[1]黄荣辉. 我国气候灾害的特征、成因和预测研究进展[J]. 中国科学院院刊, 1999, 3: 188-192.
[2]秦甲, 丁永建, 叶柏生, 等. 两类El Nino事件对我国河西走廊地区水文气象要素的影响[J]. 高原气象, 2011, 30(5): 1279-1285.
[3]王亮, 朱仲元, 刘轩晓, 等. 近50年气候变化对滦河上游径流的影响[J]. 高原气象, 2012, 31(4): 1158-1165.
[4]段旭, 陶云, 段长春, 等. 云南省冰冻灾害气候区划[J]. 高原气象, 2011, 30(3): 683-691.
[5]方海义, 杨书运. 一次北半球中高纬度地区冬季气象灾害分析[J]. 高原气象, 2012, 31(3): 723-730.
[6]邓振镛, 闵庆文, 张强, 等. 中国生态气象灾害研究[J]. 高原气象, 2010, 29(3): 810-817.
[7]Chen D, Mark A C. El Nino prediction and predictability[J]. Journal of Computational Physics, 2007, 227: 3625-3640.
[8]Tang Y, Deng Z, Zhou X, et al. Interdecadal variation of ENSO predictability in multiple models[J]. J Climate, 2008, 21: 4811-4833.
[9]Luo J J, Masson S, Behera S, et al. Extended ENSO predictions using a fully coupled ocean-atmosphere model[J]. J Climate, 2008, 21: 84-93.
[10]Moore A M, Kleeman R. The dynamics of error growth and predictability in a coupled model of ENSO[J]. Quart J Roy Met Soc, 1996, 122: 1405-1446.
[11]Xue Y, Cane M A, Zebaik S E. Predictability of a coupled model of ENSO using singular vector analysis. Part I: Optimal growth in seasonal background and ENSO cycles[J]. Mon Wea Rev, 1997, 125: 2043-2056.
[12]Chen D, Zebiak S E, Busalacchi A J, et al. An improved procedure for El Nio forecasting: Implications for predictability[J]. Science, 1995, 269: 1699-1702.
[13]Chen D, Cane M A, Kaplan A, et al. Predictability of El Nio over the past 148 years[J]. Nature, 2004, 428: 733-736.
[14]Mu Mu, Xu Hui, Duan Wansuo. A kind of initial errors related to 'spring predictability barrier’ for El Nio events in Zebiak-Cane model[J]. Geophys Res Lett, 2007, 34: L03709, doi:10.1029/2006GL-27412.
[15]Mu Mu, Duan Wansuo, Wang Bin. Season-dependent dynamics of nonlinear optimal error growth and El Nio-Southern Oscillation predictability in a theoretical model[J]. J Geophys Res,2007, 112: D10113, doi:10.1029/2005JD006981.
[16]Duan Wansuo, Liu Xinchao, Zhu Keyun, et al. Exploring the initial errors that cause a significant "spring predictability barrier" for El Nino events[J]. J Geophys Res, 2009, 114: C04022, Doi: 10.1029/2008JC004925.
[17]Yu Yanshan, Duan Wansuo, Xu Hui, et al. Dynamics of nonlinear error growth and season-dependent predictability of El Nio events in the Zebiak-Cane model[J]. Quart J Roy Met Soc, 2009, Doi: 10.1002/qj.526.
[18]Duan Wansuo, Zhang Rui. Is model parameter error related to a significant SPB for El Nino events? [J]. Adv Atmos Sci, 2010, 27(5): 1003-1013.
[19]Sperber K R, Slingo J M, Inness P M, et al. On the maintenance and initiation of the intraseasonal oscillation in the NCEP/NCAR reanalysis and in the GLA and UKMO AMIP simulations[J]. Climate Dyn, 1997, 13(11): 769-795.
[20]McPhaden M J. Equatorial waves and the 1997-98 El Nio[J]. Geophys Res Lett, 1999, 26: 2961-2964.
