Attribution of the Tibetan Plateau to northern drought

被引：1

作者：

Yuzhi Liu ^{[1
]}

Yaohui Li ^{[2
]}

Jianping Huang ^{[1
]}

Qingzhe Zhu ^{[1
]}

Shanshan Wang ^{[2
]}

机构：

[1] Key Laboratory for Semi-Arid Climate Change of the Ministry of Education, Lanzhou University

[2] Institute of Arid Meteorology China Meteorology Administration

来源：

NationalScienceReview | 2020年 / 7卷 / 03期

基金：

中国国家自然科学基金;

关键词：

Attribution of the Tibetan Plateau to northern drought;

D O I：

暂无

中图分类号：

P426.616 [降水引起的灾害];

学科分类号：

摘要：

The Tibetan Plateau (TP), which is located in Asia and has an average elevation of over 4000 m, acts as a raised source of heat [1] and an isolated region of humidity in the atmosphere [2]. The TP serves as a ‘world water tower’ because it stores large amounts of water as glaciers,lakes and rivers [2]. Furthermore, pre-

引用

页码：489 / 492

页数：4

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