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基于遥感信息的中国耕地动态变化和典型区的土地覆盖变化(英文)

Dynamic of Chinas cultivated land and landcover changes of its typical regions based on remote sensing data

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【作者】 张佳华董文杰王长耀刘纪远姚凤梅

【Author】 ZHANG Jia-hua, DONG Wen-jie (The Global Change Research Center for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China) WANG Chang-yao, LIU Ji-yuan Institute of Remote Sensing Application, Chinese Aca

【机构】 中国科学院大气物理所全球变化东亚研究中心中国科学院遥感应用研究所北京林业大学生态工程学院 北京100029北京100029北京100101北京100083

【摘要】 利用多时相的Landsat-TM数据和国家资源调查数据,对我国耕地动态变化和典型区的土地覆盖变化进行了研究,结果显示:我国耕地的分布向东北和西北推移,移动的结果导致耕地的生态背景质量下降。黄河河口的耕地和海岸带扩大,扩大的速度是0.73 kma-1,沉积速率是2.1 kma-1。 对科尔沁沙地的研究结果表明,该区沙化面积从70年代的60.02%上升到80年代的64.82%,但是90年代后沙化面积缩小为54.90%;对藏北的湖泊动态变化研究结果显示,湖泊的面积下降,下降的速度为2.14 km2a-1。

【Abstract】 Using the multi-temporal Landsat data and survey data of national resources, the authors studied the dynamics of cultivated land and landcover changes of typical ecological regions in China. The results of investigation showed that the whole distribution of the cultivated land shifted to Northeast and Northwest China, and as a result, the ecological quality of cultivated land dropped down. The seacoast and cultivated land in the area of Yellow River Mouth expanded by an increasing rate of 0.73 kma-1, with a depositing rate of 2.1 kma-1. The desertification area of the dynamic of Horqin Sandy Land increased from 60.02% of the total land area in1970s to 64.82% in1980s but decreased to 54.90% in early 1990s. As to the change of North Tibet lakes, the water area of the Namu Lake decreased by 38.58 km2 from year 1970 to 1988, with a decreasing rate of 2.14 km2a-1.

【基金】 National Natural Sci-ence Foundation of China (Grant No. 39900084) and KZCX1-10-07.
  • 【文献出处】 Journal of Forestry Research ,林业研究(英文版) , 编辑部邮箱 ,2001年03期
  • 【分类号】S159
  • 【被引频次】3
  • 【下载频次】192
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