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首页> 外文期刊>Mountain Research & Development >Spatial-Temporal NDVI Variation of Different Alpine Grassland Classes and Groups in Northern Tibet from 2000 to 2013
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Spatial-Temporal NDVI Variation of Different Alpine Grassland Classes and Groups in Northern Tibet from 2000 to 2013

机译:2000年至2013年藏北地区不同高山草地类型和种群的时空NDVI变化

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The Normalized Difference Vegetation Index (NDVI) can usually be used as a good proxy for evaluating potential variability in regional ecosystems and under climate change. We used 16-day MODIS-NDVI composite satellite data with 250-m resolution for the period 2000 to 2013 to assess the temporal and spatial variation of the NDVI among different alpine grassland classes and groups in northern Tibet. The annual average NDVI of the whole alpine grassland area in northern Tibet generally increased slightly from 2000 to 2003, and the annual average NDVI values ranged from 0.112 to 0.492 across all alpine grassland groups and years. The NDVI clearly decreased from the southeastern to the northwestern areas, with 22.50% of total grasslands significantly having increased or decreased, while 77.50% presented little change during 2000-2013. Both temperature and precipitation were key factors that controlled the NDVI variations of the entire alpine grassland. However, for different alpine grassland classes and groups, the NDVI displayed different correlation patterns with temperature and precipitation. Our results demonstrate that the NDVI variations of alpine grassland generally increased slightly but differed among different classes and groups. Although temperature and precipitation were the driving forces influencing the NDVI of the entire alpine grassland, it was more difficult to define the driving forces for the individual classes and groups, and more detailed analyses covering prolonged observation periods are still needed.
机译:归一化植被指数(NDVI)通常可以用作评估区域生态系统和气候变化下潜在变异性的良好代表。我们使用2000年至2013年期间为期16天的MODIS-NDVI复合卫星数据,其分辨率为250-m,以评估藏北不同高山草地类别和群体之间NDVI的时空变化。从2000年到2003年,西藏北部整个高寒草地地区的年均NDVI总体上略有增加,并且在所有高寒草地种群和年份中,年均NDVI值在0.112至0.492之间。从东南到西北,NDVI明显下降,在2000-2013年期间,总草地的22.50%显着增加或减少,而77.50%的草地几乎没有变化。温度和降水都是控制整个高山草原NDVI变化的关键因素。但是,对于不同的高寒草原类别和群体,NDVI显示出与温度和降水不同的相关模式。我们的结果表明,高寒草地的NDVI变化总体上略有增加,但在不同类别和组之间有所不同。尽管温度和降水是影响整个高寒草原NDVI的驱动力,但要为各个类别和群体定义驱动力更加困难,并且仍需要更详细的分析来涵盖较长的观察期。

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