摘要
柯西河发源于喜马拉雅山脉中部希夏邦马峰北坡的达索普冰川,自喜马拉雅山北侧,穿过整个山体,南至恒河平原,跨中国、尼泊尔和印度3国,是恒河重要的支流,也是南亚地区重要的跨界河流。柯西河流域水系主要由西支的孙科西河、北支的阿润河和东支的塔姆尔河等3条支流构成[1-4]。
The Koshi River originates from the Dasuopu Glacier,which located on the north slope of Xixabangma in the central Himalayas.It crosses the entire mountain range from the north and eventually reaches the Ganges plain in the south.The Koshi River flows through China,Nepal,and India,making it a crucial tributary of the Ganges River and a significant transboundary river in South Asia.
作者
张镱锂
吴雪
高俊刚
李炳元
Zhang,Y.L.;Wu,X.;Gao,J.G.;Li,B.Y.(Institute of Geographic Sciences and Natural Resources Research(IGSNRR),Chinese Academy of Sciences,Beijing 100101,China;University of Chinese Academy of Sciences,Beijing 100049,China;Texas A&M University,Texas 76502,USA)
出处
《全球变化数据学报（中英文）》
CSCD
2022年第4期656-658,V0656-V0658,共6页
Journal of Global Change Data & Discovery
基金
中华人民共和国科学技术部(2019QZKK0603)
中国科学院(XDA20040201)
国家自然科学基金(41371120,41761144081)。
关键词
柯西河流域
边界
希夏邦马峰
珠穆朗玛峰
朋曲
叶如藏布
西藏
Koshi River basin
boundary
Mount Xixabangma
Mount Qomolangma
Pumqu,Yairuzang TibetAutonomousRegion
