Reconstructing Typhoons in Southeast Coastal Areas during Ming and Qing Dynasties and Analyzing the Factors

SUN Li; BI Shuoben; PAN Wei; CHEN Changchun; XU Zhihui

doi:10.6054/j.jscnun.2019106

Journal of South China Normal University (Natural Science Edition) > 2019 > 51(6): 88-97. > DOI: 10.6054/j.jscnun.2019106

SUN Li, BI Shuoben, PAN Wei, CHEN Changchun, XU Zhihui. Reconstructing Typhoons in Southeast Coastal Areas during Ming and Qing Dynasties and Analyzing the Factors[J]. Journal of South China Normal University (Natural Science Edition), 2019, 51(6): 88-97. DOI: 10.6054/j.jscnun.2019106

Citation:

PDF (3996 KB)

Reconstructing Typhoons in Southeast Coastal Areas during Ming and Qing Dynasties and Analyzing the Factors

1.
School of Geographical Sciences, Nanjing University of Information Science and Technology, Nanjing 210044, China
2.
Institute of History of Science and Technology, Nanjing University of Information Science and Technology, Nanjing 210044, China
3.
School of History and Archives, Yunnan University, Yunnan 650091, China

More Information

Received Date: April 23, 2019
Available Online: March 21, 2021

Graphical Abstract

Abstract

Abstract

Through systematically sorting out the historical data such as the chronicles of prefectures and counties, 1 180 typhoon disasters in the southeast coastal areas during Ming and Qing Dynasties are reconstructued and the frequency sequence of typhoon disasters is established. The temporal and spatial distribution of typhoon disasters in the region and their main factors are analyzed. The results are as follows. The impacts of typhoons concentrate in the coastal areas and decrease from the coastal areas to the inland. The decay of typhoons is a rapid process. The area most seriously affected by the typhoons is South China, of which Guangdong Province suffers the most. The factors for typhoons include temperature changes and sunspot. When temperature changes are stable, the typhoon frequency changes smoothly. The typhoon frequency shows great turbulence when temperature fluctuations are steep. When the sunspot cycle is at a low activity value, the subtropical high pressure moves northward, and the influence of typhoon in the southeast coastal areas increases. When the sunspot cycle enters an active period, the subtropical high pressure moves southward, and the influence of typhoons in the southeast coastal areas decreases.
- Ming and Qing dynasties,
- southeast coastal areas,
- time and space characteristics,
- factors,
- typhoon reconstruction

FullText(HTML)

References (32)

