Comparison of Reanalysis Data and Observations about Summer Maximum Temperature on Different Time Scales in Eastern China

  • ZHANG Ting ,
  • GAO Qingjiu ,
  • SUN Yuting
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  • Climate Dynamics Research Center (CDRC) of the College of Atmospheric Sciences/Key Laboratory of Meteorological Disaster of the Ministry of Education (ELME)/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science & Technology, Nanjing 210044, China;Hubei province public meteorological service center, Wuhan 430074, China

Received date: 2015-10-26

  Online published: 2017-04-28

Abstract

Based on daily maximum temperature derived from the ground observation dataset of China meteorological data sharing network (OT) and JRA-55, ERA-Interim, NCEP/NCAR, NCEP/DOE reanalysis datasets, respectively, linear trend analysis, variance analysis, EOF analysis and filtering methods were used to compare multi-scale features of reanalysis and observation daily maximum temperature in summer during 19792013 in eastern China.Results show that: The average daily maximum temperature in summer during 1979-2013 decreased gradually from south to north and is above 30 ℃ to the south of the middle and lower reaches of the Yangtze River; The ability of reanalysis data to depict these characteristics from high to low is JRA-55, ERA-Interim, NCEP/DOE, NCEP/NCAR.In recent 35 years, the daily maximum temperature in summertime in the eastern region shows increasing trend, while the middle and lower reaches of the Yangtze river and eastern Inner Mongolia region shows obvious increase trend; The ability of reanalysis data to reproduce the characteristics in different regions have their own advantages and disadvantages, with JRA-55 slightly better than other datasets.The average daily maximum temperature in summer shows opposite distribution to the north and south of the middle and lower reaches of the Yangtze River, the distribution of ERA-Interim is very closely to the observations, then the NCEP/DOE.The temporal feature of summer maximum temperature is interannual variation, the ERA-Interim data is the one which interannual feature is most similar to the observations'.After 21st century, the temporal characteristics of JRA-55, NCEP/NCAR and NCEP/DOE is relatively similar to the observation data, showing the amplitude decreased and then picks up; The daily maximum temperature of summer main period is 20~60 days.The variance contribution of intra seasonal variability of the summer daily maximum temperature in Yunnan, Guizhou, Northeast China and the eastern Gansu, Shanxi area is larger.The reproduction ability of the 4 reanalysis for intra-seasonal variability from high to low is JRA-55, ERA-Interim, NCEP/DOE and NCEP/NCAR.

Cite this article

ZHANG Ting , GAO Qingjiu , SUN Yuting . Comparison of Reanalysis Data and Observations about Summer Maximum Temperature on Different Time Scales in Eastern China[J]. Plateau Meteorology, 2017 , 36(2) : 468 -479 . DOI: 10.7522/j.issn.1000-0534.2016.00030

