首页> 外文期刊>地理学报(英文版) >1480-1940年广东地区气候干湿变化与旱涝灾害区域分异特征
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1480-1940年广东地区气候干湿变化与旱涝灾害区域分异特征

机译:1480-1940年广东地区气候干湿变化与旱涝灾害区域分异特征

摘要

Based on the historical records of the drought and flood disasters during 1480-1940AD, this paper reconstructs the sequences of wetness index (WI) and drought and flood disasters. We find a good identical relationship between the fluctuation of WI sequence and the δ18O record of the GISP2 ice core in Greenland, which shows an apparent monsoonal disposal pattern of moisture and temperature. By applying the Morlet Wavelet Transform Method to deal with the data, several apparent periodicities, such as 7-8a, 11-15a, 20-23a and ca 50a, are revealed, among which some can be attributed to the solar forcing. Based on results of Cluster Analysis of dry-wet changes, we resume the regional differentiation pattern of flood-drought disasters all over Guangdong during different climatic intervals in the LIA and, find the western and northern parts of Guangdong have undergone drastic changes in drought-flood regional differentiation, but the eastern part is relatively stable, and the area of the Pearl River Delta shows stable condition of more flood disasters.
机译:基于1480-1940AD期间干旱和洪水灾害的历史记录,重建了湿润指数(WI)和干旱和洪水灾害的序列。我们在格陵兰术后序列波动与GISP2冰芯的波动之间找到了良好的相同关系,这表明了一种含水量和温度的表观季风处理模式。通过应用Morlet小波变换方法来处理数据,揭示了几种表观周期,例如7-8A,11-15A,20-23A和CA 50A,其中一些可以归因于太阳迫使。根据干湿变化的集群分析结果,在利亚的不同气候间隔期间恢复广东各地的洪水干旱灾害的区域分化模式,发现广东西部和北部都经历了干旱的大剧变化 - 洪水区别化,但东部相对稳定,珠江三角洲的地区显示出更多的洪水灾害状况。

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