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| DOI | 10.1016/j.scitotenv.2021.145463 |
| Comprehensive estimation of lake volume changes on the Tibetan Plateau during 1976-2019 and basin-wide glacier contribution | |
| Zhang, Guoqing; Bolch, Tobias; Chen, Wenfeng; Cretaux, Jean-Francois | |
| 通讯作者 | Zhang, GQ (通讯作者) |
| 发表日期 | 2021 |
| ISSN | 0048-9697 |
| EISSN | 1879-1026 |
| 卷号 | 772 |
| 英文摘要 | 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 km(2) 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 +/- 82 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 decease in the southern TP. The ratio of excess glacier meltwater runoff to lake volume increase between 2000 and similar to 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. (C) 2021 Elsevier B.V. All rights reserved. |
| 关键词 | WATER STORAGE CHANGESDIGITAL ELEVATION MODELSHIGH-MOUNTAIN ASIANAM CO LAKEREGIONAL CLIMATEMOISTURE FLUXMASS BALANCESLEVEL CHANGESPRECIPITATIONDYNAMICS |
| 英文关键词 | Lake volume change; Glacier mass balance; Lake water balance; Tibetan Plateau |
| 语种 | 英语 |
| WOS研究方向 | Environmental Sciences & Ecology |
| WOS类目 | Environmental Sciences |
| WOS记录号 | WOS:000628753700088 |
| 来源期刊 | SCIENCE OF THE TOTAL ENVIRONMENT
 |
| 来源机构 | 中国科学院青藏高原研究所 |
| 文献类型 | 期刊论文 |
| 条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/260489 |
| 推荐引用方式 GB/T 7714 | Zhang, Guoqing,Bolch, Tobias,Chen, Wenfeng,et al. Comprehensive estimation of lake volume changes on the Tibetan Plateau during 1976-2019 and basin-wide glacier contribution[J]. 中国科学院青藏高原研究所,2021,772. |
| APA | Zhang, Guoqing,Bolch, Tobias,Chen, Wenfeng,&Cretaux, Jean-Francois.(2021).Comprehensive estimation of lake volume changes on the Tibetan Plateau during 1976-2019 and basin-wide glacier contribution.SCIENCE OF THE TOTAL ENVIRONMENT,772. |
| MLA | Zhang, Guoqing,et al."Comprehensive estimation of lake volume changes on the Tibetan Plateau during 1976-2019 and basin-wide glacier contribution".SCIENCE OF THE TOTAL ENVIRONMENT 772(2021). |
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