References

[1]Cornes R C, Jones P D.2013.How well does the ERA-Interim reanalysis replicate trends in extremes ofsurface temperature across Europe?[J].J Geophys Res Atmos, 118(18): 10262-10276.
[2]Field C B.2012.Managing the risks of extreme events and disasters to advance climate change adaptation: special report of the intergovernmental panel on climate change[M].Cambridge: Cambridge University Press, 1-19.
[3]Kobayashi S, Ota Y, Harada Y, et al.2015.The JRA-55 Reanalysis: General Specifications and Basic Characteristics[J].J Meteor Soc Japan, 93(1): 5-48.
[4]Kanamitsu M, Ebisuzaki W, Woollen J, et al.2002.NCEP-DOE AMIP-II reanalysis (R-2)[J].Bull Amer Meteor Soc, 83(11): 1631-1643.
[5]Kistler R, Collins W, Saha S, et al.2001.The NCEP-NCAR 50-year reanalysis: monthly means CD-ROM and documentation[J].Bull Amer Meteor Soc, 82(2): 247-268.
[6]North G R, Bell T, Cahalan R, et al.1982.Sampling errors in the estimation of empirical orthogonal function[J].Mon Wea Rev, 110(7): 699-706.
[7]Onogi K, Tsutsui J, Koide H, et al.2007.The JRA-25 reanalysis[J].J Meteor Soc Japan, 85(3): 369-432.DOI: 10.2151/jmsj.85.369.
[8]Shea D J.1994.An introduction to atmospheric and oceanographic data[J].National Center for Atmospheric Research Tech.Note 404, 136.http: [WT《Times New Roman》]//<a href="http://www.dss.ucar.edu/docs/data-intro-technote/tn-404.pdf.">dss.ucar.edu/docs/data-intro-technote/tn-404.pdf.</a>[2015-10-26].
[9]You Q L, Fraedrich K, Min J Z, et al.2013.Can temperature extremes in China be calculated from reanalysis?[J].Global &amp; Planetary Change, 111(4): 268-279.
[10]Zhao T, Guo W, Fu C.2008.Calibrating and evaluating reanalysis surface temperature error by topographic correction[J].J Climate, 21(6): 1440-1446.
[11]曹丽娟, 严中伟.2011.地面气候资料均一性研究进展[J].气候变化研究进展, 7(2): 129-135.
[12]Cao Lijuan, Yan Zhongwei.2011.Progresses in research of homogenization of climate data[J].Adv Climate Change Res, 7(2): 129-135.
[13]陈少勇, 王劲松, 郭俊庭, 等.2012.中国西北地区1961-2009年极端高温事件的演变特征[J].自然资源学报, 27(5): 27-32.
[14]Chen Shaoyong, Wang Jinsong, Guo Junting, et al.2012.Evolution characteristics of the extreme high temperature event in Northwest China from 1961 to 2009[J].J Natural Res, 27 (5): 27-32.
[15]戴泽军, 宇如聪, 李建, 等.2011.三套再分析资料的中国夏季降水日变化特征[J].气象, 37(1): 21-30.
[16]Dai Zejun, Yu Rucong, Li Jian, et al.2011.The characteristics of summer precipitation diunal variations in three reanalysis datasets over China[J].Meteor Mon, 37(1): 21-30.
[17]董敏, 李崇银.2007.热带季节内振荡模拟研究的若干进展[J].大气科学, 31(6): 1114-1122.
[18]Dong Min, Li Chongyin.2007.Some progress in the simulation study of intraseasonal oscillation of the tropical atmosphere[J].Chinese J Atmos Sci, 31(6): 1114-1122.
[19]高庆九, 管兆勇, 蔡佳熙, 等.2010.两种再分析资料中夏季地表气温与中国测站资料的差异[J].大气科学, 34(3): 472-482.
[20]Gao Qingjiu, Guan Zhaoyong, Cai Jiaxi, et al.2010.Differences in 1958-2001 sumertime surface air temperatures between two reanalysis data and observations in China[J].Chinese J Atmos Sci, 34 (4): 471-482.
[21]高庆九. 2013. 中国东部夏季多尺度气候变化研究中再分析资料的比较[D]. 南京: 南京信息工程大学, 56-115.
[22]Gao Qingjiu.2013.Data Intercomparison among reanalyses and observations in perspective of multi-scalevariations of summer climate in East China[D].Nanjing: Nanjing University of Information Science and Technology, 56-115.
[23]何冬燕, 田红, 邓伟涛.2013.三种再分析地表温度资料在青藏高原区域的适用性分析[J].大气科学学报, 36(4): 458-465.
