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DOI10.1016/j.earscirev.2018.06.012
Linkages of the dynamics of glaciers and lakes with the climate elements over the Tibetan Plateau
Sun, Jian; Zhou, Tiancai; Liu, Miao; Chen, Youchao; Shang, Hua; Zhu, Liping; Shedayi, Arshad Ali; Yu, Huan; Cheng, Genwei; Liu, Guohua; Xu, Ming; Deng, Wei; Fan, Jihui; Lu, Xuyang; Sha, Yukun
通讯作者Sun, J ; Zhu, LP (通讯作者)
发表日期2018
ISSN0012-8252
EISSN1872-6828
起始页码308
结束页码324
卷号185
英文摘要Future climate warming is expected to have a significant effect on the operation of Earth and Ecological systems. A key concern in the future is water resource availability. In regions such as the Tibet Plateau (TP) lakes and glaciers appear to be highly sensitive to climate forcing and variations in the size and extent of these system will have profound socio-economic and environmental consequences in South and Central Asia. Although the variety of glaciers and lake son the TP is a heavily researched and discussed topic the interaction between glaciers/lakes and climate change has not be thoroughly investigated. Here we present, through a review of existing studies and original remote sensing analysis, a reconstruction of changes in the spatial coverage of glaciers and lakes on the TP from 1990 to 2015 along with an analysis of climate data for the same period. The results revealed that these systems responded to changes in both temperature and precipitation but the nature of this response, and the controlling factor, was spatially diverse. During this interval the total number of lakes increased from 868 to 1207, thus a large number of new lakes (n = 339) formed. The total water surface area of the lakes increase from 38,823.3 km(2) in 1990 to 48,793.0 km(2) in 2015, at a rate of 383.5 km(2) yr(-1). Over this period intensive glacial shrinkage occurred, primarily driven by increasing average temperature, except in the Karakoram Mountains where a slight increase in glacier extent was explained by low and stable temperatures along with increasing precipitation. The expansion of lakes in the central and northeastern TP can, therefore, be explained by a trend of increasing precipitation and the accelerated melting of glaciers associated with rising temperatures, both of which contributed to the enhanced total basin runoff. The shrinkage of lake areas along the Himalayan Mountains is accounted for by low precipitation coupled with high evaporation and limited basin space. The lakes within the Qaidam Basin express a complex pattern of response in association with fluctuating precipitation and strong evaporation. The pattern of shrinking glaciers and expanding lakes indicate that water cycle processes on the TP have been accelerating during the past 25 years. Under current climates, and future climate change, the shrinkage of glaciers and the enlargement of lakes may be expected to continue to accelerate until a tipping point is reached when the meltwater of declining glaciers can no longer sustain the enhanced lake levels. Such a scenario would have severe socio-economic and ecological consequences for this region making the continued study of water-cycle activity across the TP an urgent priority.
关键词NAM CO LAKEMT. QOMOLANGMA REGIONWATER STORAGE CHANGESMASS-BALANCEMONITORING GLACIERHAILUOGOU GLACIERQILIAN MOUNTAINSLEVEL CHANGESNYAINQENTANGLHA RANGEQUANTITATIVE-ANALYSIS
英文关键词Tibetan Plateau; Lakes and glaciers; Regional climate; Water resource
语种英语
WOS研究方向Geology
WOS类目Geosciences, Multidisciplinary
WOS记录号WOS:000448493500016
来源期刊EARTH-SCIENCE REVIEWS
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/259349
推荐引用方式
GB/T 7714
Sun, Jian,Zhou, Tiancai,Liu, Miao,et al. Linkages of the dynamics of glaciers and lakes with the climate elements over the Tibetan Plateau[J]. 中国科学院青藏高原研究所,2018,185.
APA Sun, Jian.,Zhou, Tiancai.,Liu, Miao.,Chen, Youchao.,Shang, Hua.,...&Sha, Yukun.(2018).Linkages of the dynamics of glaciers and lakes with the climate elements over the Tibetan Plateau.EARTH-SCIENCE REVIEWS,185.
MLA Sun, Jian,et al."Linkages of the dynamics of glaciers and lakes with the climate elements over the Tibetan Plateau".EARTH-SCIENCE REVIEWS 185(2018).
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