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Spatial-temporal variations of natural disasters during the Ming & Qing Dynasties (1368-1912AD) in Chaohu Lake Basin, East China

机译:中国东部巢湖流域的明清(1368-1912AD)自然灾害的时空变化

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The Ming & Qing Dynasties experienced the Little Ice Age (LIA), a most abnormal climate event in nearly 2000 years' of Chinese history, in which various natural disasters took place frequently. On the basis of systematically collecting and collating historical documents related to natural disasters, and by adopting mathematical statistics, geological succession, correlation and other methods, analysis and comparison were made on the spatial-temporal differentiation of disasters and correlation between various major natural disasters taking place in the Chaohu Lake Basin during the Ming & Qing Dynasties (1368-1912AD). The results show that 753 major disasters took place in the Chaohu Lake Basin during the Ming & Qing Dynasties. Among these, floods and droughts accounted for the largest percentage, while other disasters occurred occasionally. The Little Ice Age (1550-1850AD) was the period with a high incidence of natural disasters, and in the years from 1701 to 1750 natural disasters took place most frequently; between 1651-1700AD there was a declining period of flood frequency, though there were historically high occurrences of droughts and earthquakes. There were more floods than droughts suffered by Hefei, Shucheng, Chaohu, Wuwei and Hexian, while more droughts than floods suffered by Hanshan and Lujiang. Earthquakes in the basin mainly occurred in Chaohu, Shucheng, Hexian and Hefei, which are all near the Tan-Lu Fracture. The opposite is true for changes in the time scale of floods and droughts; this was probably caused by intra-seasonal oscillations of the subtropical high. The correlation between hails and wind disasters is significant, while other disasters are weakly correlated. There exists a certain association between spatial differentiation of occurrence frequency of natural disasters and landforms in the basin. The disaster-prone environment features landforms including plains, hills, low mountains, and these have a significant impact on the spatial distribution of five major natural disasters in the Chaohu Lake Basin. (C) 2018 Elsevier Ltd and INQUA. All rights reserved.
机译:明清时期经历了小冰期(LIA),这是中国近2000年以来最异常的气候事件,其间频繁发生各种自然灾害。在系统整理和整理与自然灾害有关的历史文献的基础上,采用数理统计,地质演替,关联等方法,对灾害的时空分异和各种重大自然灾害之间的相关性进行分析比较。在明清(1368-1912AD)时期位于巢湖流域。结果表明,明清时期巢湖流域发生了753起重大灾害。其中,洪水和干旱占最大比例,而其他灾害偶发。小冰河时期(1550-1850AD)是自然灾害的高发时期,在1701至1750年的自然灾害中发生得最为频繁。在1651-1700年之间,洪水频率呈下降趋势,尽管历史上干旱和地震的发生率很高。合肥,蜀城,巢湖,无为和合县遭受的洪灾多于旱灾,而韩山和庐江遭受的旱灾多于旱灾。流域的地震主要发生在-庐断裂附近的巢湖,蜀城,合县和合肥。洪水和干旱时间尺度的变化则相反。这可能是由于副热带高压的季节内振荡引起的。冰雹与风灾之间的相关性很重要,而其他灾害之间的相关性很弱。流域自然灾害发生频率的空间分异与地貌之间存在一定的联系。灾害多发的环境具有平原,丘陵,低山等地貌,对巢湖流域五种重大自然灾害的空间分布具有重大影响。 (C)2018爱思唯尔有限公司和INQUA。版权所有。

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