[1]侯雨乐,赵景波*,胡 尧.清代时期都江堰地区洪涝灾害与气候特征研究[J].山地学报,2017,(06):865-873.[doi:10.16089/j.cnki.1008-2786.000288]
 HOU Yule,ZHAO Jingbo*,HU Yao.Flood Disasters Events and Associated Climate in Dujiangyan City during Qing Dynasty[J].Mountain Research,2017,(06):865-873.[doi:10.16089/j.cnki.1008-2786.000288]
点击复制

清代时期都江堰地区洪涝灾害与气候特征研究()
分享到:

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2017年06期
页码:
865-873
栏目:
山地灾害
出版日期:
2017-11-30

文章信息/Info

Title:
Flood Disasters Events and Associated Climate in Dujiangyan City during Qing Dynasty
文章编号:
1008-2786-(2017)6-865-09
作者:
侯雨乐1 赵景波2*胡 尧1
1.阿坝师范学院, 四川 汶川 623002; 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 710061
Author(s):
HOU Yule1 ZHAO Jingbo2*HU Yao1
1.Aba Teachers College, Wenchuan, Sichuan 623002, China; 2.Institute of Earth Environment, Chinese Academy of Sciences, State Key Laboratory of Loess and Quaternary Geology, Xi'an 710061, China
关键词:
洪涝灾害 周期性 降水增多事件 清代 都江堰市
Keywords:
Flood disaster Periodicity Increased precipitation events Qing Dynasty Dujiangyan City
分类号:
P426.616
DOI:
10.16089/j.cnki.1008-2786.000288
文献标志码:
A
摘要:
分析历史时期洪涝灾害对揭示古气候环境有重要科学价值。本研究通过对都江堰地区历史资料的整理分析,运用数理统计和小波分析等研究方法,探讨了该地区清代洪涝灾害的等级、频次、周期以及历史气候特征。结果表明,在清代268年中共发生洪灾62次,平均每4.3年发生一次,从清代早期到晚期洪灾呈现波动增加趋势且有明显的阶段性:1644—1679年和1790—1839年是洪灾少发期,1680—1789年和1840—1911年是洪灾高发期。小波分析结果显示清代都江堰地区的洪灾明显地存在4 a左右短期振荡周期、23 a左右的长期振荡周期,清中晚期还存在一个约8 a的中振荡周期。清代该地区出现了6次降水增多事件,分别发生于1744—1746年、1863—1868年、1873—1875年、1878—1881年、1897—1902年和1906—1908年,集中于清代中后期。厄尔尼诺事件也是诱发本地区洪灾发生的一大因子。推断本地区发生特大洪灾和大洪灾年份的降水量显著增多,年降水量约1510 mm或更多。
Abstract:
By examining historical data of Dujiangyan region, this research conducted statistical analysis and wavelet transform to retrieve the ancient flood information in Qing Dynasty, including the grading, frequency and periodicity of flooding as well as climate pattern.Results showed that flooding occurrences amounted to 62 for the whole 268 years of the Qing dynasty, once every 4.3 years, and from early Qing dynasty to the late, flooding occurred with a fluctuated increase trend and obvious periodic pattern: a period of less flooding during 1644-1679 and 1790-1839, and at high risk of flooding for 1680-1789 and 1840-1911.Flooding in Dujiangyan region in Qing dynasty obviously existed a short period of 4a and long-term oscillated period of 23a.Besides, there was an 8a in the middle and late Qing dynasty.There were 6 incremental precipitation period in the region during Qing dynasty, occurred in 1744-1746, 1863-1868, 1873-1875, 1878-1881, 1897-1902 and 1906-1908 years, respectively, concentrated in the middle and late Qing dynasty.El Nino event was also a major factor inducing flood disasters.It referred to a significant increment of rainfall in the year of catastrophic flood and great flood, with an estimation of precipitation about 1510 mm or more.

参考文献/References:

