Vol.24, NO.5, 2013
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Article Navigation >  Journal of Applied Meteorological Science  > 2013  >  24(5): 521-532
Chen Lijuan, Yuan Yuan, Yang Mingzhu, et al. A review of physical mechanisms of the global SSTA impact on EASM. J Appl Meteor Sci, 2013, 24(5): 521-532.
Citation: Chen Lijuan, Yuan Yuan, Yang Mingzhu, et al. A review of physical mechanisms of the global SSTA impact on EASM. J Appl Meteor Sci, 2013, 24(5): 521-532.
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A Review of Physical Mechanisms of the Global SSTA Impact on EASM

  • Laboratory of Climate Studies, National Climate Center, CMA, Beijing 100081

  • Received Date: 2013-04-08
  • Rev Recd Date: 2013-07-12
  • Publish Date: 2013-10-31
    Abstract
  • The impact of global sea surface temperature anomaly (SSTA) on the East Asia Summer Monsoon (EASM) and summer precipitation in China is reviewed from the aspects of physical mechanisms, on the basis of key external forcing signals in short-term climate prediction. Focusing on El Niño-Southern Oscillation (ENSO) cycle in the tropical Pacific and the main SSTA modes in Indian and Atlantic Ocean, their inter-annual variability are further reviewed as well as their different impacts on the EASM, especially their relationship with the main summer rainfall belt in China.During different phases of ENSO cycle, ENSO exerts different impacts on the EASM and the summer precipitation in China. In the developing summer of El Niño, the EASM tends to be weak and the main summer rainfall belt would shift southward in eastern China. However, in the decaying summer of El Niño, the EASM tends to be strong, and the summer precipitation would be below normal in the Yangtze-Huaihe Valley. The situations are approximately reverse for the impact of La Ni a on the EASM and summer precipitation in China, although the impact of La Ni a is not as significant. The influence of ENSO on the EASM and the summer rainfall belt in China is closely correlated with the SSTA in the western Pacific warm pool as well as the resulted convective activities in its northern part. Moreover, the Philippine Sea anticyclone also plays an important role. In recent years, different types of El Niño are widely discussed. It is revealed that the Central Pacific (CP) El Niño not only has different evolution mechanisms, but also shows different impacts on the global atmospheric circulation as compared with the Eastern Pacific (EP) El Niño or classical El Niño.Indian Ocean SSTA modes also show significant influences on the EASM and the summer precipitation in China. For example, the basin-wide warming (cooling) mode in the tropical Indian Ocean would cause a late (an early) South China Sea summer monsoon (SCSSM) onset; in the summer of positive (negative) tropical Indian Ocean dipole phase, more precipitation would occur in South China (North China); during the positive (negative) phase of subtropical southern Indian Ocean dipole, Indian summer monsoon tends to be stronger (weaker), and SCSSM may establish earlier (later). The positive (negative) North Atlantic tri-pole mode would lead to a stronger (weaker) EASM through motivating quasi-barotropic zonal tele-connection wave train across the Eurasian continent.SSTA is the important pre-signal on the prediction of summer precipitation anomaly in China. Because of the predictability of short-term climate prediction, it is still difficult to give high skill prediction for summer rainfall anomaly in China. Some advices and requirements on the physical mechanism research and dynamical model development are proposed in order to improve the prediction of the EASM and summer rainfall in China.
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    References(135)
  • [1]
    李维京.现代气候业务.北京:气象出版社, 2012:202-203.
