage based on a regression relationship between the modeled (Rn - G) and EC-observed (H + LE) to deal with the energy non-closure problem inherent in the EC system. Then, we quantify lake heat storage's impacts on evaporation using multiple evaporation estimation models with lake heat storage considered or not and observations of three types of evaporators. The PE-III model can optimally estimate lake evaporation when considering lake heat storage. By contrast, the average daily evaporation is overestimated before early October while underestimating afterward with models neglecting lake heat storage, peaking 4-6 months earlier than EC observation. Besides, the observed evaporation differences between the EC technique and three types of evaporators vary with the evaporator scale related to heat storage magnitude. We also reveal that net radiation and heat storage capacity jointly control lake heat storage, whose impacts on lake evaporation are prominent when deepening lake depth. Our findings provide a framework to quantify lake heat storage and its impacts on lake evaporation over alpine deep lakes lacking water-temperature- profile observations, hopefully improving the accuracy of lake evaporation estimation and deepening the understanding of lake water and heat balance. |
URL标识 | 查看原文 |
WOS关键词 | SURFACE-ENERGY FLUXES ; TIBETAN PLATEAU ; SONIC ANEMOMETER ; BALANCE ; RESERVOIRS ; QUALITY ; LOSSES ; LEVEL ; MODEL |
WOS研究方向 | Engineering ; Geology ; Water Resources |
语种 | 英语 |
WOS记录号 | WOS:001423392500001 |
出版者 | ELSEVIER |
源URL | [http://ir.igsnrr.ac.cn/handle/311030/212272] ![]() |
专题 | 陆地表层格局与模拟院重点实验室_外文论文 |
通讯作者 | Zhang, Xueqin |
作者单位 | 1.Univ Chinese Acad Sci, 19A,Yuquan Rd, Beijing 100049, Peoples R China 2.Inst Geog Sci & Nat Resources Res, Key Lab Land Surface Pattern & Simulat, 11A,Datun Rd, Beijing 100101, Peoples R China; |
推荐引用方式 GB/T 7714 | Zhang, Fang,Zhang, Xueqin. Quantifying lake heat storage's impacts on lake evaporation for an alpine deep lake lacking water-temperature-profile observation[J]. JOURNAL OF HYDROLOGY,2025,653:132791. |
APA | Zhang, Fang,&Zhang, Xueqin.(2025).Quantifying lake heat storage's impacts on lake evaporation for an alpine deep lake lacking water-temperature-profile observation.JOURNAL OF HYDROLOGY,653,132791. |
MLA | Zhang, Fang,et al."Quantifying lake heat storage's impacts on lake evaporation for an alpine deep lake lacking water-temperature-profile observation".JOURNAL OF HYDROLOGY 653(2025):132791. |
入库方式: OAI收割
来源:地理科学与资源研究所
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