[1] 秦嘉励,杨万勤,张健.岷江上游典型生态系统水源涵养量及价值评估[J].应用与环境生物学报,2009,15(4): 453-458.[QIN Jiali, YANG Wanqin, ZHANG Jian.Assessment of Ecosystem Water Conservation Value in the Upper Minjiang Rive[J].Journal of Applied and Environmental Biology,2009,15(4 ): 453-458.]
[2] 杨斌,詹金凤,李茂娇.岷江上游流域环境脆弱性评价[J].国土资源遥感,2014,26(4):138-144.[YANG B,ZHAN JF,LI M J.Evaluation of environmental vulnerability in the upper reaches of the Minjiang River[J].Remote Sensing for Land and Re-sources,2014,26(4):138-144.]
[3] 张继飞,邓伟,朱昌丽,等.岷江上游生态系统服务与居民福祉的空间关联及其动态特征[J].山地学报, 2017,35(3): 388-398.[ZHANG Jifei, DENG Wei, ZHU Changli, et al.Spatial Relationship and Its Dynamic Features of Ecosystem Services and Human Wellbeing in the Upper Reaches of Minjiang River[J].Mountain Research, 2017, 35(3): 388-398.]
[4] 张萍.明清时期岷江流域水旱灾害初步研究[D].重庆:西南大学,2014:16-31.[ZHANG Ping.Preliminary study of drought during the Ming and Qing Dynasties on Minjiang River Basin[D].Chongqing: Southwestern University, 2014:16-31.]
[5] 刘兴亮,苏春江,徐 云.岷江上游水资源问题及可持续利用[J].水土保持研究,2006,13(3)189-192.[ LIU Xingliang, SU Chunjiang, XU Yun.Water Resource Problem and Sustainable Utilization in the Upper Reaches of Minjiang Rive[J] Research of Soil and Water Conservation.2006,13(3)189-192.]
[6] 邓绍辉.建国以来四川洪涝灾害的特点及对策[J].四川师范大学学报(社会科学版),2001,28(5):96-104.[DENG Shaohui.Flood Features in Sichuan Since 1949 and Measures[J].Journal of Sichuan Normal University(Social Sciences Edition).2001,28(5):96-104.]
[7] 李 喆,何政伟.地震前后都江堰市土地利用动态变化研究[J].四川师范大学学报(自然科版),2012,35(3):412-416.[ LI Zhe, HE Zhengwei, XU Hui-xi.The Research of Land Use Dynamic Change before and after the Earthquake in Dujiangyan City[J].Journal of Sichuan Normal University(Natural Science),2012,35(3):412-416.]
[8] 中央气象局气象科学研究院.中国近五百年旱涝分布图集[M].北京:新华书店,1981:10-39.[Central Meteorological Bureau.Atlas of flood and drought distribution nearly five hundred years in China.[M].Beijing: Xinhua Bookstore,1981:10-39.]
[9] 冯广宏.岷江志[M].成都:四川省水利电力厅,1990:125-146.[FENG Guanghong.Minjiangzhi[M]:Chengdu: Sichuan Provincial Water Conservancy and electric power department,1990:125-146.]
[10] 水利电力部水管司科技司.清代长江流域西南国际河流洪涝档案史料[M].北京:中华书局,1991:30-126.[Department of water resources division.Records of flood records of international rivers in Southwest China during the Qing Dynasty[M].Beijing: Zhong Hua Book Company,1991:30-126.]
[11] 詹兆渝.中国气象灾害大典·四川卷[M].北京:气象出版社,2006:8-35.[Zhan zhaoyu.Meteorological disasters.Chinese-Sichuan roll ceremony[M]Beijing: Meteorological Press,2006: 8-35.]
[12] 苏慧慧,查小春.清代时期汾河中游地区洪涝灾害研究[J].干旱区资源与环境,2010,24(1):90-94.[SU Huihui, ZHA Xiaochun.Study on flood disasters reaches in the middle of Fenhe river during Qing Dynasty[J].Journal of Arid Land Resources and Environment,2010,24(1):90-94.]
[13] 韩庆玉.四川洪灾及其特性浅析[J].四川水利,1996,17(3):18-22.[HAN Qingyu.Flood disaster and its characteristics in Sichuan[J].Sichuan Water Resources, 1996,17(3):18-22.]
[14] 孙金岭,何元庆,何则,等.基于Morlet小波的清代民国河西走廊洪涝灾害与气候变化研究[J].干旱区资源与环境,2016,30(1):60-65.[ SUN Jinling, HE Yuanqing, HE Ze, et al.Study on the flood disasters and climate changes in the Hexi Corridor during Qing dynasty and the Republic of China[J].Journal of Arid Land Resources and Environment, 2016, 30(1):60-65.]
[15] 王兴梅,张 勃,王海军,等.石羊河流域近50年最高最低气温变化分析[J].干旱区地理,2010,33(6):880-889.[WANG Xingmei, ZHANG Bo, WANG Hajun, et al.Maximum and minimum temperature changes in Shiyang River Basin in the last 50 years[J].Rid Land Geography, 2010,33(6):880-889.]
[16] 张 强,姜 彤,吴宜进.ENSO事件对长江上游1470-2003年旱涝灾害影响分析[J].冰川冻土,2004,26(6):691-697.[ZHANG Qiang, JIANG Tong, WU Yijin.Impact of ENSO Events on Flood/Drought Disasters of Upper Yangtze River during 1470-2003[J].Journal of Glaciology and Geocryology, 2004, 26(6):691-697.]
[17] 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,2015,31(1):344-348.[ZHAO jingbo, ZHOU yue, LI ruyi, et al.Characteristics of Flood Disaster and Climate Events In Western Ordos Plateau in Qing Dynatsy[J].Bulletin of soil and Water Conservation,2015,31(1):344-348.]
