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Quantitative Assessment of Desertification Using Landsat Data on a Regional Scale – A Case Study in the Ordos Plateau, China

机译:利用Landsat数据在区域范围内对荒漠化进行定量评估–以中国鄂尔多斯高原为例

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Desertification is a serious threat to the ecological environment and social economy in our world and there is a pressing need to develop a reasonable and reproducible method to assess it at different scales. In this paper, the Ordos Plateau in China was selected as the research region and a quantitative method for desertification assessment was developed by using Landsat MSS and TM/ETM+ data on a regional scale. In this method, NDVI, MSDI and land surface albedo were selected as assessment indicators of desertification to represent land surface conditions from vegetation biomass, landscape pattern and micrometeorology. Based on considering the effects of vegetation type and time of images acquired on assessment indictors, assessing rule sets were built and a decision tree approach was used to assess desertification of Ordos Plateau in 1980, 1990 and 2000. The average overall accuracy of three periods was higher than 90%. The results showed that although some local places of Ordos Plateau experienced an expanding trend of desertification, the trend of desertification of Ordos Plateau was an overall decrease in from 1980 to 2000. By analyzing the causes of desertification processes, it was found that climate change could benefit for the reversion of desertification from 1980 to 1990 at a regional scale and human activities might explain the expansion of desertification in this period; however human conservation activities were the main driving factor that induced the reversion of desertification from 1990 to 2000.
机译:荒漠化对我们世界的生态环境和社会经济构成严重威胁,迫切需要开发一种合理且可再现的方法来对不同规模的荒漠化进行评估。本文以中国鄂尔多斯高原为研究区域,利用Landsat MSS和TM / ETM +数据在区域范围内开发了定量的荒漠化评估方法。该方法选择NDVI,MSDI和地表反照率作为荒漠化评价指标,以植被生物量,景观格局和微气象学为代表地表条件。在考虑植被类型和图像获取时间对评估指标的影响的基础上,建立评估规则集,并采用决策树方法评估鄂尔多斯高原在1980、1990和2000年的荒漠化。三个时期的平均总体准确度为高于90%。结果表明,尽管鄂尔多斯高原某些地方出现了荒漠化的扩大趋势,但从1980年到2000年,鄂尔多斯高原的荒漠化趋势总体上有所减少。通过分析荒漠化过程的成因,发现气候变化可以在区域范围内从1980年到1990年使荒漠化恢复受益,人类活动可能解释了这一时期荒漠化的扩大;然而,人类保护活动是促使荒漠化从1990年到2000年恢复的主要驱动因素。

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