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Aeolian desertification monitoring in the Source Region of Yellow River by remote sensing technology

机译:遥感技术遥感技术中黄河源区中的风沙荒漠化监测

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The Source Region of Yellow River locates in the hinterland of Qinghai-Tibet Plateau, which is especially sensitive to global environment change because of its high elevation and cold environment. Under the influence of global warming, aeolian desertified land expanded rapidly in this area during the last decades. To assess the trends of aeolian desertification from 1975 to 2005, we employed remote sensing and GIS technology to monitor the extent of aeolian desertification at four times (1975, 1990, 2000, and 2005). The data sources included Landsat multi-spectral scanner (MSS) images acquired in 1975 with an 80-m spatial resolution, Enhanced Thematic Mapper (ETM+) images acquired in 2000 with a 30-m resolution, and Thematic Mapper (TM) images acquired in 1990 and 2005 with a 30-m spatial resolution. The remote sensing monitoring result shows that the area of aeolian desertification land increased rapidly between 1975 and 1990, kept stable between 1990 and 2000, and turned to decrease slightly between 2000 and 2005.
机译:黄河的源区位于青藏高原的腹地,对全球环境变化特别敏感,因为其高海拔和寒冷的环境。在全球变暖的影响下,在过去几十年中,Aeolian荒漠化土地在这一领域迅速扩大。为评估1975年至2005年的风沙荒漠化趋势,我们采用了遥感和GIS技术来监测四次地区荒漠化的程度(1975年,1990年,2000年和2005年)。数据源包括在1975年获取的LANDSAT多光谱扫描仪(MSS)图像,其具有80米的空间分辨率,增强的专题映射器(ETM +)图像,其分辨率为30米,并且在其中获取的主题映射器(TM)图像1990年和2005年,空间分辨率为30米。遥感监测结果表明,1975年至1990年间,海湾荒漠化土地的面积迅速增加,1990年至2000年间保持稳定,并转动2000年至2005年之间略微下降。

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