References

[1]	CHAN J C L, SHI J E. Frequency of typhoon landfall over Guangdong Province of China during the period 1470-1931[J]. International Journal of Climatology, 2000, 20:183-190. doi: 10.1002/(SICI)1097-0088(200002)20:2<183::AID-JOC479>3.0.CO;2-U
[2]	LIU K, SHEN C, LOUIE K. A 1000-year history of typhoon landfalls in Guangdong, Southern China, reconstructed from Chinese history documentary records[J]. Annals of the Association of American Geographers, 2001, 91(3):453-464. doi: 10.1111/0004-5608.00253
[3]	王洪波.明清苏浙沿海台风风暴潮灾害序列重建与特征分析[J].长江流域资源与环境, 2016, 25(2):342-349. http://d.old.wanfangdata.com.cn/Periodical/cjlyzyyhj201602021 WANG H B. Research on sequence reconstruction and characteristics diagnosis of typhoon storm surges affecting Jiangsu and Zhejiang, AD1368-1911[J]. Resources and Environment in the Yangtze Basin, 2016, 25(2):342-349. http://d.old.wanfangdata.com.cn/Periodical/cjlyzyyhj201602021
[4]	穆海振, 屠其璞. 1949~1995年西太平洋热带气旋活动的气候特征[J].南京气象学院学报, 2000, 23(1):81-86. doi: 10.3969/j.issn.1674-7097.2000.01.013 MU H Z, TU Q Z. Climatological characteristics of tropical cyclone activities in the west pacific[J]. Journal of Nanjing Institute of Meteorology, 2000, 23(1):81-86. doi: 10.3969/j.issn.1674-7097.2000.01.013
[5]	高建国, 朱晓东, 余有胜.我国沿海地区台风灾害影响研究[J].灾害学, 1999, 14(2):73-77. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zhx199902016 GAO J G, ZHU X D, YU Y S. Study of the impact of typhoon disaster on coastal region of China[J]. Journal of Catastrophology, 1999, 14(2):73-77. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zhx199902016
[6]	颜停霞, 毕硕本, 魏军, 等.清代长江三角洲地区重大台风的对比分析[J].热带地理, 2014, 34(3):374-382. http://d.old.wanfangdata.com.cn/Periodical/rddl201403013 YAN T X, BI S B, WEI J, et al. Comparative analysis of major typhoons of the Yangtze River Delta in the Qing Dynasty[J]. Tropical Geography, 2014, 34(3):374-382. http://d.old.wanfangdata.com.cn/Periodical/rddl201403013
[7]	陈香.福建省台风灾害时空变化分析[J].灾害学, 2007, 22(4):66-70. http://d.old.wanfangdata.com.cn/Periodical/zhx200704015 CHEN X. Analysis of temporal and spatial changes of typhoon disasters in Fujian Province[J]. Journal of Catastrophology, 2007, 22(4):66-70. http://d.old.wanfangdata.com.cn/Periodical/zhx200704015
[8]	李晴, 薛积彬.近500年广东沿海地区台风活动历史重建与分析[J].华南师范大学学报(自然科学版), 2018, 50(2):86-93. http://journal-n.scnu.edu.cn/article/id/4120 LI Q, XUE J B. Reconstruction and analysis of historical typhoon activities in coastal areas of Guangdong over the past 500 Years[J]. Journal of South China Normal University (Natural Science Edition), 2018, 50(2):86-93. http://journal-n.scnu.edu.cn/article/id/4120
[9]	严华生, 万云霞, 邓自旺, 等.用正交小波分析近百年来中国降水气候变化[J].大气科学, 2004, 28(1):151-157. http://d.old.wanfangdata.com.cn/Periodical/daqikx200401015 YAN H S, WAN Y X, DENG Z W, et al. Orthogonal wavelet analysis of the variations of the recent 100-years precipitation in China[J]. Chinese Journal of Atmospheric Sciences, 2004, 28(1):51-157. http://d.old.wanfangdata.com.cn/Periodical/daqikx200401015
[10]	佚名.大清帝国全图[M].上海:上海商务印书馆, 1908.
[11]	复旦大学历史地理研究中心.中国历史地理信息系统(CHGIS)[Z/OL]. (2003-06-01)[2019-03-10].http://yugong.fudan.edu.cn/views/chgis_download.php#1911list.
[12]	张德二.中国三千年气象记录总集[M].江苏:凤凰出版社, 2004.
[13]	温克刚.中国气象灾害大典[M].北京:气象出版社, 2008.
[14]	陆人骥.中国历代灾害性海潮史料[M].北京:海洋出版社, 1984.
[15]	赵静波, 李艳芳, 董雯, 等.关中地区清代干旱灾害研究[J].干旱区研究, 2008, 25(6):872-876. ZHAO J B, LI Y F, DONG W, et al. Study on drought disa-sters in the Guanzhong Region in the Qing Dynasty[J]. Arid Zone Research, 2008, 25(6):872-876.
[16]	TORRENCE C, COMPO G P. A practical guide to wavelet analysis[J]. Bulletin of the American Meteorological Society, 1998, 79:61-78. doi: 10.1175/1520-0477(1998)079<0061:APGTWA>2.0.CO;2
[17]	魏凤英.现代气候统计诊断与预测技术[M].北京:气象出版社, 2007.
[18]	邹兆麟, 蔡逢恩.广东省高明县志[M].[出版地不详]: [出版者不详], 1894.
[19]	郭裴.广东通志[M].[出版地不详]: [出版者不详], 1602.
[20]	潘威, 王美苏, 满志敏, 等. 1644~1911年影响华东沿海的台风发生频率重建[J].长江流域资源与环境, 2012, 21(2):237-241. http://www.cqvip.com/QK/71135X/201107/40877361.html PAN W, WANG M S, MAN Z M, et al. Reconstruction of the affecting east China typhoon frequency, 1644~1911AD[J]. Resources and Environment of the Yangtze River Basin, 2012, 21(2):237-241. http://www.cqvip.com/QK/71135X/201107/40877361.html
[21]	冯栻宗.九江儒林乡志[M].南京:江苏古籍出版社, 1992.
[22]	魏学琼, 张向萍, 叶瑜.长江三角洲地区1644—1949年重大台风灾害年辨识与重建[J].陕西师范大学学报(自然科学版), 2013, 41(4):79-84. doi: 10.3969/j.issn.1672-4291.2013.04.016 WEI X Q, ZHANG X P, YE Y. Identification and reconstruction of sever typhoon disasters based on the impacted counties in Yangtze River Delta during 1644-1949[J]. Journal of Shaanxi Normal University(Natural Science Edition), 2013, 41(4):79-84. doi: 10.3969/j.issn.1672-4291.2013.04.016
[23]	梁有叶, 张德二.最近一千年来我国的登录台风及其与ENSO的关系[J].气候变化研究进展, 2007, 3(2):120-121. doi: 10.3969/j.issn.1673-1719.2007.02.011 LIANG Y Y, ZHANG D E. Landing typhoon in China du-ring the last millennium and its relationship with ENSO[J]. Advances in Climate Change Research, 2007, 3(2):120-121. doi: 10.3969/j.issn.1673-1719.2007.02.011
[24]	ZHANG X P, YE Y, FANG X Q, et al. Reconstruction of typhoons in the Yangtze River Delta during 1644-1949AD based on historical chorographies[J]. Journal of Geographical Sciences, 2012, 22(5):810-824. doi: 10.1007/s11442-012-0965-7
[25]	吴祖立, 崔雪森, 张胜茂, 等.南海台风活动特征及其对渔业活动的影响[J].海洋渔业, 2018, 40(5):548-559. doi: 10.3969/j.issn.1004-2490.2018.05.005 WU Z L, CUI X S, ZHANG S M, et al. An analysis of characteristics of typhoons and their impacts on fishery activities in the South China Sea[J]. Marine Fisheries, 2018, 40(5):548-559. doi: 10.3969/j.issn.1004-2490.2018.05.005
[26]	刘大伟.清代入境中国南部沿海台风事件初步重建[D].上海: 复旦大学, 2013.
[27]	孙劭, 黄大鹏, 张颖娴. 2018年夏季登陆中国台风的主要特点及影响评估[J].中国减灾, 2018(19):14-17. doi: 10.3969/j.issn.1002-4549.2018.19.006
[28]	方修琦, 萧凌波, 苏筠, 等.中国历史时期气候变化对社会发展的影响[J].古地理学报, 2017, 19(4):729-736. http://d.old.wanfangdata.com.cn/Periodical/gdlxb201704014 FANG X Q, XIAO L B, SU J, et al. Social impacts of climate change on the history of China[J]. Journal of Palaeo-geography, 2017, 19(4):729-736. http://d.old.wanfangdata.com.cn/Periodical/gdlxb201704014
[29]	GE Q S, ZHENG J Y, FANG X Q, et al. Winter half-year temperature reconstruction for the middle and lower reaches of the Yellow River and Yangtze River, China, during the past 2000 years[J]. The Holocene, 2003, 13(6):933-940. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=10.1191/0959683603hl680rr
[30]	徐振韬, 蒋窈窕.中国古代太阳黑子研究与现代应用[M].南京:南京大学出版社, 1990.
[31]	孙彭龄.浙江的梅雨和台风年际变化[J].浙江气象科技, 1999(3):20-23. http://www.cnki.com.cn/Article/CJFDTotal-ZJQX199903005.htm
[32]	李慧芳.太阳黑子活动与我国不同区域气候变化相关关系研究[D].西安: 陕西师范大学, 2016.