[24]He Dongyan, Tian Hong, Deng Weitao.2013.Applicability analysis of three reanalysis surf-ace temperature data over the Tibetan Plateau[J].Trans Atmos Sci, 36(4): 458-465.
[25]李汀, 琚建华.2013.亚洲夏季风季节内振荡对云南主汛期降水的影响Ⅱ:云南主汛期季节内振荡活动过程及其对MJO活动的响应[J].高原气象, 32(3): 626-634.
[26]Li Ting, Ju Jianhua.2013.Impact of intra seasonal oscillation in Asian summer monsoon on precipitation in main rainy season of Yunnan Ⅱ: Intra seasonal oscillation activity[J].Plateau Meteor, 32(3): 626-634.DOI: 10.7522/j.issn.1000-0534.2012.00061.
[27]李娇, 任国玉, 任玉玉, 等.2014.资料均一化对沈阳站气温趋势和城市化偏差分析的影响[J].大气科学学报, 37(3): 297-303.
[28]Li Jiao, Ren Guoyu, Ren Yuyu, et al.2014.Effect of data homogenization on temperature trend estimation and urban bias at Shenyang station[J].Trans Atmos Sci, 37(3): 297-303.
[29]李瑞青, 吕世华, 韩博, 等.2012.青藏高原东部三种再分析资料与地面气温观测资料的对比分析[J].高原气象, 31(6): 1488-1502.
[30]Li Ruiqing, LüShihua, Han Bo, et al.2012.Preliminary Comparison and Analyses of Air Temperature at 2m Height between Three Reanalysis Data-Sets and Observation in the East of Qinghai-Xiang Plateau[J].Plateau Meteorology, 31(6): 1488-1502.
[31]梁萍, 陈葆德.2015.近139年中国东南部站点气温变化的多尺度特征[J].高原气象, 34(5): 1324-1329.
[32]Liang Ping, Chen Baode.2015.Multiscale features of climate change for temeprature of centurial weather stations over Southeast China during latest 139 years[J].Plateau Meteor, 34(5): 1324-1329.DOI: 10.7522/j.issn.1000-0534.2014.00058.
[33]吕少宁, 文军, 刘蓉.2011.中国大陆地区不同降水资料的适用性及其应用潜力[J].高原气象, 30(3): 628-640.
[34]LüShaoning, Wen Jun, Liu Rong.2011.Applicability and potential of the different precipitation data in mainland China[J].Plateau Meteor, 30(3): 628-640.
[35]马音, 陈文, 冯瑞权, 等.2012.我国东部梅雨期降水的年际和年代际变化特征及其与大气环流和海温的关系[J].大气科学, 36(2): 397-410.
[36]Ma Yin, Chen Wen, Feng Ruiquan, et al.2012.Interannual and interdecadal variations of precipitation over Eastern China during Meiyu season and their relationships with the atmoshpheric circulation and SST[J].Trans Atmos Sci, 36(2): 397-410.
[37]任福民, 翟盘茂.1998.1951-1990年中国极端气温变化分析[J].大气科学, 22(2): 217-227.
[38]Ren Fumin, Zhai Panmao.1998.Study on changes of China's extreme temperatures during 1951-1990[J].Trans Atmos Sci, 22(2): 217-227.
[39]任国玉, 封国林, 严中伟.2010.中国极端气候变化观测研究回顾与展望[J].气候与环境研究, 15(4): 337-353.
[40]Ren Guoyu, Feng Guolin, Yan Zhongwei.2010.Progresses in observation studies of climate extremes and changes in mainland China[J].Climatic Environ Res, 15(4): 337-353.
[41]施能.2002.气象科学与预报中的多元分析方法[M].北京:气象出版社, 157-159.
[42]Shi Neng.2002.Meteoro-logical science and the forecast method of multivariate analysis[M].Beijing: Meteorological press, 157-159.
[43]孙玉婷, 高庆九, 闵锦忠.2013.再分析温度资料与西藏地区冬、夏季观测气温的比较[J].高原气象, 32(4): 910-920.
[44]Sun Yuting, Gao Qingjiu, Min Jingzhong.2013.Comparison of reanalysis data and obervation about summer/winter surface air temperature in Tibet[J].Plateau Meteor, 32(4): 910-920.DOI: 10.7522/j.issn.1000-0534.2012.000087.
[45]王琼, 张明军, 王圣杰, 等.2013.1962-2011年长江流域极端气温事件分析[J].地理学报, 68(5): 611-625.
[46]Wang Qiong, Zhang Mingjun, Wang Shengjie, et al.2013.Extreme temperature events in Yangtze River basin during 1962-2011[J].Acta Geographica Sinica, 68(5): 611-625.
[47]荀学义, 胡泽勇, 吴学宏, 等.2011.三套位势高度再分析资料在青藏高原地区的对比分析[J].高原气象, 30(6): 1445-1452.
