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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第31卷

期数:

2009年第02期

页码:

207-211

栏目:

环境地学

出版日期:

2009-06-15

文章信息/Info

Title:

Research on the Flood Distaste of Southern Shaanxi in Ming Dynasty

文章编号:

1672-6561(2009)02-0207-05

作者:

赵景波¹; 2; 马 莉¹; 3

(1.陕西师范大学 旅游与环境学院,陕西 西安 710062; 2.中国科学院地球环境研究所 黄土与第四纪地质 国家重点实验室,陕西 西安 710075; 3.宝鸡文理学院 地理科学与环境工程系,陕西 宝鸡 721007)

Author(s):

ZHAO Jing-bo¹; 2;  MA Li¹; 3

(1.School of Tourism and Environment Science, Shaanxi Normal University, Xi'an 710062, Shaanxi, China; 2. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, Shaanxi, China; 3.Department of Geographical Science and Environment Engineering,Baoji University of Arts and Sciences, Baoji 721007, Shaanxi, China)

关键词:

明代; 陕南地区; 灾害等级; 洪涝灾害

Keywords:

Ming Dynasty;  southern Shaanxi;  disaster grade;  flood disaster

分类号:

P331.1

DOI:

-

文献标志码:

A

摘要:

通过对历史文献资料的搜集和整理,对明代自公元1369年到1644年的276年间陕南地区洪涝灾害变化阶段、趋势、等级分布和成因进行了研究。统计分析结果显示,明代陕南地区洪涝灾害可划分轻度涝灾、中度涝灾、大涝灾、特大涝灾4级灾害,各占洪灾总次数的33%、40%、21%、6%。明代陕南地区洪涝灾害共发生76次,平均每3.6年发生1次。从明代早期到晚期,洪水发生总体上呈波动上升趋势。明代陕南洪灾可分为3个阶段,第1阶段在1369～1435年之间,为洪灾贫发阶段;第2阶段在1436～1550年之间,为洪灾多发阶段;第3阶段在1551～1644年之间,为洪灾较少阶段。洪灾集中于夏、秋两季。明代陕南地区洪涝灾害的发生主要是由地形、降水和气候异常波动以及人为活动综合因素影响的结果。

Abstract:

Through the collection and analysis to the historical materials, the characteristic and the reason of the interannual and the season has been researched. The results show that, Ming Dynasty flood disaster level may divide into small, middle, big and super-big in southern Shaanxi. Their occurrence probability is 33%, 40%, 21% and 6%. From 1369 to 1644, flood disaster of the Ming Dynasty altogether has 76 times, and averagely occurred one time per 3.6 year. From the early Ming Dynasty to the late, floods occurred on the whole showed an upward trend fluctuation. The disaster has been divided into three periods. During the first period, from the 1369 to 1435, there were few disasters. During the second period, from 1436 to 1550, this region had the most disaster. During the third period, between 1551 and 1644, there were fewer disasters. On season, the disaster occurrence frequency concentrates on summer and autumn. Main factors producing flood disaster are geography, precipitation, climatic anomaly undulation and the synthetically action of artificial flexible affection.

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相似文献/References:

[1]赵景波,张冲.延安地区明代干旱灾害与气候变化研究[J].地球科学与环境学报,2010,32(04):430.
　ZHAO Jing-bo,ZHANG Chong.Drought Disaster and Climatic Change During Ming Dynasty in Yan'an Area[J].Journal of Earth Sciences and Environment,2010,32(02):430.

备注/Memo

备注/Memo:

收稿日期:2008-10-20
基金项目: 教育部人文社科研究基地重大研究项目(05JJD770014); 国家自然科学基金项目(40571004); 中国科学院黄土与第四纪地质国家重点实验室项目(SKLLQG0605)
作者简介: 赵景波(1953-),男,山东滕州人,理学博士,教授,博士研究生导师,从事第四纪与自然地理研究。E-mail:zhaojb@snnu.edu.cn

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更新日期/Last Update: 2009-06-20