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[1]ZHAO Yan,YUE Dapeng,ZHAO Jingbo,et al.Flood Disasters in the Central and Southern Loess Plateau of Shaanxi in Ming Dynasty[J].Research of Soil and Water Conservation,2021,28(05):187-195.

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Flood Disasters in the Central and Southern Loess Plateau of Shaanxi in Ming Dynasty

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 28 Number of periods: 2021 05 Page number: 187-195 Column: Public date: 2021-08-20

Title:: Flood Disasters in the Central and Southern Loess Plateau of Shaanxi in Ming Dynasty

Author(s):: ZHAO Yan^1,2,YUE Dapeng¹,ZHAO Jingbo^1,2,LIU Le¹; (1.School of Geography and Tourism,Shaanxi Normal University,Xi'an 710119,China; 2.State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment,Chinese Academy of Sciences,Xi'an 710061,China)

Keywords:: flood disaster; occurrence cycle; wavelet analysis; Ming Dynasty; Loess Plateau

CLC:: P426.616

DOI:: -

Abstract:: In order to explore the regularity of floods in the Loess Plateau of Shaanxi Province,and to provide help for the climate recovery and disaster prediction and prevention in the historical period of the region,this paper collected and sorted out the historical documents of floods,and used mathematical statistics,wavelet analysis and other methods to studied the flood disaster grade,frequency,cycle and causes in the central and southern part of Shaanxi Loess Plateau in the Ming Dynasty. Through the collection of relevant historical documents of flood disasters,mathematical statistics,wavelet analysis and other methods were used to study the flood disasters grade,frequency,cycle and cause of the Ming Dynasty in the central and southern Loess Plateau in Shaanxi. The results showed that:(1)the central and southern part of the Loess Plateau in Shaanxi experienced 73 floods in 277 years during the Ming Dynasty,with an average occurrence frequency of 3.78 years; mild floods,middle floods,great floods and serious floods accounted for 19.18%,61.64%,16.44%,and 2.74% of the total occurrences,respectively,and mild floods and middle floods were dominant;(2)it could be divided into six stages:1368—1427,1428—1487,1488—1517,1518—1567,1568—1587 and 1588—1644; the first,third and fifth stages were the periods with less floods,and the second,fourth and sixth stages were the periods with frequent floods; the frequency and level of flood disasters in the middle and late Ming Dynasty were significantly higher than those in the early period;(3)the distribution of flood disasters was mostly concentrated in summer and autumn;(4)in the Ming Dynasty,the flood disasters in the central and southern part of the Loess Plateau in Shaanxi had occurrence cycles of 4-year,6-year,20-year,and 58-year;(5)the occurrence of flood disasters in the central and southern Loess Plateau in the Ming Dynasty was the result of both natural and human factors; the warm and humid climate and the enhancement of summer monsoon activity were the main factors on flood disasters in Ming Dynasty in the study area,and the flood disasters were mainly the response to climate warming and humidity. The factors such as imperfect urban facilities and excessive reclamation also had some influence on the flood disasters. To sum up,the change stage of flood disasters in this area is obvious,which is mainly controlled by the fluctuation of natural factors. In order to strengthen the prevention and control of flood disasters in this area,relevant monitoring and management are urgently needed.

