Articles | Volume 28, issue 1
https://doi.org/10.5194/hess-28-163-2024
https://doi.org/10.5194/hess-28-163-2024
Research article
 | 
10 Jan 2024
Research article |  | 10 Jan 2024

Evaporation and sublimation measurement and modeling of an alpine saline lake influenced by freeze–thaw on the Qinghai–Tibet Plateau

Fangzhong Shi, Xiaoyan Li, Shaojie Zhao, Yujun Ma, Junqi Wei, Qiwen Liao, and Deliang Chen

Data sets

ERA5-Land hourly data from 1950 to present J. Muñoz Sabater https://doi.org/10.24381/cds.e2161bac

China meteorological forcing dataset (1979-2018) K. Yang et al. https://doi.org/10.11888/AtmosphericPhysics.tpe.249369.file

River lake ice phenology data in QPT V1.0 (2002-2018) Y. Qiu https://doi.org/10.11888/Meteoro.tpdc.270236

Model code and software

Clocks-Shi/Code-for-hess-2023-100: Evaporation and sublimation measurement and modeling of an alpine saline lake influenced by freeze–thaw on the Qinghai–Tibet Plateau F. Z. Shi https://doi.org/10.5281/zenodo.10464766

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Short summary
(1) Evaporation under ice-free and sublimation under ice-covered conditions and its influencing factors were first quantified based on 6 years of eddy covariance observations. (2) Night evaporation of Qinghai Lake accounts for more than 40 % of the daily evaporation. (3) Lake ice sublimation reaches 175.22 ± 45.98 mm, accounting for 23 % of the annual evaporation. (4) Wind speed weakening may have resulted in a 7.56 % decrease in lake evaporation during the ice-covered period from 2003 to 2017.