    [2]
    刘永强, 丁一汇.ENSO事件对我国天气气候的影响.应用气象学报, 1992, 3(4):473-481. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=19920476&flag=1
    [3]
    倪允琪, 沈新勇.ENSO动力学及其数值模拟的研究评述.应用气象学报, 1998, 9(2):239-245. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=19980233&flag=1
    [4]
    金祖辉, 陶诗言.ENSO循环与中国东部地区夏季和冬季降水关系的研究.大气科学, 1999, 23(6):663-672. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK199906003.htm
    [5]
    张人禾, 李强.热带海洋变异对东亚季风的影响.气象, 2004, 30(12):22-26. doi:  10.3969/j.issn.1000-0526.2004.12.005
    [6]
    王蕾, 张人禾.不同区域海温异常对中国夏季旱涝影响的诊断研究和预测试验.大气科学, 2006, 30(6):1147-1159. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200606008.htm
    [7]
    张人禾, 殷永红, 李清泉, 等.利用ARGO资料改进ENSO和我国夏季降水气候预测.应用气象学报, 2006, 17(5):538-547. doi:  10.11898/1001-7313.20060511
    [8]
    魏凤英.我国短期气候预测的物理基础及其预测思路.应用气象学报, 2011, 22(1):1-11. doi:  10.11898/1001-7313.20110101
    [9]
    王万秋.土壤温湿异常对短期气候影响的数值模拟试验.大气科学, 1991, 15(5):115-123. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK199105013.htm
    [10]
    李巧萍, 丁一汇, 董文杰.土壤湿度异常对区域短期气候影响的数值模拟试验.应用气象学报, 2007, 18(1):1-11. doi:  10.11898/1001-7313.20070102
    [11]
    Zhang R H, Zuo Z Y.Impact of spring soil moisture on surface energy balance and summer monsoon circulation over East Asia and precipitation in East China.J Climate, 2011, 24:3309-3322. doi:  10.1175/2011JCLI4084.1
    [12]
    陈烈庭, 阎志新. 青藏高原冬春季积雪对大气环流和我国南方汛期降水的影响//中长期水文气象预报文集 (第一集). 北京: 水利电力出版社, 1979: 145-148.
    [13]
    韦志刚, 罗四维, 董文杰, 等.青藏高原积雪资料分析及其与我国夏季降水的关系.应用气象学报, 1998, 9(增刊):39-46. http://www.cnki.com.cn/Article/CJFDTOTAL-YYQX8S1.005.htm
    [14]
    Wu B Y, Yang K, Zhang R H.Eurasian snow cover variability and its association with summer rainfall in China.Adv Atmos Sci, 2009, 26(1):31-44, doi: 10.1007/s00376-009-0031-2.
    [15]
    Zhao P, Zhang X, Zhou X J, et al.Sea-ice extent anomaly in the North Pacific and impact on the East Asian summer monsoon rainfall.J Climate, 2004, 17:3434-3447. doi:  10.1175/1520-0442(2004)017<3434:TSIEAI>2.0.CO;2
    [16]
    王嘉, 郭裕福.北半球海冰强迫作用下大气可预报性研究.应用气象学报, 2004, 15(3):291-305. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20040338&flag=1
    [17]
    Wu B, Zhang R, Wang B, et al.On the association between spring Arctic sea ice concentration and Chinese summer rainfall.Geophys Res Lett, 2009, 36, L09501, doi: 10.1029/2009GL037299.
    [18]
    Zhang J Y, Dong W J, Fu C B, et al.The influence of vegetation cover on summer precipitation in China:A statistical analysis of NDVI and climate data.Adv Atmos Sci, 2003, 20(6):1002-1006. doi:  10.1007/BF02915523
    [19]
    Zuo Z Y, Zhang R H, Zhao P.The relation of vegetation over the Tibetan Plateau to rainfall in China during the boreal summer.Clim Dyn, 2011, 36:1207-1219. doi:  10.1007/s00382-010-0863-6
    [20]
    陈兴芳, 赵振国.中国汛期降水预测研究及应用.北京:气象出版社, 2000:191-194.
    [21]
    王绍武.现代气候学研究进展.北京:气象出版社, 2001:304-326.
    [22]
    Wang B, Wu R G, Fu X.Pacific-East Asian teleconnection:How does ENSO affect East Asian climate?J Climate, 2000, 13:1517-1535. doi:  10.1175/1520-0442(2000)013<1517:PEATHD>2.0.CO;2
    [23]
    Wang B, Ding Q, Fu X, et al.Fundamental challenge in simulation and prediction of summer monsoon rainfall.Geophys Res Lett, 2005, 32, L15711, doi: 10.1029/2005GL022734.
