首页> 外文会议>International symposium on multispectral image processing and pattern recognition;MIPPR 2009 >Characterizing snow cover interannual variability with Empirical Orthogonal Function (EOF) analysis and its climate effect in the inland region, northwest China
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Characterizing snow cover interannual variability with Empirical Orthogonal Function (EOF) analysis and its climate effect in the inland region, northwest China

机译:利用经验正交函数(EOF)分析表征积雪的年际变化及其在中国内陆地区的气候效应

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Satellite images and field temperature data have been used to derive the winter snow cover change in the northwest inland regions for the period 1978-2005. Decomposition of the satellite-derived snow depth field yields several statistically-significant EOFs (modes) and spectrums of variability according to the selection rule. The first three leading EOF modes account for 63%, 5%, and 4% of the total variance respectively. Spatially, their sensitive regions are characterized significantly with slope orientation, EOF1 towards northwest, EOF2 towards south and EOF3 towards southeast. A primary analysis shows the three modes can be explained by the precipitation events induced by the water vapor conveyed by atmospheric circulation originated from northwest, south and southeast oceans accordingly. As for the temporal dimension, EOF1 shows evidently different from EOF2 and EOF3, and services as a stable process during the 27 years. Their temporal processes correlate temperature in a complicated way. On the whole, the temperature correlates EOF 1, EOF2 and EOF3 more significantly, which indicates the impact of climate warming to the snow cover is, to some extent, acted with circulation originated from different orientations, or as a result of their interactions.
机译:卫星图像和野外温度数据已用于推算西北内陆地区1978-2005年期间的冬季积雪变化。根据选择规则,分解源自卫星的雪深场会产生几个具有统计意义的EOF(模式)和可变性频谱。前三个领先的EOF模式分别占总方差的63%,5%和4%。在空间上,它们的敏感区域具有明显的坡度特征,EOF1朝西北,EOF2朝南,EOF3朝东南。初步分析表明,这三种模式可以解释为由西北,南部和东南部海洋相应产生的大气环流输送的水蒸气引起的降水事件。至于时间维度,EOF1显示出与EOF2和EOF3明显不同,并且在27年中是稳定的过程。它们的时间过程以复杂的方式将温度关联起来。总体而言,温度与EOF 1,EOF2和EOF3的相关性更强,这表明气候变暖对积雪的影响在一定程度上与源自不同方向的环流或它们相互作用的结果有关。

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