首页|中国先秦-清代重大旱灾的时空分布格局与变迁过程

中国先秦-清代重大旱灾的时空分布格局与变迁过程

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从历史文献和史料记载中提取从先秦至清代(850aB.C.-1911年)有详尽灾害描述的重大旱灾记录,以县域为最小研究单元构建重大旱灾频次和累计等级的时间序列并进行空间分布可视化.利用熵权法确定重大旱灾综合指数,结合空间自相关、重心分析法和标准差椭圆研究中国历史时期重大旱灾分布格局及变化过程.结果表明:① 从先秦至清代(850aB.C.-1911年)中国重大旱灾共发生580 a,平均每4.76年发生1次,总体呈现上升趋势.② 整体上,重大旱灾的发生频次北方高于南方,旱灾频次最高的地区是陕西、河南和山东的一些县域.③明代为重大旱灾累计等级最高时期,全国近56.81%的地区都有发生重大旱灾.重大旱灾累计等级具有显著的空间自相关性,其相关性变化经历了"增-减-增-减"的过程,全期莫兰指数为0.43,具有显著空间集聚性.④重大旱灾分布县数共占总发生旱灾县数的21.42%,不同时间段上,重灾区在陕西、河南、山西、河北、山东间变化.其重心始终位于河南省境内,在河南省内部,沿"西南-东北-西南-东南-西北"方向移动.⑤重大旱灾频次与气温、降水呈现显著负相关.中国西高东低的地势条件、温带大陆性季风气候和人类不合理活动与华北及其周边地区成为重灾区有一定的关联.此外,气候变化与人口分布对历史时期重大旱灾分布格局变动具有重要的影响.
Spatial and temporal distribution pattern and changing process of major drought in Pre-Qin and Qing Dynasties of China
The major drought records with detailed disaster descriptions from Pre-Qin Dynasty to Qing Dynasty(850 a B.C.-1911 a A.D.)are extracted from historical documents and historical material records.The entropy weight method was used to determine the comprehensive index of major drought,and the spatial autocorrelation,barycentric analysis and standard deviation ellipse were used to study the distribution pattern and change process of major drought in historical period of China.The results show that:1)From Pre-Qin Dynasty to Qing Dynasty,the frequency of major drought in China was 580 times,with an average of once every 4.76 years,showing an overall upward trend.2)On the whole,the frequency of major drought in the north is higher than that in the south,and the highest frequency of drought is in some counties of Shaanxi,Henan and Shandong.3)The Ming Dynasty is the period with the highest cumulative level of major drought,and nearly 56.81%of the areas in China have experienced major drought.The cumulative grade of major drought has significant spatial autocor-relation,and its correlation changes have experienced the process of"increase-decrease-increase-decrease".The Moran index of the whole period is 0.43,which has significant spatial agglomeration.4)The number of counties with major drought accounted for 21.42%of the total number of counties with major drought.Its cen-ter of gravity is always located in Henan Province,moving in the direction of"southwest-northeast-southwest-southeast-northwest".5)The frequency of major drought was significantly negatively correlated with temperat-ure and precipitation.The terrain conditions of high in the west and low in the east of China,temperate contin-ental monsoon climate and unreasonable human activities are related to North China and its surrounding areas becoming the hardest hit-areas.In addition,climate change and population distribution have an important im-pact on the changes in the distribution pattern of major droughts in historical periods.

major droughtseverely affected areasfocus migrationShenyang-Lanzhou-Xishuangbanna Arc

郭艺澍、殷淑燕、车录胜

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陕西师范大学地理科学与旅游学院,陕西西安 710119

重大旱灾 重灾区 重心迁移 沈兰西弧线

教育部人文社会科学研究规划基金项目

18YJA770021

2024

地理科学
中国科学院 东北地理与农业生态研究所

地理科学

CSTPCDCSSCICHSSCD北大核心
影响因子:3.117
ISSN:1000-0690
年,卷(期):2024.44(8)
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