    [24]
    Zhang Renhe, Akimasa Sumi, Masahide Kinoto.A diagnostic study of the impact of El Nino on the precipitation in China.Adv Atmos Sci, 1999, 16(2):229-241. doi:  10.1007/BF02973084
    [25]
    Ropelewski C F, Halpert M S.Global and regional scale precipitation patterns associated with the El Niño/Southern Oscillation.Mon Wea Rev, 1987, 115:1606-1626. doi:  10.1175/1520-0493(1987)115<1606:GARSPP>2.0.CO;2
    [26]
    Ropelewski C F, Halpert M S.Precipitation patterns associated with the high index phase of the Southern Oscillation.J Climate, 1989, 2:268-284. doi:  10.1175/1520-0442(1989)002<0268:PPAWTH>2.0.CO;2
    [27]
    Halpert M S, Ropelewski C F.Surface temperature patterns associated with the Southern Oscillation.J Climate, 1992, 5:577-593. doi:  10.1175/1520-0442(1992)005<0577:STPAWT>2.0.CO;2
    [28]
    Huang R H, Wu Y F.The influence of ENSO on the summer climate change in China and its mechanism.Adv Atmos Sci, 1989, 6:21-32. doi:  10.1007/BF02656915
    [29]
    符淙斌, 腾星林.我国夏季的气候异常与埃尔尼诺/南方涛动现象的关系.大气科学, 1988, 12(增刊):133-141. http://cdmd.cnki.com.cn/Article/CDMD-10423-2009172361.htm
    [30]
    陈文.El Nino和La Nina事件对东亚冬、夏季风循环的影响.大气科学, 2002, 26(5):595-610. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200205001.htm
    [31]
    倪东鸿, 孙照渤, 赵玉春.ENSO循环在夏季的不同位相对东亚夏季风的影响.南京气象学院学报, 2000, 23(1):18-54. http://www.cnki.com.cn/Article/CJFDTOTAL-NJQX200001007.htm
    [32]
    Huang R H, Li C Y.Influence of the Heat Source Anomaly over the Tropical Western Pacific on the Subtropical High over East Asia.Proceeding of the International Conference on the General Circulation of East Asia, 1987:40-51.
    [33]
    Huang R H, Sun F Y.Impact of the tropical western Pacific on the East Asian summer monsoon.J Meteor Soc Japan, 1992, 70:243-256. doi:  10.2151/jmsj1965.70.1B_243
    [34]
    Huang R H, Yin B Y, Liu A D.Intraseasonal Variability of the East Asian Summer Monsoon and Its Association with the Convective Activities in the Tropical Western Pacific//Ye Duzheng.Climate Variability.Beijing:Chinese Meteorological Press, 1992:134-155.
    [35]
    曹杰, 黄荣辉, 谢应齐, 等.西太平洋副热带高压演变物理机制的研究.中国科学:D辑, 2002, 32:659-666. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200208005.htm
    [36]
    Huang R H, Wu S S.Impact of the Thermal State of the Tropical Western Pacific on the Onset of the South China Sea Summer Monsoon.Proceedings of the Third International Symposium on Asian Monsoon System (ISAM3), 2001:8-21.
    [37]
    黄荣辉, 陈文, 丁一汇, 等.关于季风动力学以及季风与ENSO循环相互作用的研究.大气科学, 2003, 27(4):484-502. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200304004.htm
    [38]
    黄荣辉, 陈文.关于亚洲季风与ENSO循环相互作用研究最近的进展.气候与环境研究, 2002, 7(2):146-159. http://www.cnki.com.cn/Article/CJFDTOTAL-QHYH200202002.htm
    [39]
    Zhang R H, Sumi A, Kimoto M.Impact of El Nino on the East Asian monsoon:A diagnostic study of the '86/87 and '91/92 events.J Meteor Soc Japan, 1996, 74:49-62. doi:  10.2151/jmsj1965.74.1_49
    [40]
    Zhang R H, Sumi A.Moisture circulation over East Asia during El Nino episode in northern winter, spring and summer.J Meteor Soc Japan, 2002, 80:213-227. doi:  10.2151/jmsj.80.213
    [41]
    Wang B, Zhang Q.Pacific-East Asian teleconnection.Part Ⅱ:How the Philippine Sea anomalous anticyclone is established during El Niño development?J Climate, 2002, 15:3252-3265.