[48]Xun Xueyi, Hu Zeyong, Wu Xuehong, et al.2011.Comparative analyses of three geopotential height reanalysis data in Qinghai Xizang Plateau[J].Plateau Meteor, 30(6): 1445-1452.
[49]杨萍, 刘伟东, 王启光, 等.2010.近40年我国极端温度变化趋势和季节特征[J].应用气象学报, 21(1): 29-36.
[50]Yang Ping, Liu Weidong, Wang Qiguang, et al.2010.The climatic change trend and seasonal characteristics of daily temperature extremes in China for the latest 40 years[J].J Appl Meteor Sci, 21(1): 29-36.
[51]杨续超, 陈葆德, 胡可嘉.2015.城市化对极端高温事件影响研究进展[J].地理科学进展, 34(10): 1220-1228.
[52]Yang Xuchao, Chen Baode, Hu Kejia.2015.A review of impacts of urbanization on extreme heat event[J].Progress in Geography, 34(10): 1220-1228.
[53]俞永强, 蒋国荣, 何金海.2007.大气季节内振荡的数值模拟Ⅱ.全球变暖的影响[J].大气科学, 31(4): 578-586.
[54]Yu Yongqiang, Jiang Guorong, He jinhai.2007.Numerical simulation of the intraseasonal oscillation part Ⅱ: Impact of global warming[J].Chinese J Atmos Sci, 31(4): 578-586.
[55]翟盘茂, 潘晓华.2003.中国北方近50年温度和降水极端事件变化[J].地理学报, 58(增刊): 1-10.
[56]Zhai Panmao, Pan Xiaohua.2003.Change in extreme temperature and precipitation over Northern China during the second half of the 20<sup>th</sup> century[J].Acta Geographica Sinica, 58(Suppl): 1-10.
[57]翟盘茂, 刘静.2012.气候变暖背景下的极端天气气候事件与防灾减灾[J].中国工程科学, 14(9): 55-63.
[58]Zhai Panmao, Liu Jing.2012.Extreme weather/climate events and disaster prevention and mitigation unde-rglobal warming background[J].Engineering Sciences, 14(9): 55-63.
[59]张雷. 2014. 东亚地区城市化对极端气温的影响[D]. 南京: 南京信息工程大学.
[60]Zhang Lei.2014.Urbanization effect on the changes of extreme temperature in eaxt Asia[D].Nanjing: Nanjing University of Information Science and Technology.
[61]赵佳莹, 徐海明.2014.中国区域位势高度场探空与再分析资料的对比分析[J].气象科学, 34(2): 128-138.
[62]Zhao Jiaying, Xu Haiming.2014.Comparison of geopotential height between reanalysis and radiosonde data over China[J].J Meteor Sci, 34(2): 128-138.DOI: 10.369/2013jms.0013.
[63]赵天保, 符淙斌.2009.应用探空观测资料评估几类再分析资料在中国区域的适用性[J].大气科学, 33(3), 634-648.
[64]Zhao Tianbao, Fu Congbin.2009.Applicability evaluation for several reanalysis datasets using the upper-air observations over China[J].Chinese J Atmos Sci, 33(3): 634-648.
[65]赵天保, 艾丽坤, 冯锦明.2004.NCEP再分析资料和中国站点观测资料的分析与比较[J].气候与环境研究, 9(2): 278-294.
[66]Zhao Tianbao, Ai Likun, Feng Jinming.2004.An intercomparison between NCEP reanalysis and observed data over China[J].Climatic Environ Res, 9(2): 278-294.
[67]赵天保, 符淙斌.2009.几种再分析地表气温资料在中国区域的适用性[J].高原气象, 28(3): 594-606.
[68]Zhao Tianbao, Fu Congbin.2009.Applicability evaluation of surface air temperature from several reanalysis datasets in China[J].Plateau Meteor, 28(3): 594-606.
[69]赵天保, 符淙斌, 柯宗建, 等.2010.全球大气再分析资料的研究现状与进展[J].地球科学进展, 25(3): 242-254.
[70]Zhao Tianbao, Fu Congbin, Ke Zongjian, et al.2010.Global atmosphere reanalysis datasets: current status and recent advances[J].Adv Earth Sci, 25(3): 242-254.
[71]周雅清, 任国玉.2009.城市化对华北地区最高、最低气温和日较差变化趋势的影响[J].高原气象, 28(5): 1159-1166.
[72]Zhou Yaqing, Ren Guoyu.2009.The effect of urbanization on maximum, minimum temperatures and daily temperature range in North China[J].Plateau Meteor, 28(5): 1159-1166.
[73]周雅清, 任国玉.2014.城市化对华北地区极端气温事件频率的影响[J].高原气象, 33(6): 1590-1598.
[74]Zhou Y-aqing, Ren Guoyu.2014.Urbanization effect on long-term trends of extreme temperature events in North China[J].Plateau Meteor, 33(6): 1590-1598.DOI: 10.7522/j.issn.1000-0534.2013.00153.
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