中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
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
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
DOI10.1016/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

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。