Abstract
Volume changes and water balances of the lakes on the Tibetan Plateau (TP) are spatially heterogeneous and the lake-basin scale drivers remain unclear. In this study, we comprehensively estimated water volume changes for 1132 lakes larger than 1 km2 and determined the glacier contribution to lake volume change at basin-wide scale using satellite stereo and multispectral images. Overall, the water mass stored in the lakes increased by 169.7 ± 15.1 Gt (3.9 ± 0.4 Gt yr−1) between 1976 and 2019, mainly in the Inner-TP (157.6 ± 11.6 or 3.7 ± 0.3 Gt yr−1). A substantial increase in mass occurred between 1995 and 2019 (214.9 ± 12.7 Gt or 9.0 ± 0.5 Gt yr−1), following a period of decrease (−45.2 ± 8.2 Gt or −2.4 ± 0.4 Gt yr−1) prior to 1995. A slowdown in the rate of water mass increase occurred between 2010 and 2015 (23.1 ± 6.5 Gt or 4.6 ± 1.3 Gt yr−1), followed again by a high value between 2015 and 2019 (65.7 ± 6.7 Gt or 16.4 ± 1.7 Gt yr−1). The increased lake-water mass occurred predominately in glacier-fed lakes (127.1 ± 14.3 Gt) in contrast to non-glacier-fed lakes (42.6 ± 4.9 Gt), and in endorheic lakes (161.9 ± 14.0 Gt) against exorheic lakes (7.8 ± 5.8 Gt) over 1976–2019. Endorheic and glacier-fed lakes showed strongly contrasting patterns with a remarkable storage increase in the northern TP and slight decrease in the southern TP. The ratio of excess glacier meltwater runoff to lake volume increase between 2000 and ~2019 was less than 30% for the entire Inner-TP based on several independent data sets. Among individual lake-basins, 14 showed a glacier contribution to lake volume increase of 0.3% to 29.1%. The other eight basins exhibited a greater glacier contribution of 116% to 436%, which could be explained by decreased net precipitation. The lake volume change and basin scale glacier contribution reveal that the enhanced precipitation predominantly drives lake volume increase but it is spatially heterogeneous.
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