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中国沙漠 ›› 2010, Vol. 30 ›› Issue (3): 505-509.

• 沙漠与沙漠化 • 上一篇    下一篇

长江源区沙漠化土地遥感调查及分析

胡光印, 董治宝, 逯军峰, 宋 翔, 魏振海   

  1. 中国科学院 寒区旱区环境与工程研究所 沙漠与沙漠化重点实验室, 甘肃 兰州 730000
  • 收稿日期:2008-10-27 修回日期:2008-12-01 出版日期:2010-05-20 发布日期:2010-05-20

Desertification Land Survey in Source Region of Yangtze River and Analysis of Its Distribution Characteristics

HU Guang-yin, DONG Zhi-bao, LU Jun-feng, SONG Xiang, WEI Zhen-hai   

  1. Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Science, Lanzhou 730000, China
  • Received:2008-10-27 Revised:2008-12-01 Online:2010-05-20 Published:2010-05-20

摘要: 利用2000年的ETM+影像,在遥感(RS)和地理信息系统(GIS)技术的支持下,对长江源区的沙漠化现状进行了调查。调查结果显示,长江源区沙漠化土地面积为28 982 km2,占整个源区面积的20.43%,其中,极重度沙漠化土地面积为4 241.12 km2,重度沙漠化土地面积为3 996.75 km2,中度沙漠化土地面积为12 716.66 km2,轻度沙漠化土地面积为8 027.16 km2,潜在沙漠化土地面积为92.46 km2。通过坡度分析发现,0°~2°的平地是长江源区的主要坡度类型,也是沙漠化土地主要的分布区域。

关键词: 长江源, 沙漠化, 遥感监测, 青藏高原

Abstract: This study based on the technology of remote sensing (RS) and geographic information system (GIS)surveyed the desertification land in source region of Yangtze River with the purpose of quantifying its distribution status. The result shows that the total area of desertification land is 28 982 km2, accounting for 20.43% of the source region area of Yangtze River. In detail, the area of extremely severe desertification land, severe desertification land, moderate desertification land and light desertification land are 4 241.12 km2, 3 996.75 km2, 12 716.66 km2 and 8 027.16 km2 respectively. In addition, it was found that the land with slope gradient between 0°~2° is the main land type in source region of Yangtze River, where is distributed with most of the desertification land of the study region.

Key words: desertification, remote sensing monitoring, source region of Yangtze River, Qinghai-Tibet Plateau

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