    [42]
    高辉, 王永光.ENSO对中国夏季降水可预测性变化的研究.气象学报, 2007, 65(1):131-137. doi:  10.11676/qxxb2007.013
    [43]
    宗海峰, 陈烈庭, 张庆云.ENSO与中国夏季降水年际变化关系的不稳定性特征.大气科学, 2010, 34(1):184-192. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK201001017.htm
    [44]
    袁媛, 杨辉, 李崇银.不同分布型El Nino事件及对中国次年夏季降水的可能影响.气象学报, 2012, 70(3):467-478. doi:  10.11676/qxxb2012.039
    [45]
    Rasmusson E M, Wallace J M.Meteorological aspects of El Niño/Southern Oscillation.Science, 1983, 222:1195-1202. doi:  10.1126/science.222.4629.1195
    [46]
    Fu C B, Diaz H, Fletcher J.Characteristics of the response of sea surface temperature in the central Pacific associated with the warm episodes of the Southern Oscillation.Mon Wea Rev, 1986, 114:1716-1738. doi:  10.1175/1520-0493(1986)114<1716:COTROS>2.0.CO;2
    [47]
    Wang B.Interdecadal changes in El Niño onset in the last four decades.J Climate, 1995, 8:267-285. doi:  10.1175/1520-0442(1995)008<0267:ICIENO>2.0.CO;2
    [48]
    李崇银.气候动力学引论.北京:气象出版社, 2000:240-260.
    [49]
    Ashok K, Behera S K, Rao S A, et al.El Niño Modoki and its possible teleconnection.J Geophys Res, 2007, 112:C11007, doi: 10.1029/2006JC003798.
    [50]
    Yu J Y, Kao H Y.Decadal changes of ENSO persistence barrier in SST and ocean heat content indices:1958—2001.J Geophys Res, 2007, 112, D13106, doi: 10.1029/2006JD007654.
    [51]
    Kao H Y, Yu J Y.Contrasting Eastern-Pacific and Central-Pacific types of ENSO.J Climate, 2009, 22:615-632. doi:  10.1175/2008JCLI2309.1
    [52]
    Kug J S, Jin F F, An S I.Two types of El Niño events:Cold tongue El Niño and warm pool El Niño.J Climate, 2009, 22:1499-1515. doi:  10.1175/2008JCLI2624.1
    [53]
    Yeh S W, Kug J S, Dewitte B, et al.El Niño in a changing climate.Nature, 2009, 461:511-514. doi:  10.1038/nature08316
    [54]
    Lee T, McPhaden M J.Increasing intensity of El Niño in the central-equatorial Pacific.Geophys Res Lett, 2010, 37, L14603, doi: 10.1029/2010GL044007.
    [55]
    任福民, 袁媛, 孙丞虎, 等.近30年ENSO研究进展回顾.气象科技进展, 2012, 2(3):17-24. http://www.cnki.com.cn/Article/CJFDTOTAL-QXKZ201203005.htm
    [56]
    Yuan Y, Yang S.Impacts of different types of El Niño on the East Asian climate:Focus on ENSO cycles.J Climate, 2012, 25:7702-7722, doi: 10.1175/JCLI-D-11-00576.1.
    [57]
    Kim H M, Webster P J, Curry J A.Impact of shifting patterns of Pacific Ocean warming on North Atlantic tropical cyclones.Science, 2009, 325:77-80, doi: 10.1126/science.1174062.
    [58]
    Chen G, Tam C.Different impacts of two kinds of Pacific Ocean warming on tropical cyclone frequency over the western North Pacific.Geophys Res Lett, 2010, 37, L01803, doi: 10.1029/2009GL041708.
    [59]
    Wang G, Hendon H H.Sensitivity of Australian rainfall to inter-El Niño variations.J Climate, 2007, 20:4211-4226. doi:  10.1175/JCLI4228.1
    [60]
    Taschetto A S, England M H.El Niño Modoki impacts on Australian rainfall.J Climate, 2009, 22:3167-3174. doi:  10.1175/2008JCLI2589.1
    [61]
    Weng H Y, Ashok K, Behera S K, et al.Impacts of recent El Niño Modoki on dry/wet conditions in the Pacific Rim during boreal summer.Climate Dyn, 2007, 29:113-129. doi:  10.1007/s00382-007-0234-0
    [62]
    Weng H, Behera S K, Yamagata T.Anomalous winter climate conditions in the Pacific rim during recent El Niño Modoki and El Niño events.Climate Dynamics, 2009, 32:663-674, doi: 10.1007/s00382-008-0394-6.
