院报 ›› 2022, Vol. 39 ›› Issue (11): 73-81.DOI: 10.11988/ckyyb.202107132022

• 水灾害 • 上一篇    下一篇

公元前887年—公元1911年长江流域水、疫灾害时空分布特征

胡兴涛1,2, 杨广斌1,2, 石秀雄1,2, 崔瀚文1,2, 李蔓1,2   

  1. 1.贵州师范大学 地理与环境科学学院,贵阳 550025;
    2.贵州省山地资源与环境遥感应用重点实验室,贵阳 550025
  • 收稿日期:2021-07-14 修回日期:2021-09-24 出版日期:2022-11-01 发布日期:2022-11-14
  • 通讯作者: 杨广斌(1973-),男,山东聊城人,教授,博士,主要方向为地理信息系统开发与应用。E-mail: ygbyln@163.com
  • 作者简介:胡兴涛(1995-),男,贵州织金人,硕士研究生,主要研究方向为地理信息系统与遥感。E-mail:tgdkyxx@163.com
  • 基金资助:
    国家自然科学基金委员会-贵州省人民政府喀斯特科学研究中心项目(U1812401);黔科合重大专项[2022]001

Temporal and Spatial Distribution Characteristics of Floods and Epidemics in the Yangtze River Basin from 887 BC to 1911 AD

HU Xing-tao1,2, YANG Guang-bin1,2, SHI Xiu-xiong1,2, CUI Han-wen1,2, LI Man1,2   

  1. 1. School of Geography and Environmental Sciences,Guizhou Normal University,Guiyang 550025,China;
    2. Guizhou Key Laboratory of Mountain Resources and Environment Remote Sensing,Guiyang 550025,China
  • Received:2021-07-14 Revised:2021-09-24 Online:2022-11-01 Published:2022-11-14

摘要: 水灾和疫灾均是对人类生命健康造成巨大威胁的灾害。采用空间自相关、热点分析和空间统计分析等方法,建立先秦至清代时期(公元前887年—公元1911年)水、疫灾害序列,研究了这一时期的长江流域水、疫灾害时空分布特征。研究结果表明:①长江流域水、疫灾害在先秦至清末2 798 a中至少有789个水灾年、201个疫灾年,灾害年数总体呈波动上升趋势,水、疫灾害在元朝至清末时期的发生年数为先秦至元朝时期的两倍;在10 a尺度和世纪尺度下二者具有相同的波动趋势,同时期下水灾发生频率高于疫灾。②长江流域水灾和疫灾的季节性变化为:进入防汛期的夏秋季节,是水灾的高发期,而进入冬春季节,为水灾低发期。疫灾高发期主要在春夏季节,秋冬季节属于疫灾低发时期。③从灾害广度上看,各历史时期水灾以大型灾害为主,疫灾以小微型灾害为主,不完善的救灾机制是导致灾害损失延续的重要原因。④水灾和疫灾的总体空间分布特征为受灾市域间具有较强的相互影响性;随着时代的发展,在空间格局变化上具有相似的迁移扩展趋势;同时期的水、疫灾害热点显著区也具有较高的重合度。

关键词: 水灾, 疫灾, 时空分布, 历史时期, 长江流域, 热点分析

Abstract: There are no debates on whether floods and epidemics as disasters pose a threat to human life and health.In this study we constructed a time sequence from the Pre Qin Dynasty to the Qing Dynasty (887 BC to 1911 AD) to explore the spatial-temporal distribution characteristics of floods and epidemics in the Yangtze River basin via spatial autocorrelation,hot spot analysis,and spatial statistical approaches.The results indicated that: (1) There are at least 789 flood years and 201 epidemic years in the total 2798 years from Pre Qin Dynasty to late Qing Dynasty in the Yangtze River basin.The number of disaster years shows an fluctuating upward trend,and in particular,the number of disaster years between the Yuan Dynasty and late Qing Dynasty is twice as many as that in the period from the Pre Qin Dynasty to the Yuan Dynasty.Both periods witnessed the same fluctuation trend in decadal and centurial scales,and in the same period,the frequency of flood is higher than epidemic.(2) High-incidence seasons of flood were mainly concentrated in summer and autumn,while low-incidence seasons are linked to winter and spring.Nevertheless,the high-incidence seasons of epidemics mainly coincided with spring and summer,whereas low-incidence seasons of epidemics with autumn and winter.(3) Floods in historical periods were large-scale disasters and epidemics were mainly microscale.The incomplete mechanism of disaster-relief work mainly triggered the continuation of disaster losses.(4) The disaster-affected cities interacted with each other deeply,and presented similar spatial variation trends in a time sequence.Moreover,the significant area of hot spot of floods overlaps to a large extent with that of epidemics in the same period.

Key words: flood disaster, epidemics, temporal and spatial distribution, historical periods, the Yangtze River basin, hot spot analysis

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