Arid
DOI10.1007/s11434-013-5818-y
Water balance estimates of ten greatest lakes in China using ICESat and Landsat data
Zhang GuoQing1,2; Xie HongJie3; Yao TanDong1; Kang ShiChang1
通讯作者Zhang GuoQing
来源期刊CHINESE SCIENCE BULLETIN
ISSN1001-6538
EISSN1861-9541
出版年2013
卷号58期号:31页码:3815-3829
英文摘要

Lake level and area variations are sensitive to regional climate changes and can be used to indirectly estimate water balances of lakes. In this study, 10 of the largest lakes in China, similar to 1000 km(2) or larger, are examined to determine changes in lake level and area derived respectively from ICESat and Landsat data recorded between 2003 and 2009. The time series of lake level and area of Selin Co, Nam Co, and Qinghai Lake in the Tibetan Plateau (TP) and Xingkai Lake in northeastern China exhibit an increasing trend, with Selin Co showing the fastest rise in lake level (0.69 m/a), area (32.59 km(2)/a), and volume (1.25 km(3)/a) among the 10 examined lakes. Bosten and Hulun lakes in the arid and semiarid region of northern China show a decline in both lake level and area, with Bosten Lake showing the largest decrease in lake level (-0.43 m/a) and Hulun Lake showing the largest area shrinkage (-35.56 km(2)/a). However, Dongting, Poyang, Taihu, and Hongze lakes in the mid-lower reaches of the Yangtze River basin present seasonal variability without any apparent tendencies. The lake level and area show strong correlations for Selin Co, Nam Co, Qinghai, Poyang, Hulun, and Bosten lakes (R (2) > 0.80) and for Taihu, Hongze, and Xingkai lakes (similar to 0.70) and weak correlation for East Dongting Lake (0.37). The lake level changes and water volume changes are in very good agreement for all lakes (R (2) > 0.98). Water balances of the 10 lakes are derived on the basis of both lake level and area changes, with Selin Co, Nam Co, Qinghai, and Xingkai lakes showing positive water budgets of 9.08, 4.07, 2.88, and 1.09 km(3), respectively. Bosten and Hulun lakes show negative budgets of -3.01 and -4.73 km(3), respectively, and the four lakes along the Yangtze River show no obvious variations. Possible explanations for the lake level and area changes in these four lakes are also discussed. This study suggests that satellite remote sensing could serve as a fast and effective tool for estimating lake water balance.


英文关键词water balance lakes ICESat Tibetan Plateau
类型Article
语种英语
国家Peoples R China ; USA
收录类别SCI-E
WOS记录号WOS:000326823500012
WOS关键词NAM CO BASIN ; POYANG LAKE ; TIBETAN PLATEAU ; ELEVATION CHANGES ; INDEX NDWI ; RANGE ; 1970S ; OCEAN ; RIVER
WOS类目Multidisciplinary Sciences
WOS研究方向Science & Technology - Other Topics
来源机构中国科学院青藏高原研究所
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/176412
作者单位1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China;
2.E China Inst Technol, Dept Geol Sci, Nanchang 330013, Peoples R China;
3.Univ Texas San Antonio, Lab Remote Sensing & Geoinformat, San Antonio, TX 78249 USA
推荐引用方式
GB/T 7714
Zhang GuoQing,Xie HongJie,Yao TanDong,et al. Water balance estimates of ten greatest lakes in China using ICESat and Landsat data[J]. 中国科学院青藏高原研究所,2013,58(31):3815-3829.
APA Zhang GuoQing,Xie HongJie,Yao TanDong,&Kang ShiChang.(2013).Water balance estimates of ten greatest lakes in China using ICESat and Landsat data.CHINESE SCIENCE BULLETIN,58(31),3815-3829.
MLA Zhang GuoQing,et al."Water balance estimates of ten greatest lakes in China using ICESat and Landsat data".CHINESE SCIENCE BULLETIN 58.31(2013):3815-3829.
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