[18] 葛全胜,刘路路,郑景云,等.过去千年太阳活动异常期的中国东部旱涝格局[J].地理学报,2016,71(5):707-717.[GE Quansheng, LIU Lulu, ZHENG Jingyun, et al.Spatial patterns of drought/flood over eastern China in the periods of anomalous solar activity during the past millennium[J].Acta Geographical Sinica, 2016,71(5):707-717.]
[19] 汶林科,崔鹏,杨红娟,等.ENSO与长江流域中游地区雨季极端降水的关系[J].山地学报,2011,29(3):299-305.[WEN Linke, CUI Peng, YANG Hongjuan, et al.The Relationship between ENSO and the Precipitation Extremes along the Middle Reachesof Yangtze River during the Monsoon Season[J].Mountain Research,2011,29(3):299-305.]
[20] 殷淑燕,王海燕,黄春长,等.陕南汉江上游历史洪水灾害与气候变化[J].干旱区研究,2010,27(4):522-528.[YIN Shuyan, WANG Haiyan, HUANG Chunchang, et al.Study on historical flood disasters and climate change in the upper reaches of the Hanjiang River[J],2010,27(4):522-528.]
[21] 勾晓华,杨 涛,高琳琳,等.树轮记录的青藏高原东南部过去457年降水变化历史[J].科学通报,2013, 58(11): 978-985.[GOU X H, YANG T, GAO L L, et al.A 457-year reconstruction of precipitation in the southeastern Qinghai-Tibet Plateau[J].Chinese Science Bulletin, 2013, 58(11): 978-985.]
[22] 李昕翼,肖国杰,白爱娟,等.成都地区降水时空分布变化[J].气象科技, 2011,39(4): 417-422.[ Li Xinyi, Xiao Guojie, Bai Aijuan, et al.Temporal-spatial distribution of precipitation in Chengdu[J], 2011,39(4): 417-422.]
[23] 李栋梁,姚 辉.1470-1997年中国旱涝与厄尼诺事件[J].干早区地理,1991,14(2):48-52.[LI Dongliang, YAO Hui.Chinese drought \ flood disasters and El Nino events during 1470-1997[J].Arid area of Geography, 1991,14(2):48-52.]
[24] 张冲,赵景波.厄尔尼诺/拉尼娜事件对长江流域气候的影响研究[J].水土保持通报,2011,31(3):1-8.[ZHANG Chong, ZHAO Jingbo.Effects of El Nino-Southern Oscillation Events on Climate in Yangtze River Basin[J].Bulletin of Soil and Water Conservation, 2011,31(3):1-8.]
[25] 王钦,李双林,付建建.1998和2010年夏季降水异常成因的对比分析:兼论两类不同厄尔尼诺事件的影响[J],气象学报,2012,70(6):1207-1222.[WANG Qin, LI shuanglin, FU Jianjian.On the formation of anomalous summer precipitation in the years of 2010 and 1998: A comparisons of the EI Nino cases's impact between modoki and typical EI Nino cases.Acta meteorological sinaica, 2012,70(6):1207-1222.]
[26] 王绍武.近500年的厄尔尼诺事件[J].气象,1989,15(4):15-21.[WANG Shaowu.El Nino events in recent 500 years[J].Meteorology, 1989,15(4):15-21.]
[27] 竺可桢.中国五千年来气候变迁的初步研究[J].中国科学,1973,16(2):226-230.[ZHU Kezhen.A preliminary study on climate change in China for five thousand years[J].Chinese science,1973,16(2):226- 230.]
[28] 徐蕊.明清时期中国大陆的气候变化[J].首都师范大学学报(自然科学版),2009,30(6):67-71.[Xu Rui.The Climate of Chinese Continent Change in Ming and Qing Dynasty[J].Journal of Capital Normal University(Natural Science Edition), 2009,30(6):67-71.]
[29] 黄忠恕.长江流域历史水旱灾害分析[J].人民长江,2003,34(2):1-3.[ HUANG Zhongshu.The analysis of historical flood and drought disasters in the Yangtze River Basin[J].Yangtze River,2003,34(2):1-3.]
[30] 靳俊芳,殷淑燕,王学佳.汉江上游北宋时期洪水事件的沉积记录和文献记录对比[J]山地学报,2016,34(3):266-273.[JIN Junfang, YIN Shuyan, WANG Xuejia.Comparison of Extraordinary Flood Events Reflected Selected by Sediments with Historical Documents in the Upper Reaches of the Hanjiang River during the Chinese Northern Song Dynasty(950—1050 A.D.[J], Mountain Research,2016,34(3):266-273.]
[31] 姚辉,李栋梁.厄尔尼诺事件与中国降水及历史旱涝[J].应用气象学报,1992,3(2):228-235.[YAO Hui, LI Dongliang.The Relationship between EI Nino Events and the Rainfall, Historical Drought and Water Logging in China[J].Journal of Applied Meteorological Science,1992,3(2):228-235.]
[32] 袁媛,李崇银,杨崧.与厄尔尼诺和拉尼娜相联系的中国南方冬季降水的年代际异常特征[J].气象学报,2014,72(2):237-255.[YUAN Yuan, LI Chongyin, YANG Song.Decadal Anomalies of Winter Precipitation over Southern China in association with EI Nino and LA Nina[J] Acta Meteorological Sinica,2014,72(2):237-255.]
[33] 王伟,冯爽.西南地区夏季旱涝与厄尔尼诺(拉尼娜)的关系分析[J].成都信息工程学院学报,2012,27(4):412-416.[WANG Wei, FENG Shuang.The Correlation Analysis between Summer Droughts & Floods in the Southwest and ENSO[J].Journal of Chengdu University of Information Technology, 2012,27(4):412-416.]
[34] 丁文荣.西南地区极端降水的时空变化特征[J].长江流域资源与环境,2014,23(7):1071-1079.[DING Wenrong.Spatial and Temporal Variability of the Extreme Daily Precipitation in Southwest China[J].Resources and Environment in the Yangtze Basin, 2014,23(7):1071-1079.]

