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
纸质出版:2015
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赵景波, 周岳, 李如意, 等. 鄂尔多斯高原西部清代洪涝灾害与气候事件特征[J]. 水土保持通报, 2015,35(1):344-348.
ZHAO Jingbo, ZHOU Yue, LI Ruyi, et al. Characteristics of Flood Disaster and Climate Events in Western Ordos Plateau in Qing Dynasty[J]. Bulletin of Soiland Water Conservation, 2015, 35(1): 344-348.
赵景波, 周岳, 李如意, 等. 鄂尔多斯高原西部清代洪涝灾害与气候事件特征[J]. 水土保持通报, 2015,35(1):344-348. DOI: 10.13961/j.cnki.stbctb.2015.01.062.
ZHAO Jingbo, ZHOU Yue, LI Ruyi, et al. Characteristics of Flood Disaster and Climate Events in Western Ordos Plateau in Qing Dynasty[J]. Bulletin of Soiland Water Conservation, 2015, 35(1): 344-348. DOI: 10.13961/j.cnki.stbctb.2015.01.062.
[目的] 揭示鄂尔多斯高原西部清代洪涝灾害发生规律和等级。[方法] 根据历史文献统计分析
并应用小波分析等方法开展研究。[结果] 鄂尔多斯高原西部清代发生洪涝灾害89次
平均每3 a发生1次。鄂尔多斯高原西部清代洪涝灾害可分为5个阶段
第1阶段在1644-1733年
第2阶段在1734-1783年
第3阶段在1784-1813年
第4阶段在1814-1863年
第5阶段在1864-1912年。第1
3
5阶段是洪涝灾害低发阶段
第2
4阶段是高发阶段。在该区清代发生洪涝灾害89次中
轻度灾害占24.7%
中度灾害占65.2%
重度灾害占10.1%。[结论] 该区清代水涝灾害变化主要有65
32
17
10和3~4 a的周期。该区清代洪涝灾害的发生主要是年降水增加和年内降水集中造成的。鄂尔多斯高原西部清代出现了2次湿润气候事件
分别出现在1774-1783和1814-1823年。
[Objective] To reveal the rules and grade of west Ordos plateau flood disasters in Qing dynasty.[Methods] The method of historical literature analysis and wavelet analysis method were used to research relevant problem.[Results] The study concluded that the western Ordos Plateau flood disasters during the Qing Dynasty happened 89 times and occurred averagely 0.34 times per year. Flood disasters in the western Ordos Plateau during Qing Dynasty could be divided into 5 stages
from 1644 to 1733 was the Ⅰ stage
from 1734 to 1783 was the Ⅱ stage
from 1784 to 1813 was the Ⅲ stage
from 1814 to 1863 was the Ⅳ stage
and from 1864 to 1912 was the Ⅴ stage. The Ⅰ
Ⅲ and Ⅴ stage belonged to low stage
the Ⅱ and Ⅳ stage belonged to high stage. In the area during Qing Dynasty
89 times flood disaster occurred
and the mild disasters accounted for 24.7%
moderate disasters accounted for 65.2%
severe disasters accounted for 10.1%.[Conclusion] The cycles of flooding disaster occurrences during Qing Dynasty of the Western Ordos Plateau is 65 a
32 a
17 a
10 a and 3 a to 4 a
respectively. The occurrence of floods in this area is mainly due to the increasing annual precipitation and the concentration of annual precipitation. There are 2 humid climate events appeared in the Western Ordos Plateau during the Qing Dynasty
from 1774 to1783 and from 1814 to 1823.
《陕西历史自然灾害简要纪实》编委会.陕西历史自然灾害简要纪实[M].北京:气象出版社,2002.
赵景波,周晓红,顾静.西安草滩渭河古河漫滩沉积与洪水变化[J].水土保持学报,2008,22(3):36-42.
赵景波,王娜,龙腾文.唐代泾河流域洪涝灾害研究[J].海洋地质与第四纪地质,2008,28(3):109-113.
刘会玉,林振山,张明阳.建国以来中国洪涝灾害成灾面积变化的小波分析[J].地理科学,2005,25(1):43-48.
张德二.中国三千年气象记录总集[M].南京:江苏教育出版社,2004.
袁祖亮.中国灾害通史:清代卷[M].郑州:郑州大学出版社,2009.
史念海.黄河流域诸河流的演变与治理[M].西安:陕西人民出版社,1999:315-320.
甘枝茂,桑广书,甘瑞.晚全新世渭河西安段河道变迁与土壤侵蚀[J].水土保持学报,2002,16(2):129-132.
訾冬梅. 内蒙古自治区地图册[M].北京:中国地图出版社,2002.
侯甬坚.鄂尔多斯高原及其邻区历史地理研究[M].西安:三秦出版社, 2008.
袁林.西北灾荒史[M].兰州:甘肃人民出版社,1994.
翟佑安.中国气象灾害大典:陕西卷[M].北京:气象出版社,2005.
沈建国.中国气象灾害大典:内蒙古卷[M].北京:气象出版社,2008.
夏普明.中国气象灾害大典:宁夏卷[M].北京:气象出版社,2007.
榆林市编纂委员会.榆林市志[M].西安:三秦出版社,1996.
崔锦泰.小波分析导论[M].程正兴,译.西安:西安交通大学出版社,1995.
中央气象局气象科学研究院.中国近500年旱涝分布图集[M].北京:地图出版社,1981:321-332.
刘晓清,赵景波,于学峰.清代泾河中游地区洪涝灾害研究[J].地理科学,2007,27(3):445-448.
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