References:: [1] Zhang S D,Zhang D D. Population-influenced spatiotemporal pattern of natural disaster and social crisis in China,AD1-1910[J]. Science China(Earth Sciences),2019,62(7):1138-1150.
[2] 赵映慧,郭晶鹏,毛克彪,等.1949—2015年中国典型自然灾害及粮食灾损特征[J].地理学报,2017,72(7):1261-1276.
[3] 苗茜,谢志清,曾燕,等.基于统计-FloodArea模型的平原水网区致灾临界雨量研究[J].自然资源学报,2018,33(9):1563-1574.
[4] 熊俊楠,龚颖,刘志奇,等.基于灰色理论的西藏暴雨洪涝预测[J].冰川冻土,2019,41(2):457-469.
[5] 吴先华,周蕾,高歌,等.考虑防灾减灾能力的洪涝灾害灾损率曲线构建:以里下河地区的李中镇为例[J].地理科学进展,2016,35(2):223-231.
[6] 张桂香,霍治国,吴立,等.1961—2010年长江中下游地区农业洪涝灾害时空变化[J].地理研究,2015,34(6):1097-1108.
[7] 黄河,范一大,杨思全,等.基于多智能体的洪涝风险动态评估理论模型[J].地理研究,2015,34(10):1875-1886.
[8] 张会,李铖,程炯,等.基于“H-E-V”框架的城市洪涝风险评估研究进展[J].地理科学进展,2019,38(2):175-190.
[9] 徐玉霞,许小明,马楠.县域尺度下的陕西省洪涝灾害风险评估及区划[J].干旱区地理,2018,41(2):306-313.
[10] 温克刚,翟佑安.中国气象灾害大典·陕西卷[M].北京:气象出版社,2005.
[11] 袁祖亮.中国灾害通史·明代卷[M].郑州:郑州大学出版社,2009.
[12] 聂树人.陕西自然地理[M].西安:陕西人民出版社,1981.
[13] 张冲,赵景波,张淑源.渭河流域汉代洪涝灾害研究[J].地理科学,2011,31(9):1151-1156.
[14] 赵景波,马莉.明代陕南地区洪涝灾害研究[J].地球科学与环境学报,2009,31(2):207-211.
[15] 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.
[16] 刘引鸽,胡浩楠,周欢欢,等.近200年来渭河流域干旱洪涝事件特征[J].水土保持研究,2019,26(4):217-223.
[17] 陕西省地方志编纂委员会.陕西省志·黄土高原志[M].西安:陕西人民出版社,1995.
[18] 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.
[19] 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.
[20] 袁林.西北灾荒史[M].兰州:甘肃人民出版社,1994.
[21] 陕西省地方志编纂委员会.陕西省志·气象志[M].北京:气象出版社,2001.
[22] 王寿森.陕西历史自然灾害简要纪实[M].北京:气象出版社,2002.
[23] 马晓华,赵景波,温震军.鄂尔多斯高原西南部清代霜雪灾害研究[J].冰川冻土,2017,39(3):498-504.
[24] 阴雷鹏,赵景波.明代泾河流域洪涝灾害研究[J].干旱区资源与环境,2008,22(8):56-60.
[25] 任世芳.明代汾河流域洪涝灾害发展趋势研究[J].人民黄河,2020,42(8):36-39,44.
[26] Kong D M,Wei G J,Chen M T,et al. Northern South China Sea SST changes over the last two millennia and possible linkage with solar irradiance[J]. Quaternary International,2017,459:29-34.
[27] 葛全胜,郑景云,方修琦,等.过去2000年中国东部冬半年温度变化[J].第四纪研究,2002,22(2):166-173.
[28] Mann M E,Bradley R S,Hughes M K. Northern hemisphere temperatures during the past millennium:Inferences,uncertainties,and limitations[J]. Geographical Research Letters,1997,26(6):759-762.
[29] Wang S W,Gong D Y,Zhu J H. Twentieth-century climatic warming in China in the context of the Holocene[J]. the Holocene,2001,11(3):313-321.
[30] 殷淑燕,徐潇悦,党群.陕西省明代水旱灾害与干湿特征[J].干旱区资源与环境,2020,34(1):115-122.
[31] 毕硕本,钱育君,陈昌春,等.1470—1912年西北东部地区旱涝等级重建序列的特征及对比分析[J].干旱区地理,2016,39(1):12-21.
[32] Chen F,Zhang R B,Wang H Q,et al. Updated precipitation reconstruction(AD1482-2012)for Huashan,north-central China[J]. Theoretical and Applied Climatology,2016,123(3/4):723-732.
[33] 施雅风,姚檀栋,杨保.近2000年古里雅冰芯10 a尺度的气候变化及其与中国东部文献记录的比较[J].中国科学:地球科学,1999,29(S1):79-86.
[34] 毕硕本,鲁颖,武玮婷,等.清代华南地区低温灾害与旱涝灾害的相关性分析[J].热带气象学报,2018,34(6):733-744.
[35] 李长安,黄俊华,张玉芬,等.黄河上游末次冰盛期古洪水事件的初步研究[J].地球科学,2002,27(4):456-458.
[36] 王宝鉴,李栋梁,黄玉霞,等.东亚夏季风异常与西北东部汛期降水的关系分析[J].冰川冻土,2004,26(5):563-568.
[37] 张强,林婧婧,刘维成,等.西北地区东部与西部汛期降水跷跷板变化现象及其形成机制[J].中国科学:地球科学,2019,49(12):2064-2078.
[38] 王雅琦,冯娟,李建平,等.西北地区东部夏季降水年际变化特征及其与环流的关系[J].高原气象,2020,39(2):290-300.
[39] 李茜,魏凤英,李栋梁.近540 a东亚夏季海平面气压场的重建及其与数值模拟的比较[J].中国沙漠,2012,32(4):1017-1024.
[40] 延安市志编纂委员会.延安市志[M].西安:陕西人民出版社,1994.
[41] 张立.铜川市志[M].西安:陕西师范大学出版社,1997.
[42] 方钢.明初陕西农业的恢复与发展[J].陕西学前师范学院学报,2016,32(6):32-35.

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Last Update: 2021-08-20