毛 飞, 孙 涵, 张艳红, 卢志光, 侯英雨, 张佳华. 近20年藏北草地地表参数动态变化研究[J]. 农业工程学报, 2008, 24(4).
    引用本文: 毛 飞, 孙 涵, 张艳红, 卢志光, 侯英雨, 张佳华. 近20年藏北草地地表参数动态变化研究[J]. 农业工程学报, 2008, 24(4).
    Mao Fei, Sun Han, Zhang Yanhong, Lu Zhiguang, Hou Yingyu, Zhang Jiahua. Dynamic changes of land surface variables on grassland in Northern Tibet in recent 20 years[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2008, 24(4).
    Citation: Mao Fei, Sun Han, Zhang Yanhong, Lu Zhiguang, Hou Yingyu, Zhang Jiahua. Dynamic changes of land surface variables on grassland in Northern Tibet in recent 20 years[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2008, 24(4).

    近20年藏北草地地表参数动态变化研究

    Dynamic changes of land surface variables on grassland in Northern Tibet in recent 20 years

    • 摘要: 草地的覆盖度、地表反照率和地表温度是评价、监测牧草生长状况和草地退化的重要参数。利用1982~2000年NOAA/AVHRR 1、2、4、5通道的10天合成资料以及常用的遥感反演和统计方法,分析了近20年藏北那曲地区3个参数的时空变化规律。主要结果:植被区内牧草覆盖度0.1~0.95,年变率-0.012~0.012 a-1,24%的草地在退化,变异系数0.05~0.6,植被覆盖度与变异系数成反比;6~9月平均地表反照率0.152~0.300,年变率-0.009~0.007 a-1,51%的草地在退化,变异系数0.02~0.23;7~8月平均地表温度20~44℃。结论:植被生长越好,植被覆盖度越高,地表反照率越小,地表温度越低。每个参数均可单独评价和监测草地退化,但综合考虑各个参数将更客观、更合理。

       

      Abstract: The vegetation cover, surface reflectance and surface temperature on grassland are important factors for assessment and monitoring of grass growing and grassland degradation. Using 10-day composite data of NOAA/AVHRR channels 1, 2, 4 and 5 in 1982-2000 and common methods of remote sensing retrieval and statistic, spatial-temporal variation of above three factors in Naqu of Northern Tibet in recent 20 years were analyzed. The main results showed that the vegetation cover in vegetation region changed between 0.10 and 0.95. Its annual variability changed between -0.012a-1 and 0.012a-1 and its variation coefficients changed between 0.05 and 0.60 and the grassland of 24% of vegetation region degraded. The more the vegetation cover was, the less variation coefficient was. The mean surface reflectance from June to September changed between 0.152 and 0.300. Its annual variability changed between -0.009a-1 and 0.007a-1 and its variation coefficients changed between 0.02 and 0.23 and the grassland of 51% of vegetation region degraded. The mean surface temperature from July to August changed between 20℃ and 27℃. The conclusions show that the better the vegetation grows, the more the vegetation cover is and the smaller the surface reflectance is and the lower the surface temperature is. Although grassland degradation can be assessed and monitored by only one in three factors, it is assessed and monitored by three or more factors is more objective and reasonable.

       

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