[21]Slingo J M, Rowell D P, Sperber K R, et al. On the predictability of the interannual behavior of the Madden-Julian oscillation and its relationship with El Nio[J]. Quart J Roy Meteor Soc, 1999, 125: 583-610.
[22]Hendon H H, Zhang C, Glick J D. Interannual variation of the Madden-Julian oscillation during Austral Summer[J]. J Climate, 1999, 12: 2538-2550.
[23]Zebiak S E,Cane MA. A model El Nio-Southern Oscillation[J]. Mon Wea Rev, 1987, 115: 2262-2278.
[24]Blumental M B. Predictability of a coupled atmosphere-ocean model[J]. J Climate, 1991, 4: 766-784.
[25]Zebiak S E. On the 30-60 day oscillation and the prediction of El Nio[J]. J Climate, 1989, 15: 1381-1387.
[26]Madden R A. Large intraseasonal fluctuations in wind stress in the tropics[J]. J Geophys Res, 1988, 93: 5333-5340.
[27]Mu Mu, Duan Wansuo. A new approach to studying ENSO predictability: Conditional nonlinear optimal perturbation[J]. China Sci Bull, 2003, 48: 1045-1047.
[28]Duan Wansuo, Mu Mu, Wang Bin. Conditional nonlinear optimal perturbation as the optimal precursors for ENSO events[J]. J Geophys Res, 2004, 109: D23105, doi: 10.1029/2004JD004756.
[29]Duan Wansuo, Xue Feng, Mu Mu. Investigating a nonlinear characteristic of El Nino events by conditional nonlinear optimal perturbation[J]. Atmos Res, 2009, 94(1): 10-18.
[30]Duan Wansuo, Mu Mu. Investigating decadal variability of El Nio Southern Oscillation asymmetry by conditional nonlinear optimal perturbation[J]. J Geophys Res, 2006, 111, C07015, doi: 10.1029/2005JC003458.
[31]Mu M, Sun L, Henk D A. The sensitivity and stability of the ocean's thermocline circulation to finite amplitude freshwater perturbations[J]. J Phys Oceanogr, 2004, 34: 2305-2315.
[32]Mu Mu, Zhou Feifan, Wang Hongli. A method to identify the sensitive areas in targeting for tropical cyclone prediction: conditional nonlinear optimal perturbation[J]. Mon Wea Rev, 2009, 137: 1623-1639.
[33]Mu Mu, Jiang Zhina. A new approach to the generation of initial perturbations for ensemble prediction: Conditional nonlinear optimal perturbation[J]. China Sci Bull, 2008, 53(113): 2062-2068.
[34]Xu Hui, Duan Wansuo. What kind of initial errors cause the severest prediction uncertainty of El Nio in Zebiak-Cane model[J]. Adv Atmos Sci, 2008, 25: 577-584.
[35]Birgin E G, Martinez J M, Raydan M. Nonmonotone spectral projected gradient methods on convex sets[J]. SIAM J Optim, 2000, 10: 1196-1211.
[36]李丽平. 海气系统季节内振荡现象的气候学研究[D]. 南京:南京信息工程大学, 2004.
[37]Giese B S, Urizar S C, Fuckar N S. Southern hemisphere origins of the 1976 climate shift[J]. Geophys Res Lett, 2002, 29(1): 1-4.
[38]刘衍韫. 厄尔尼诺/南方涛动的海气相互作用关键区及对外强迫响应的研究[D]. 青岛:中国海洋大学, 2005.
[39]Reynolds R W, Rayner N A, Smith T M, et al. An improved in situ and satellite SST analysis for climate[J]. J Climate, 2002, 15: 1609-1625.
[40]Kaplan A, Cane M, Kushnir Y, et al. Analyses of global sea surface temperature 1856 1991[J]. J Geophys Res,1998,103: 18567-18589.
[41]Karspeck A, Kaplan A, Cane M. Predictability loss in an intermediate ENSO model due to initial error and atmosphere noise[J]. J Climate, 2006, 19: 3572-3588.