    [63]
    Weng H, Wu G X, Liu Y M, et al.Anomalous summer climate in China influenced by the tropical Indo-Pacific Oceans.Climate Dynamics, 2011, 36:769-782, doi: 10.1007/s00382-009-0658-9.
    [64]
    Feng J, Chen W, Tam C Y, et al.Different impacts of El Niño and El Niño Modoki on China rainfall in the decaying phases.Int J Climatol, 2011, 31(14):2091-2101, doi: 10.1002/joc.2217.
    [65]
    Feng J, Wang L, Chen W, et al.Different impacts of two types of Pacific Ocean warming on Southeast Asian rainfall during boreal winter.J Geophys Res, 2010, 115, D24122, doi: 10.1029/2010JD014761.
    [66]
    Feng J, Li J.Influence of El Niño on spring rainfall over south China.J Geophys Res, 2011, 116, D13102, doi: 10.1029/2010JD015160.
    [67]
    Larkin N K, Harrison D E.Global seasonal temperature and precipitation anomalies during El Niño autumn and winter.Geophys Res Lett, 2005, 32:L13705, doi: 10.1029/2005GL022738.
    [68]
    Yuan Y, Yang S, Zhang Z Q.Different evolutions of the Philippine Sea anticyclone between Eastern and Central Pacific El Niño:Effects of Indian Ocean SST.J Climate, 2012, 25:7867-7883, doi: 10.1175/JCLI-D-12-00004.1.
    [69]
    袁媛.热带印度洋海温异常及其与ENSO事件的相互联系.北京:中国科学院研究生院, 2008.
    [70]
    晏红明, 袁媛.印度洋海温异常的特征及其影响.北京:气象出版社, 2012.
    [71]
    Saji N H, Goswami B N, Vinayachandran P N, et al.A dipole mode in the tropical Indian Ocean.Nature, 1999, 401:360-363.
    [72]
    Webster P J, Moore A M, Loschnigg J P, et al.Coupled ocean-atmosphere dynamics in the Indian Ocean during 1997—98.Nature, 1999, 401:356-360. doi:  10.1038/43848
    [73]
    肖莺, 张祖强, 何金海.印度洋偶极子研究进展综述.热带气象学报, 2009, 25(5):621-627. http://www.cnki.com.cn/Article/CJFDTOTAL-RDQX200905014.htm
    [74]
    肖子牛, 晏红明, 李崇银.印度洋地区异常海温的偶极振荡与中国降水及温度的关系.热带气象学报, 2002, 18(4):335-344. http://www.cnki.com.cn/Article/CJFDTOTAL-RDQX200204005.htm
    [75]
    唐卫亚, 孙照渤.印度洋海温偶极振荡对东亚环流及降水影响.南京气象学院学报, 2005, 28(3):316-322. http://www.cnki.com.cn/Article/CJFDTOTAL-NJQX200503004.htm
    [76]
    钱玮, 管兆勇.中国南方夏季降水与热带印度洋偶极型海温异常的联系.南京气象学院学报, 2007, 30(1):9-16. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGQX200711005118.htm
    [77]
    袁媛, 李崇银.热带印度洋偶极子与ENSO事件关系的年代际变化.科学通报, 2008, 53(12):1429-1436. doi:  10.3321/j.issn:0023-074X.2008.12.012
    [78]
    Yuan Y, Li C Y.Decadal variability of the IOD-ENSO relationship.Chinese Science Bulletin, 2008, 53:1745-1752.
