拉萨河流域高寒湿地分布(英文)

被引:39
作者
张镱锂 [1 ]
王春连 [1 ,2 ]
摆万奇 [1 ]
王兆锋 [1 ]
土艳丽 [3 ]
央珍 [3 ]
机构
[1] Institute of Geographic Sciences and Natural Resource Research(IGSNRR),CAS
[2] Graduate University of Chinese Academy of Sciences
[3] Tibet Plateau Institute of Biology(TPIB)
关键词
Lhasa River Basin; alpine wetland; classification system; distribution; 3S technology;
D O I
暂无
中图分类号
P941.77 [河流];
学科分类号
0705 ; 070501 ;
摘要
The Lhasa River Basin is one of the typical distribution regions of alpine wetlands on the Tibetan Plateau.It is very important to get a better understanding of the background and characteristics of alpine wetland for monitoring,protection and utilization.Wetland construction and distribution in the basin were analyzed based on multi-source data including field investigation data,CBERS remote sensing data and other thematic data provided by 3S technology.The results are(1) the total area of wetlands is 209,322.26 hm2,accounting for 6.37% of the total land area of the basin.The wetlands are mainly dominated by natural wetland,with artificial wetland occupying only 1.09% of the wetland area;marsh wetland is the principal part of natural wetland,dominated by Kobresia littledalei swampy meadow which is distributed in the river source area and upstream of Chali,Damshung and Medro Gongkar counties.The ratio and type of wetlands in different counties differ significantly,which are widely distributed in Chali and Damshung counties(accounting for 62% of the total wetland area).(2) The concentrated vertical distribution of wetlands is at an elevation of 3600-5100 m.The wetlands are widely distributed throughout the Yarlung Zangbo River Valley from river source to river mouth into the Yarlung Zangbo River.Marsh wetland is dominant in the source area and upstream of the river,with the mosaic distribution of lakes,Kobresia littledalei and Carex moorcroftii swampy meadow,shrubby swamp and river;as for the middle-down streams,the primary types are river wetland and flooded wetland.The distribution is in a mosaic pattern of river,Kobresia humilis and Carex moorcroftii swampy meadow,Phragmites australis and subordinate grass marsh,flooded wetland and artificial wetland.
引用
收藏
页码:375 / 388
页数:14
相关论文
共 21 条
[1]   近40年来若尔盖高原高寒湿地景观格局变化 [J].
白军红 ;
欧阳华 ;
崔保山 ;
王庆改 ;
陈辉 .
生态学报, 2008, (05) :2245-2252
[2]   1990—2001年黄河玛曲高寒沼泽湿地遥感动态监测 [J].
蔡迪花 ;
郭铌 ;
韩涛 .
冰川冻土, 2007, (06) :874-881
[3]   长江、黄河源区高寒湿地动态变化研究 [J].
潘竟虎 ;
王建 ;
王建华 .
湿地科学, 2007, (04) :298-304
[4]   近40年来青藏高原典型高寒湿地系统的动态变化 [J].
王根绪 ;
李元寿 ;
王一博 ;
陈玲 .
地理学报, 2007, (05) :481-491
[5]   基于RS和GIS技术青藏高原湖泊动态变化研究 [J].
武慧智 ;
姜琦刚 ;
程彬 .
世界地质, 2007, (01) :66-70
[6]   拉萨地区土地利用变化 [J].
除多 ;
张镱锂 ;
郑度 .
地理学报, 2006, (10) :1075-1083
[7]   若尔盖高原湿地资源变化过程与机制分析 [J].
刘红玉 ;
白云芳 .
自然资源学报, 2006, (05) :810-818
[8]   拉萨河冬季径流对气候变暖和冻土退化的响应 [J].
巩同梁 ;
刘昌明 ;
刘景时 .
地理学报, 2006, (05) :519-526
[9]   流域湿地景观空间梯度格局及其影响因素分析 [J].
刘红玉 ;
李兆富 .
生态学报, 2006, (01) :213-220
[10]   若尔盖高原湿地生态恢复过程中土壤有机质的变化研究 [J].
田应兵 ;
熊明彪 ;
宋光煜 .
湿地科学, 2004, (02) :88-93