Abstract
AbstractLake ice sublimation plays an important role in lake water budget, while there is huge uncertainty in estimation of lake ice sublimation and its proportion in annual lake total water vapor flux. In the present study, we investigated the annual total water vapor flux and ice sublimation at 15 frozen lakes or lake groups in China using three different methods, namely, the Community Land Model (CLM) simulations (Penman‐Monteith equation and pan observations) that considers (could not reflect) heat storage of lakes; the potential changes of lake total water vapor flux and ice sublimation with climate warming were also predicted. The results illustrate that the annual lake total water vapor flux obtained from Penman‐Monteith equation, pan observation, CLM simulation decreased in sequence, and ice sublimation obtained from pan observation, Penman‐Monteith equation, CLM simulation decreased in sequence. The lake ice sublimation from CLM occupied 7.4%–26.6% of corresponding annual lake total water vapor flux during 1950s–2010s in different regions of China. The ice sublimation and its proportion in lake total water vapor flux from these three methods were all highly correlated, with R2 being 0.86–0.97. The annual lake total water vapor flux will significantly increase in all frozen‐lake regions in China with the climate warming. Climate warming potentially reduce sublimation at most lakes.
Published Version
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