    [79]
    刘宣飞, 袁慧珍, 管兆勇.ENSO对IOD与中国夏季降水关系的影响.热带气象学报, 2008, 24(5):502-506. http://www.cnki.com.cn/Article/CJFDTOTAL-RDQX200805010.htm
    [80]
    Meyers G.Variation of Indonesian throughflow and El Niño/Southern Oscillation.J Geophys Res, 1996, 101:12255-12263. doi:  10.1029/95JC03729
    [81]
    Klein S A, Soden B J, Lau N C.Remote sea surface temperature variations during ENSO:Evidence for a tropical atmospheric bridge.J Climate, 1999, 12:917-932. doi:  10.1175/1520-0442(1999)012<0917:RSSTVD>2.0.CO;2
    [82]
    Lau N C, Nath M J.Impact of ENSO on the variability of the Asian-Australian monsoons as simulated in GCM experiments.J Climate, 2000, 13:4287-4309. doi:  10.1175/1520-0442(2000)013<4287:IOEOTV>2.0.CO;2
    [83]
    Yang S, Ding X, Zheng D, et al.Time-frequency characteristics of the relationships between tropical Indo-Pacific SSTs.Adv Atmos Sci, 2007, 24:343-359. doi:  10.1007/s00376-007-0343-z
    [84]
    Xie S P, Annamalai H, Schott F A, et al.Structure and mechanism of south Indian Ocean climate variability.J Climate, 2002, 15:864-878. doi:  10.1175/1520-0442(2002)015<0864:SAMOSI>2.0.CO;2
    [85]
    Wu R, Kirtman B.Understanding the impacts of the Indian Ocean on ENSO variability in a coupled GCM.J Climate, 2004, 17:4019-4031. doi:  10.1175/1520-0442(2004)017<4019:UTIOTI>2.0.CO;2
    [86]
    Annamalai H, Xie S P, McCreary J P, et al.Impact of Indian Ocean sea surface temperature on developing El Niño.J Climate, 2005, 18:302-319. doi:  10.1175/JCLI-3268.1
    [87]
    Yang J, Liu Q, Xie S P, et al.Impact of the Indian Ocean SST basin mode on the Asian summer monsoon.Geophys Res Lett, 2007, 34, L02708, doi: 10.1029/2006GL028571.
    [88]
    Yuan Y, Zhou W, Chan J C L, et al.Impacts of the basin-wide Indian Ocean SSTA on the South China Sea summer monsoon onset.Int J Climatol, 2008, 28:1579-1587. doi:  10.1002/joc.v28:12
    [89]
    Xie S P, Hu K, Hafner J, et al.Indian Ocean capacitor effect on Indo-western Pacific climate during the summer following El Niño.J Climate, 2009, 22:730-747. doi:  10.1175/2008JCLI2544.1
    [90]
    Chou C.Establishment of the low-level wind anomalies over the western North Pacific during ENSO development.J Climate, 2004, 17:2195-2212. doi:  10.1175/1520-0442(2004)017<2195:EOTLWA>2.0.CO;2
    [91]
    Chen J M, Li T, Shih J.Fall persistence barrier of sea surface temperature in the South China Sea associated with ENSO.J Climate, 2007, 20:158-172. doi:  10.1175/JCLI4000.1
    [92]
    Matsuno T.Quasi-geostrophic motions in the equatorial area.J Meteor Soc Japan, 1966, 44:25-43. doi:  10.2151/jmsj1965.44.1_25
    [93]
    Gill A E.Some simple solutions for heat induced tropical circulation.Quart J Roy Meteor Soc, 1980, 106:447-462. doi:  10.1002/(ISSN)1477-870X
    [94]
    李琰, 王亚非, 朱伟军.热带太平洋、印度洋海温异常在菲律宾海异常反气旋建立过程中的作用.气象学报, 2010, 68(6):865-876. doi:  10.11676/qxxb2010.082
    [95]
    Watanabe M, Jin F F.Role of Indian Ocean warming in the development of Philippine Sea anticyclone during ENSO.Geophys Res Lett, 2002, 29, 1478, doi: 10.1029/2001GL014318.
    [96]
    Wu B, Zhou T, Li T.Seasonally evolving dominant interannual variability mode over the East Asia.J Climate, 2009, 22:2992-3005. doi:  10.1175/2008JCLI2710.1
    [97]
    Wu B, Li T, Zhou T.Asymmetry of atmospheric circulation anomalies over the western north Pacific between El Niño and La Nina.J Climate, 2010, 15:4807-4822.