相似文献/References:

[1]李文田.信阳市洪涝灾害基本特征与防治对策[J].山地学报,2014,(01):105.
 LI Wentian.Basic Characteristics and Countermeasures of Flood Disaster in Xinyang City of Henan,China[J].Mountain Research,2014,(06):105.
[2]张娜,林丽梅,俞鸣同,等.福州大学城洪涝灾害成因[J].山地学报,2015,(03):379.
 ZHANG Na,LIN Limei,YU Mingtong,et al.Flood Disaster Cause of Fuzhou University Area[J].Mountain Research,2015,(06):379.
[3]高若允,杨柳生,罗清虎,等.洪涝灾害致损森林在自然恢复过程中的土壤种子库变化[J].山地学报,2022,(2):183.[doi:10.16089/j.cnki.1008-2786.000664]
 GAO Ruoyun,YANG Liusheng,LUO Qinghu,et al.Variation of Soil Seed Bank in Natural Restoration Processes of Different Types of Forests Disturbed by Floods[J].Mountain Research,2022,(06):183.[doi:10.16089/j.cnki.1008-2786.000664]

备注/Memo

备注/Memo:
收稿日期(Received date):2016-12-20; 改回日期(Accepted date):2017-09-06
基金项目(Foundation item):阿坝师范学院校级科研项目岷江上游旱涝灾害研究(ASB15-13)项目; 四川省教育厅项目岷江上游旱涝灾害原因及治理探析(16ZB0386); 黄土与第四纪地质国家重点实验室项目(SKLLQG1428)[Drought and Flood Disasters of the Upper Reaches of Minjiang River from Project in Aba Teachers College Scientific Research.(ASB15-13); Drought and Flood Disasters of the Upper Reaches of Minjiang River from Project in Sichuan Province Department of Education.(16ZB0386); Project in State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences,(SKLLQG1428)]
作者简介(Biography):侯雨乐(1983-),男,山西交城人,讲师,硕士,研究方向:区域自然地理。E-mail:512570915@qq.com [Hou Yule(1983-),male, born in Jiaocheng, Shanxi Province, Lecturer, master degree, research on regional physical geography.E-mail:512570915@qq.com]
*通信作者(Corresponding author):赵景波(1953-),男,山东滕州人,教授,博士生导师,研究方向:区域环境研究。E-mail:zhaojb@snnu.edu.cn[Zhao Jingbo(1953-),male, born in Tengzhou Shandong Province, Professor, doctoral supervisor, research on regional environment.E-mail:zhaojb@snnu.edu.cn]
更新日期/Last Update: 2017-11-30