中国冰冻圈水文未来变化及其对干旱区水安全的影响
丁永建1,2,3(
), 赵求东1,2(), 吴锦奎2, 张世强4,5, 王生霞2, 苌亚平2, 李向应6, 上官冬辉1, 韩海东2, 秦甲2, 韩添丁1
), 赵求东1,2(), 吴锦奎2, 张世强4,5, 王生霞2, 苌亚平2, 李向应6, 上官冬辉1, 韩海东2, 秦甲2, 韩添丁1
The future changes of Chinese cryospheric hydrology and their impacts on water security in arid areas
Yongjian DING1,2,3(), Qiudong ZHAO1,2(), Jinkui WU2, Shiqiang ZHANG4,5, Shengxia WANG2, Yaping CHANG2, Xiangying LI6, Donghui SHANGGUAN1, Haidong HAN2, Jia QIN2, Tianding HAN1
), Qiudong ZHAO1,2(), Jinkui WU2, Shiqiang ZHANG4,5, Shengxia WANG2, Yaping CHANG2, Xiangying LI6, Donghui SHANGGUAN1, Haidong HAN2, Jia QIN2, Tianding HAN1
图3. 干旱区部分流域现有冰川数量及RCP4.5情景下可能消失的冰川比例（数据来源： 文献［
Fig.3. The numbers in existence and disappearance proportions of glaciers under RCP4.5 global emission scenario in the Tianshan Mts.， Altay Mts. and Qilian Mts. （data source： Reference ［
