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1985—2005年东海海表温度时空变化特征分析 被引量:13

Change of sea surface temperature in East China Sea during 1985—2005
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摘要 利用1985—2005年间AVHRR辐射计获取的东海海表温度资料,研究其时空变化特征。1985—2005年间东海海表平均温度总体呈上升趋势。对东海海温距平(SSTA)进行经验正交函数(EOF)分解,得到其2个主要变化模态,EOF1占总方差变化的34.8%,主要变化周期为3~5a,表示1985—2005年中东海绝大部分海域的表层海水温度呈现增温现象,近海比外海增温幅度大。EOF2占总方差变化的10.7%,主要变化周期为2a,显示东南与西北海区的温度异常呈反位相变化,近海海温由负异常为主转变为以正异常为主。东海SSTA以1996年5月为温度转折点,1996年5月前SSTA主要表现为负异常,之后以正异常为主,增暖特征明显。台湾海峡和东海南部海域的SSTA变化幅度基本相当,东海北部变化最剧烈,这3个海区均包含约5~7a的变化周期,与ENSO的相当。ENSO对滞后其2a左右的东海3个海区的SSTA变化影响显著,另外东海南部在滞后ENSO的8~9和16~18个月时也存在较强的响应,这主要缘于黑潮在赤道海温异常的北上输送过程中对东海的影响。与沿岸3个气象观测站的长年资料对比,东海北部海域的海温异常与该地区的气温变化关系最为密切,相关系数达到0.92。 The sea surface temperature(SST) data from AVHRR during 1985—2005 were applied to analyze the variability in East China Sea(ECS) and the warming trend is found in general.The Empirical Orthogonal Function(EOF) and Spectrum analysis were used to analyze the variability of SST anormality(SSTA).The first model(EOF1) explains 34.8% of the total variation and its main period is 3~5 a.It shows that there is a warming trend in most area and the largest variation appear in the inshore area.The period of EOF2(10.7%) is 2 a and it denotes the change of SSTA in south-east area is opposite to that of north-west.The variation range of SSTA in Taiwan Strait and the south in ECS are similar,while that of the north is much stronger.They all contain the period of 5~7 a,same as that of ENSO.The SSTA in 3 area are affected strongly by ENSO and the 2a delay is obvious.There are 8~9 and 16~18 month delay between the south of ECS and ENSO.It mainly due to the anomalous Kuroshio transport.The SSTA of the north shows a close correlation with the variation of air temperature there and the correlation up to 0.92.
出处 《海洋学报》 CAS CSCD 北大核心 2011年第6期9-18,共10页
基金 国家自然科学基金重大研究计划(90511005) 我国近海海洋综合调查与评价专项(908-02-01-03) 863计划项目(2007AA092202) 中央级公益性科研院所基本科研业务费专项资金(中国水产科学研究院东海水产研究所)资助项目(2007T09) 中国科学院海洋环流与波动重点实验室开放基金课题(KLOCAW1010)
关键词 东海 SOI 海表温度 EOF 谱分析 East China Sea SOI SST EOF spectrum analysis
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  • 1HANSEN J, SATO M, RUEDY R, et al. Global warming in the twenty-first century: an alternative scenario[J]. Proc Natl Acad Sei USA, 2000,97(18): 9875-9880.
  • 2BEHRENFELD M J, O'MALLEY R T, SIEGEL D A, et al. Climate-driven trends in contemporary ocean produetivity[J]. Nature, 2006, 444(7120) :752-755.
  • 3CHANG Y S, LEE H, YOUN Y H, et al. Interannual variability and lagged correlation during strong El Nifio events in the Pacific area [R/OL]. http://ichwc2004, metri, re. kr/absfiles/PCL 07. pdf.
  • 4PARK S, CHU P C. Interannual SST variability in the Japan/East Sea and relationship with enviromental variables[J]. Journal of Ocea- nography, 2006,62(2) : 115-132.
  • 5SENJYU T, WATANABE T. Decadal signal in the sea surface temperatures off the San'in coast in the southwestern Japan Seal[R]. Re- ports of Research Institute for Applied mechanics: 127. Japan:Kyushu University,2004.
  • 6JUAN C H, GLADYS B F, ADOLFO M C. Decadal surface ocean variability in the lower gulf of California:records for the past 300 years [J]. Geofisica Internacional, 2003,42 (3) : 397-406.
  • 7鲍献文,万修全,高郭平,吴德星.渤海、黄海、东海AVHRR海表温度场的季节变化特征[J].海洋学报,2002,24(5):125-133. 被引量:68
  • 8STEVE LaDochy, PEDRO Ramirez, WILLIAM C. Patzert. Southern California upwelling: Is recent weakening a result of global war- ming[R/O] http ://ams. confex, com/ams/pdfpapers/119047, pdf.
  • 9张秀芝,裘越芳,吴迅英.近百年中国近海海温变化[J].气候与环境研究,2005,10(4):799-807. 被引量:62
  • 10阎俊岳,李江龙.东海及邻近地区百年来的温度变化[J].海洋学报,1997,19(6):121-126. 被引量:22

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