Abstract In this paper,the series of level of cold and warm in winterof Jiangsu Province during Qing Dynasty was reconstructed based on the historical documents. The integrated analysis of multiple timescale features of series was conducted using the Morlet complex wavelet transform method.The result indicated that: (1)The winter climate change of Jiangsu Province in the Qing Dynasty could be divided into two cold periods(1644-1730 AD,1821-1900 AD)and one warm period(1731-1820 AD);(2)The reconstructed series of level of cold and warm displayed a periodic variability in multiple scales,and the obvious ones were on the timescale of 38~42 a,18~20 a,13~15 a and 8 a,in which 8 a and 38~42 a were relatively dominant,and 18~20 a was more significant during 1690-1790 AD, while 13~15 a was more significant before 1720 AD and after 1830 AD;(3)The first to fourth primary periods of the reconstructed series were 42 a,20 a,8 a and 3 a respectively. In 42 a timescale, the climate of Jiangsu Province during Qing Dynasty could be divided into six cold periods and six warm periods.
Corresponding Authors:
About the corresponding author Bi Shuoben, born in 1965, is a professor of Nanjing University of Information Science & Technology. Now he is mainly engaged in GIS and spatial data mining. E-mail:bishuoben@163.com.
About author: Wei Jun,born in 1987,is a master candidate of Nanjing University of Information Science & Technology.Now he is engaged in research of climate of the Ming and Qing Dynasties. E-mail: weijun052700@126.com.
Cite this article:
Wei Jun,Bi Shuoben,Qian Yujun et al. Reconstruction and characteristics of series of level of cold and warm in winter of Jiangsu Province during Qing Dynasty[J]. JOPC, 2013, 15(6): 875-882.
Wei Jun,Bi Shuoben,Qian Yujun et al. Reconstruction and characteristics of series of level of cold and warm in winter of Jiangsu Province during Qing Dynasty[J]. JOPC, 2013, 15(6): 875-882.
卞光辉.2008.中国气象灾害大典·江苏卷[M].北京:气象出版社. 陈海山,朱伟军,邓自旺,等.2004.江苏冬季气温的年代际变化及其背景场分析[J].南京气象学院学报,27(4):433-442. 初子莹,任国玉.2005.近千年温度变化研究的回顾和展望[J].气候与环境研究,10(4):818-825. 傅云燕,杨修群,沈伟.2013.江苏省冬季气温、降水年代际异常及相关分析[J].气象科学,33(2):178-183. 葛全胜,方修琦,郑景云.2002.中国历史时期温度变化特征的新认识:纪念竺可桢《中国过去五千年温度变化初步研究》发表30周年[J].地理科学进展,21(4):311-317. 葛全胜,刘健,方修琦,等.2013.过去2000年冷暖变化的基本特征与主要暖期[J].地理学报,68(5):579-592. 葛全胜,郑景云,满志敏,等.2002.过去2000年中国东部冬半年温度变化序列重建及初步分析[J].地学前缘,9(2):169-181. 郝志新,郑景云,葛全胜,等.2011.中国南方过去400年的极端冷冬变化[J].地理学报,66(11):1479-1485. 李可军,苏同卫,梁红飞.2004.现代黑子观测的太阳黑子活动的周期性[J].科学通报,49(24):2511-2516. 曲建和.1986.我国1470-1954(515)年温度等级序列的初步探讨[J].南京气象学院学报,(4):405-410. 上海气象局,等.1978.华东地区近五百年气候历史资料[G].上海气象局等联合整编. 王绍武,王日昇.1990.1470年以来我国华东四季与年平均气温变化的研究[J].气象学报,48(1):26-35. 王绍武,闻新宇,罗勇,等.2007.近千年中国温度序列的建立[J].科学通报,52(8):958-964. 王绍武,叶瑾琳,龚道溢.1998.中国小冰期的气候[J].第四纪研究,(1):54-64. 王日昇,王绍武.1990.近500年我国东部冬季气温的重建[J].气象学报,48(2):180-189. 魏凤英.2007.现代气候统计诊断与预测技术[M].北京:气象出版社,99-104. 吴志伟,朱筱英,孙瑞林.2001.近40 a江苏省冬季气温异常的演变及其海气背景场特征[J].南京气象学院学报,24(4):581-586. 杨煜达.2007.清代昆明地区(1721—1900年)冬季平均气温序列的重建与初步分析[J].中国历史地理论丛,22(1):17-31. 占腊生,何娟美,叶艺林,等.2006.太阳活动周期的小波分析[J].天文学报,47(2):166-174. 张家诚.1976.气候变迁及其原因[M].北京:科学出版社,1-79. 张德二.2004.中国近三千年气象记录总集[M].江苏南京:凤凰出版社. 张德二.1980.近500年来我国南部冬温状况的初步探讨[J].科学通报,(6):270-272. 张丕远,龚高法.1979.16世纪以来中国气候变化的若干特征[J].地理学报,34(3):238-247. 张向萍,叶瑜,王辉.2011.从1849年长江中下游地区洪涝灾害记录谈整编方志资料的使用[J].古地理学报,13(2):229-235. 郑景云,郑斯中.1993.山东历史时期冷暖旱涝状况分析[J].地理学报,48(4):348-357. 郑景云,葛全胜,方修琦,等.2007.基于历史文献重建的近2000年中国温度变化比较研究[J].气象学报,65(3):428-439. 郑景云,葛全胜,郝志新,等.2003.1736—1999年西安与汉中地区年冬季平均气温序列重建[J].地理研究,22(3):343-348. 周书灿.2007.20世纪中国历史气候研究述论[J].史学理论研究,(4):127-136. 竺可桢.1972.中国近五千年来气候变迁的初步研究[J].考古学报,(1):168-189. 竺可桢,吕炯,张宝堃.1947.中国之温度[M].北京:国立中央研究院气象研究所,55-56. Ge Q S,Wang S B,Zheng J Y.2006.Reconstruction of temperature series in China for the last 5000 years[J].Progress in Natural Science,16(8):838-845. Ge Q S,Zheng J Y,Fang X Q, et al. 2003.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].Holocene,13(6):933-940. IGBP.2009.PAGES science plan and implementation strategy[R].Stockholm: IGBP Secr,3-9.