An integrated investigation of lake storage and water level changes in the Paiku Co basin, central Himalayas
文献类型：期刊论文
| 作者 | Lazhua (Lazhua)2; Wang, L (Wang, Lei)2,3; Lei, YB (Lei, Yanbin)2,3; Yao, TD (Yao, Tandong)2,3; Yang, K (Yang, Kun)3,4; Bird, BW (Bird, Broxton W.)1; Tian, LD (Tian, Lide)2,3; Zhang, XW (Zhang, Xiaowen)2; Wang, WC (Wang, Weicai)2,3; Xiang, Y (Xiang, Yang)2 |
| 刊名 | JOURNAL OF HYDROLOGY
 |
| 出版日期 | 2018-07-01 |
| 卷号 | 562期号:0页码:599-608 |
| 关键词 | CENTRAL TIBETAN PLATEAU NAM CO CLIMATE-CHANGE GLACIERS ENERGY NAIMONANYI DYNAMICS KANGWURE FEATURES EVEREST |
| ISSN号 | 0022-1694 |
| DOI | 10.1016/j.jhydrol.2018.05.040 |
| 英文摘要 | Since the late 1990s, lakes in the southern Tibetan Plateau (TP) have shrunk considerably, which contrasts with the rapid expansion of lakes in the interior TP. Although these spatial trends have been well documented, the underlying hydroclimatic mechanisms are not well understood. Since 2013, we have carried out comprehensive water budget observations at Paiku Co, an alpine lake in the central Himalayas. In this study, we investigate water storage and lake level changes on seasonal to decadal time scales based on extensive in-situ measurements and satellite observations. Bathymetric surveys show that Paiku Co has a mean and maximum water depth of 41.1 m and 72.8 m, respectively, and its water storage was estimated to be 109.3 x 10(8) m(3) in June 2016. On seasonal scale between 2013 and 2017, Paiku Co's lake level decreased slowly between January and May, increased considerably between June and September, and then decreased rapidly between October and January. On decadal time scale, Paiku Co's lake level decreased by 3.7 +/- 0.3 m and water storage reduced by (10.2 +/- 0.8) x 10(8) m(3) between 1972 and 2015, accounting for 8.5% of the total water storage in 1972. This change is consistent with a trend towards drier conditions in the Himalaya region during the recent decades. In contrast, glacial lakes within Paiku Co's basin expanded rapidly, indicating that, unlike Paiku Co, glacial meltwater was sufficient to compensate the effect of the reduced precipitation. |
| WOS研究方向 | Engineering ; Geology ; Water Resources |
| 语种 | 英语 |
| WOS记录号 | WOS:000438003000046 |
| 出版者 | ELSEVIER SCIENCE BV |
| 源URL | [http://ir.itpcas.ac.cn/handle/131C11/8608]  |
| 专题 | 青藏高原研究所_图书馆 |
| 作者单位 | 1.IUPUI, Dept Earth Sci, Indianapolis, IN 46202 USA. 2.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China; 3.CAS Ctr Excellence Tibetan Plateau Earth Syst, Beijing 100101, Peoples R China; 4.Tsinghua Univ, Dept Earth Syst Sci, Beijing 10084, Peoples R China; |
| 推荐引用方式 GB/T 7714 | Lazhua ,Wang, L ,Lei, YB ,et al. An integrated investigation of lake storage and water level changes in the Paiku Co basin, central Himalayas[J]. JOURNAL OF HYDROLOGY,2018,562(0):599-608. |
| APA | Lazhua .,Wang, L .,Lei, YB .,Yao, TD .,Yang, K .,...&Zhou, J .(2018).An integrated investigation of lake storage and water level changes in the Paiku Co basin, central Himalayas.JOURNAL OF HYDROLOGY,562(0),599-608. |
| MLA | Lazhua ,et al."An integrated investigation of lake storage and water level changes in the Paiku Co basin, central Himalayas".JOURNAL OF HYDROLOGY 562.0(2018):599-608. |
入库方式： OAI收割
来源：青藏高原研究所
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