1. Lake evaporation and its effects on basin evapotranspiration and lake water storage on the inner Tibetan Plateau
- Author
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Liuming Wang, Junxiao Wang, and Xingong Li
- Abstract
Effects of lake evaporation (EW) on basin evapotranspiration (ETB) and lake water storage change (△SW) at lake-basin scale have never been reported for most basins on the inner Tibetan Plateau (IB). In this study, EW of 117 large lakes in 95 closed lake-basins were estimated, and its effects on ETB and △SW over 2001-2018 were examined using several newly derived diagnostic equations from the aspects of EW amount, rate, trend slope and inter-annual variability. The significant increasing trend (0.29 ± 0.04 km3/a) in annual EW amount is mainly caused by increase (224.65 km2/a) in lake area (82.13%), and increase (2.12 ± 1.28 mm/a) in EW rate is responsible for the rest (17.87%). EW accounts for 23.16% ± 4.94% of the ETB (107.24 ± 21.90 km3) for the 95 basins, and its impact has increased significantly (0.20% ± 0.09%/a). The increasing trends of EW rate and lake area ratio (0.06%, P < 0.05) contributed 14.49% and 52.69% to the increase trend in ETB (0.85 mm/a), and their variances contributed 1.60% ~ 4.79% and 1.64% ~ 6.50% to ETB variance (155.44 ± 107.97 mm2), respectively. The contribution of EW, quasi lake inflow (RL, 23.48 km3), and lake surface precipitation (PW, 9.18 km3) to mean △SW (7.82 km3) are -43.02%, 40.84% and 15.96%, respectively. The increasing trends of the three components (EW, RL and PW) account for -58.02%, 29.59% and 12.39% of the decrease trend in annual △SW (-0.81 × 10 km3/a, P > 0.05), respectively., The 28th IUGG General Assembly (IUGG2023) (Berlin 2023)
- Published
- 2023