globalchange  > 气候变化与战略
CSCD记录号: CSCD:5037532
论文题名:
近30年来长江源区土地覆被变化特征分析
其他题名: Characteristics of Land Cover Change in Headwaters of the Yangtze River over the Past 30 Years
作者: 吴丹; 邵全琴
刊名: 地球信息科学学报
ISSN: 1560-8999
出版年: 2014
卷: 16, 期:1
语种: 中文
中文关键词: 土地覆被 ; 状况指数 ; 转类指数 ; 长江源区
英文关键词: land cover ; condition index ; change index ; headwaters of the Yangtze River
WOS学科分类: ENGINEERING MULTIDISCIPLINARY ; FORESTRY
WOS研究方向: Engineering ; Forestry
中文摘要: 长江源区是我国重要的水源涵养地。本文利用20世纪70年代中后期、90年代初期、2004年和2008年共4期土地覆被数据,通过土地覆被转类途径与幅度、土地覆被状况指数和土地覆被转类指数,分析评价了长江源区近30年来土地覆被与生态状况的时空变化特征。结果表明:草地是长江源区主要的土地覆被类型,2008年草地面积占该区总面积的66.93%。在70年代中后期-90年代初期、90年代初期-2004年和2004-2008年的3个时段内,土地覆被状况指数变化率分别为-0.15、-0.24和0.01;土地覆被转类指数分别为-0.20、-0.66和0.08。近30年来,长江源区土地覆被和生态状况总体经历了变差-显著变差-略有好转的过程。2004-2008年,长江源区年平均温度比前期(70年代中后期-2004年)升高了0.57℃,年平均降水量比前期增加了17.63mm。区域气候变化有助于自然生态系统的恢复。后期生态保护与建设工程的实施,对植被恢复产生了一定的积极作用。
英文摘要: The water conservation service of headwaters of the Yangtze River is very important for ecological se-curity in China. It is generally acknowledged that the source of the Yangtze River includes the Tuotuohe headwa-ter, Dangqu headwater and Chumaerhe headwater. Based on the land cover dataset of middle and late 1970s, ear-ly 1990s, 2004 and 2008, this paper analyzed temporal and spatial change characteristics of land cover and eco-logical condition in headwaters of the Yangtze River over the past 30 years, using the method of direction and ex-tent of land cover change, land cover condition index and land cover change index. The results showed that grass-land was the main land cover type in this region in 2008, with a ratio of 66.93%in area. The glaciers were main-ly distributed in Tuotuohe headwater, while the marshland was mainly distributed in Dangqu headwater. The change rate of land cover condition index during 1970s-1990s, 1990s-2004 and 2004-2008 was-0.15,-0.24 and 0.01, respectively;while the land cover change index of three periods was-0.20,-0.66 and 0.08, respective-ly. The land cover and ecological condition of the study area had overall experienced a process of degenerated-obviously degenerated-slightly meliorated since 1970s. The mean annual temperature and precipitation from 2004 to 2008 was 0.57℃and 17.63mm higher than that from 1970s to 2004. Regional climate change over re-cent years was helpful for natural ecosystem recovery. In addition, implementation of the ecological protection and construction project since 2004 also had certain positive effects on vegetation restoration.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/147622
Appears in Collections:气候变化与战略

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作者单位: 中国科学院地理科学与资源研究所, 北京 100101, 中国

Recommended Citation:
吴丹,邵全琴. 近30年来长江源区土地覆被变化特征分析[J]. 地球信息科学学报,2014-01-01,16(1)
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