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Dryness-wetness change and regional differentiation of flood-drought disasters in Guangdong during 1480-1940AD

机译:1480-1940年广东省旱涝灾害的干湿变化与区域分异

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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 δ~(18)O 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, ll-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:根据1480-1940年干旱和洪水灾害的历史记录,重建了湿度指数(WI)和干旱和洪水灾害的序列。我们发现,WI序列的波动与格陵兰岛GISP2冰芯的δ〜(18)O记录之间存在良好的相同关系,这显示出明显的季风性水分和温度处置模式。通过应用Morlet小波变换方法来处理数据,揭示了一些明显的周期性,例如7-8a,11-15a,20-23a和ca 50a,其中一些可以归因于太阳强迫。根据干湿变化的聚类分析结果,我们恢复了LIA在不同气候间隔内广东全省水旱灾害的区域分异模式,发现广东西部和北部地区经历了干旱的剧烈变化。洪灾区域分异,但东部相对稳定,珠江三角洲地区呈现出更多洪涝灾害的稳定状态。

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