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A GIS-Based Assessment of Vulnerability to Aeolian Desertification in the Source Areas of the Yangtze and Yellow Rivers

机译:基于GIS的长江黄河源区风沙荒漠化脆弱性评价。

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Aeolian desertification is a kind of land degradation that is characterized by aeolian activity, resulting from the responses of land ecosystems to climate change and anthropogenic disturbances. The source areas of the Yangtze and Yellow Rivers are typical regions of China’s Tibetan Plateau affected by aeolian desertification. We assessed the vulnerability of these areas to aeolian desertification by combining remote sensing with geographical information system technologies. We developed an assessment model with eight indicators, whose weights were determined by the analytical hierarchy process. Employing this model, we analyzed the spatial distribution of vulnerability to aeolian desertification and its changes from 2000 to 2010, and discuss the implications. Overall, low-vulnerability land was the most widespread, accounting for 64%, 62%, and 71% of the total study area in 2000, 2005, and 2010, respectively. The degree of vulnerability showed regional differences. In the source areas of the Yangtze River, land with high or very high vulnerability accounted for 17.4% of this sub-region in 2010, versus 2.6% in the source areas of the Yellow River. In the Zoige Basin, almost all of the land had very low to low vulnerability. To understand the change in vulnerability to aeolian desertification, we calculated an integrated vulnerability index ( IVI ). This analysis indicated that the vulnerability to aeolian desertification increased from 2000 to 2005 ( IVI increased from 2.1709 to 2.2463), and decreased from 2005 to 2010 ( IVI decreased from 2.2463 to 2.0057). Increasing regional temperatures appear to be primarily responsible for the change in vulnerability to aeolian desertification throughout the region. The effects of other factors (climatic variation and human activities) differed among the various sub-regions. The implementation of the ecological restoration project has achieved a noticeable effect since 2005. Our results provide empirical support for effort to protect the ecology of this ecologically fragile region.
机译:风沙荒漠化是一种以土地风沙活动为特征的土地退化,这是土地生态系统对气候变化和人为干扰的反应导致的。长江和黄河的源区是中国青藏高原受风沙化影响的典型地区。通过将遥感与地理信息系统技术相结合,我们评估了这些地区对风沙荒漠化的脆弱性。我们开发了具有八个指标的评估模型,其权重由层次分析法确定。利用这种模型,我们分析了2000年至2010年风沙荒漠化脆弱性的空间分布及其变化,并讨论了其含义。总体而言,低脆弱性土地分布最广,在2000年,2005年和2010年分别占研究总面积的64%,62%和71%。脆弱程度显示出地区差异。在长江源头地区,高脆弱性或极高脆弱性的土地在2010年占该次区域的17.4%,而黄河源头地区则为2.6%。在Zoige盆地,几乎所有土地的脆弱性都非常低。为了了解风沙化脆弱性的变化,我们计算了综合脆弱性指数(IVI)。该分析表明,对风沙荒漠化的脆弱性从2000年到2005年(IVI从2.1709上升到2.2463)增加,而从2005年到2010年(IVI从2.2463下降到2.0057)下降。区域温度升高似乎是造成整个区域风沙荒漠化脆弱性变化的主要原因。其他因素(气候变化和人类活动)的影响在各个次区域之间有所不同。自2005年以来,生态修复项目的实施取得了显著成效。我们的结果为保护这一生态脆弱地区的生态工作提供了经验支持。

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