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Variability of spatial-temporal character of ice rain in recent decades

机译:近几十年来冰雨的时空变化特征

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This study firstly examines fifty three times processes of ice rain chose from the period 1978–2002, defines the incidental region and discusses its character of the spatial-temporal variability in recent decades. The results show the time series of ice rain frequency over the region has a significant trend, with a break point happened in 1990. Then, the number of station that experienced the ice rain and the duration are connected closely, meaning either of them could be used to describe the variability of ice rain. Moreover, through the methods of composite analysis and empirical orthogonal function (EOF), we reveal that the inversion layer is not only the requirement for producing the ice rain, but also it acts as an intensity adjustor for the strength of latter.
机译:这项研究首先研究了从1978年至2002年间选择的53次冰雨过程,定义了偶然的区域,并讨论了其近几十年来的时空变化特征。结果表明,该地区冰雨频率的时间序列具有明显的趋势,发生在1990年是一个转折点。然后,经历冰雨的台站数量和持续时间紧密相连,这意味着它们可能是用来描述冰雨的变化。此外,通过综合分析和经验正交函数(EOF)的方法,我们揭示了反演层不仅是产生冰雨的必要条件,而且还充当了冰雨强度的强度调节器。

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