    [98]
    Reason C J C.Warm and cold events in the southeast Atlantic/southwest Indian Ocean region and potential impacts on circulation and rainfall over southern Africa.Meteor Atmos Phys, 1998, 69:49-65. doi:  10.1007/BF01025183
    [99]
    Behera S K, Yamagata T.Subtropical SST dipole in the southern Indian.Geophys Res Lett, 2001, 28(2):327-330. doi:  10.1029/2000GL011451
    [100]
    贾小龙, 李崇银.南印度洋海温偶极子型振荡及其气候影响.地球物理学报, 2005, 48(6):1238-1249. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX200506003.htm
    [101]
    杨明珠, 丁一汇.印度洋海表温度的变化及其对印度夏季季风降水影响的诊断研究.海洋学报, 2006, 28(4):9-16. http://www.cnki.com.cn/Article/CJFDTOTAL-SEAC200604001.htm
    [102]
    晏红明, 李崇银, 周文.南印度洋副热带偶极模在ENSO事件中的作用.地球物理学报, 2009, 52(10):2436-2449. doi:  10.3969/j.issn.0001-5733.2009.10.003
    [103]
    杨明珠, 丁一汇.中国夏季降水对南印度洋偶极子的响应研究.大气科学, 2007, 31(4):685-694. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200704012.htm
    [104]
    Schouten M W, de Ruijter W P M, van Leeuwen P J, et al.An oceanic teleconnection between the equatorial and southern Indian Ocean.Geophys Res Lett, 2002, 29(16), doi: 10.1029/2001GL014542-59-1-4.
    [105]
    杨秋明.南印度洋副热带偶极子型海温异常与全球环流和我国降水变化的关系.海洋学报, 2006, 28(3):47-56. http://www.cnki.com.cn/Article/CJFDTOTAL-SEAC200603004.htm
    [106]
    Ray G P, White W B.Slow oceanic teleconnections linking the Antactic circumpolar wave with the tropical El Niño-Southern Oscillation.J Geophys Res, 1998, 103(C11):24573-24583. doi:  10.1029/98JC01947
    [107]
    Mason S J.Sea-surface temperature-South African rainfall associations, 1910—1989.Int J Climatol, 1995, 15:119-135. doi:  10.1002/(ISSN)1097-0088
    [108]
    Reason C J C.Interannual warm and cool events in the subtropical mid-latitude South Indian Ocean region.Geophys Res Lett, 1999, 26(2):215-218. doi:  10.1029/1998GL900285
    [109]
    丁一汇.高等天气学 (第二版).北京:气象出版社, 2005:212-235.
    [110]
    梁肇宁, 温之平, 吴丽姬.印度洋海温异常和南海夏季风建立迟早的关系:Ⅰ耦合分析.大气科学, 2006, 30(4):619-634. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200604007.htm
    [111]
    温之平, 梁肇宁, 吴丽姬.印度洋海温异常和南海夏季风建立迟早的关系:Ⅱ机理分析.大气科学, 2006, 30(6):1138-1146. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200604007.htm
    [112]
    Gambo K, Lu L, Li W J.Numerical simulation of Eurasian teleconnection pattern in atmospheric circulation during the Northern Hemisphere winter.Adv Atmos Sci, 1987, 4(4):385-394. doi:  10.1007/BF02656739
    [113]
    Wu Z, Wang B, Li J, et al.An empirical seasonal prediction model of the East Asian summer monsoon using ENSO and NAO.J Geophys Res, 2009, 114, D18120, doi: 10.1029/2009JD011733.
    [114]
    Gu W, Li C Y, Wang X, et al.Linkage between Mei-yu precipitation and North Atlantic SST on the decadal time scale.Adv Atmos Sci, 2009, 26(1):101-108. doi:  10.1007/s00376-009-0101-5
    [115]
    Zuo J Q, Li W J, Sun C H, et al.The impact of North Atlantic sea surface temperature tripole on the East Asian summer monsoon.Adv Atmos Sci, 2013, doi:10.1007/s00376-012-2125-5.
