Vertical distribution changes in land cover between 1990 and 2015 within the Koshi River Basin, Central Himalayas

被引:2
|
作者
Wu Xue [1 ,2 ]
Paudel Basanta [1 ]
Zhang Yili [1 ,3 ]
Liu Linshan [1 ]
Wang Zhaofeng [1 ,3 ]
Xie Fangdi [1 ]
Gao Jungang [4 ]
Sun Xiaomin [2 ]
机构
[1] Chinese Acad Sci, Key Lab Land Surface Pattern & Simulat, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
[2] Chinese Acad Sci, Key Lab Ecosyst Network Observat & Modeling, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
[3] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[4] Texas A&M AgriLife, Blackland Res & Extens Ctr, Temple, TX 76502 USA
基金
中国国家自然科学基金;
关键词
vertical belt; land cover; Central Himalayas; Koshi River Basin; climate change; MT. QOMOLANGMA EVEREST; CLIMATE-CHANGE; VEGETATION; BELTS; INDEX; NDVI;
D O I
10.1007/s11442-021-1904-2
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The study of mountain vertical natural belts is an important component in the study of regional differentiation. These areas are especially sensitive to climate change and have indicative function, which is the core of three-dimensional zonality research. Thus, based on high precision land cover and digital elevation model (DEM) data, and supported by MATLAB and ArcGIS analyses, this paper aimed to study the present situation and changes of the land cover vertical belts between 1990 and 2015 on the northern and southern slopes of the Koshi River Basin (KRB). Results showed that the vertical belts on both slopes were markedly different from one another. The vertical belts on the southern slope were mainly dominated by cropland, forest, bare land, and glacier and snow cover. In contrast, grassland, bare land, sparse vegetation, glacier and snow cover dominated the northern slope. Study found that the main vertical belts across the KRB within this region have not changed substantially over the past 25 years. In contrast, on the southern slope, the upper limits of cropland and bare land have moved to higher elevation, while the lower limits of forest and glacier and snow cover have moved to higher elevation. The upper limit of alpine grassland on the northern slope retreated and moved to higher elevation, while the lower limits of glacier and snow cover and vegetation moved northward to higher elevations. Changes in the vertical belt were influenced by climate change and human activities over time. Cropland was mainly controlled by human activities and climate warming, and the reduced precipitation also led to the abandonment of cropland, at least to a certain extent. Changes in grassland and forest ecosystems were predominantly influenced by both human activities and climate change. At the same time, glacier and snow cover far away from human activities was also mainly influenced by climate warming.
引用
收藏
页码:1419 / 1436
页数:18
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