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Variation of extreme drought and flood in North China revealed by document-based seasonal precipitation reconstruction for the past 300 years

机译:基于文档的近300年季节性降水重建揭示了华北地区极端干旱和洪水的变化

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Using a 17-site seasonal precipitation reconstruction from a unique historical archive, Yu-Xue-Fen-Cun, the decadal variations of extreme droughts and floods (i.e., the event with occurrence probability of less than 10 % from 1951 to 2000) in North China were investigated, by considering both the probabilities of droughts/floods occurrence in each site and spatial coverage (i.e., percentage of sites). Then, the possible linkages of extreme droughts and floods with ENSO (i.e., El Ni?o and La?Ni?a) episodes and large volcanic eruptions were discussed. The results show that there were 29 extreme droughts and 28 extreme floods in North China from 1736 to 2000. For most of these extreme drought (flood) events, precipitation decreased (increased) evidently at most of the sites for the four seasons, especially for summer and autumn. But in drought years of 1902 and 1981, precipitation only decreased in summer slightly, while it decreased evidently in the other three seasons. Similarly, the precipitation anomalies for different seasons at different sites also existed in several extreme flood years, such as 1794, 1823, 1867, 1872 and 1961. Extreme droughts occurred more frequently (2 or more events) during the 1770s–1780s, 1870s, 1900s–1930s and 1980s–1990s, among which the most frequent (3 events) occurred in the 1900s and the 1920s. More frequent extreme floods occurred in the 1770s, 1790s, 1820s, 1880s, 1910s and 1950s–1960s, among which the most frequent (4?events) occurred in the 1790s and 1880s. For the total of extreme droughts and floods, they were more frequent in the 1770s, 1790s, 1870s–1880s, 1900s–1930s and 1960s, and the highest frequency (5?events) occurred in the 1790s. A higher probability of extreme drought was found when El Ni?o occurred in the current year or the previous year. However, no significant connections were found between the occurrences of extreme floods and ENSO episodes, or the occurrences of extreme droughts/floods and large volcanic eruptions.
机译:利用来自独特的历史档案Yu-Xue-Fen-Cun的17个站点的季节性降水重建,得出北部地区极端干旱和洪水的年代际变化(即从1951年到2000年发生概率小于10%的事件)对中国进行了调查,同时考虑了每个站点发生干旱/洪灾的可能性和空间覆盖率(即站点的百分比)。然后,讨论了极端干旱和洪水与ENSO(即El Ni?o和La?Ni?a)事件和大型火山喷发的可能联系。结果表明,从1736年到2000年,华北地区发生了29次极端干旱和28次极端洪水。对于大多数极端干旱(洪水)事件,在四个季节的大部分时间里,降水量明显减少(增加),尤其是夏天和秋天。但是在1902年和1981年的干旱年份,降水仅在夏季略有减少,而在其他三个季节则明显减少。同样,在几个极端洪水年份(例如1794、1823、1867、1872和1961),也存在不同地点不同季节的降水异常。在1770年代至1780年代,1870年代, 1900年代至1930年代和1980年代至1990年代,其中最频繁的事件(3个事件)发生在1900年代和1920年代。在1770年代,1790年代,1820年代,1880年代,1910年代和1950年代至1960年代发生了更为频繁的极端洪水,其中最频繁的(4个事件)发生在1790年代和1880年代。在极端干旱和洪水的总数中,它们在1770年代,1790年代,1870年代至1880年代,1900年代至1930年代和1960年代更为频繁,最高频率(5个事件)发生在1790年代。当本年度或上一年度发生厄尔尼诺现象时,发现极端干旱的可能性更高。但是,在极端洪水的发生和ENSO事件之间,或极端干旱/洪水和大火山喷发之间都没有发现明显的联系。

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