    [116]
    张庆云, 陶诗言.亚洲中高纬度环流对东亚夏季降水的影响.气象学报, 1998, 56(2):199-211. doi:  10.11676/qxxb1998.019
    [117]
    Deser C, Timlin M.Atmosphere-ocean interaction on weekly timescales in the North Atlantic and Pacific.J Clim, 1997, 10:393-408. doi:  10.1175/1520-0442(1997)010<0393:AOIOWT>2.0.CO;2
    [118]
    周天军, 宇如聪, 郜永琪, 等.北大西洋年际变率的海气耦合模式模拟.Ⅰ:局地海气相互作用.气象学报, 2006, 64(1):1-17. doi:  10.11676/qxxb2006.001
    [119]
    Barnston A G, Livezey R E.Classification, seasonality and persistence of low-frequency atmospheric circulation patterns.Mon Wea Rev, 1987, 115:1083-1126. doi:  10.1175/1520-0493(1987)115<1083:CSAPOL>2.0.CO;2
    [120]
    左金清, 李维京, 任宏利, 等.春季北大西洋涛动与东亚夏季风年际关系的转变及其可能成因分析.地球物理学报, 2012, 55:384-395. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX201202002.htm
    [121]
    陈文, 康丽华, 王玎.中国夏季降水与全球海温的耦合关系分析.气候与环境研究, 2006, 11:259-269. doi:  10.3878/j.issn.1006-9585.2006.03.02
    [122]
    Saravanan R, Chang P.Interaction between tropical Atlantic variability and El Niño-Southern Oscillation.J Clim, 2000, 13:2177-2194. doi:  10.1175/1520-0442(2000)013<2177:IBTAVA>2.0.CO;2
    [123]
    Lu R, Dong B.Impact of Atlantic sea surface temperature anomalies on the summer climate in the western North Pacific during 1997—1998.J Geophys Res, 2005, 110:D16102, doi: 10.1029/2004JD005676.
    [124]
    容新尧, 张人禾, Li Tim.大西洋海温异常在ENSO影响印度-东亚夏季风中的作用.科学通报, 2010, 55(14):1397-1408. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201014016.htm
    [125]
    Kug J S, Ham Y G.Are there two types of La Ni a?Geophys Res Lett, 2011, 38:L16704, doi: 10.1029/2011GL048237.
    [126]
    Shinoda T, Hurlburt H E, Metzger E J.Anomalous tropical ocean circulation associated with La Ni a Modoki.J Geophys Res, 2011, 116:C12001, doi: 10.1029/2011JC007304.
    [127]
    袁媛, 晏红明.不同分布型La Nina事件及热带大气的响应特征对比.科学通报, 2012, 57(34):3312-3322. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201234012.htm
    [128]
    Yuan Y, Yan H M.Different types of La Ni a events and different responses of the tropical atmosphere.Chinese Science Bulletin, 2013, 58(3):406-415, doi: 10.1007/s11434-012-5423-5.
    [129]
    Hoerling M P, Kumar A, Zhong M.El Niño, La Ni a and the nonlinearity of their teleconnections.J Climate, 1997, 10:1769-1786. doi:  10.1175/1520-0442(1997)010<1769:ENOLNA>2.0.CO;2
    [130]
    Wu B, Li T, Zhou T.Relative contributions of the Indian Ocean and local SST anomalies to the maintenance of the western North Pacific anomalous anticyclone during El Niño decaying summer.J Climate, 2010, 23:2974-2986. doi:  10.1175/2010JCLI3300.1
    [131]
    Wang X, Wang D X, Zhou W, et al.Interdecadal modulation of the influence of La Ni a events on Mei-yu rainfall over the Yangtze River Valley.Adv Atmos Sci, 2012, 29:157-168, doi: 10.1007/s00376-011-1021-8.
    [132]
    Peng S, Robinson W A, Li S.Mechanisms for the NAO responses to the North Atlantic SST tripole.J Climate, 2003, 16:1987-2004. doi:  10.1175/1520-0442(2003)016<1987:MFTNRT>2.0.CO;2
    [133]
    Xie S P, Du Y, Huang G, et al.Decadal shift in El Niño influences on Indo-western Pacific and East Asian climate in the 1970s.J Climate, 2010, 23:3352-3368. doi:  10.1175/2010JCLI3429.1
    [134]
    马音, 陈文, 冯瑞权, 等.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.大气科学, 2012, 36(2):397-410. doi:  10.3878/j.issn.1006-9895.2011.11050
    [135]
    Chen W, Feng J, Wu R.Roles of ENSO and PDO in the link of the East Asian winter monsoon to the following summer monsoon.J Climate, 2013, 26:622-635. doi:  10.1175/JCLI-D-12-00021.1
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    • Received : 2013-04-08
    • Accepted : 2013-07-12
    • Published : 2013-10-31
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