Cited By

Cited by

Periodical cited type(5)

1.	杨雨锟，毕硕本，邱湘开，李士毫. 明清时期中国沿海地区台风灾害的时空特征. 古地理学报. 2024(02): 446-459 .
2.	张森，杨煜达. 1640—1949年影响江浙沪地区超强台风序列的重建. 历史地理研究. 2023(04): 34-47+148 .
3.	潘威，王一帆，白江涛，小林雄河. 1650～1900年代华东、日本入境台风路径变化及社会影响. 第四纪研究. 2021(02): 589-599 .
4.	杨昊岩，栾涛，韩仲志，倪建功，高霁月. 基于深度学习声谱图分类的“听声识风”. 华南师范大学学报(自然科学版). 2021(05): 10-16 .
5.	廖茂传，衷海燕. 历史时期广东沿海风暴潮灾害研究. 防灾科技学院学报. 2020(04): 99-105 .

Other cited types(0)

Get Citation

PDF

XML

Article views (1561) PDF downloads (51) Cited by(5)

Turn off MathJax

Article Contents

Abstract

References

Reconstructing Typhoons in Southeast Coastal Areas during Ming and Qing Dynasties and Analyzing the Factors

Abstract

References

Cited by

Periodical cited type(5)

Other cited types(0)

Catalog

Export File

Citation

Format

Content