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初始强迫风场对Zebiak-Cane海气耦合模式预报能力的影响研究

岳彩军 陆维松 李清泉

岳彩军, 陆维松, 李清泉. 初始强迫风场对Zebiak-Cane海气耦合模式预报能力的影响研究[J]. 热带气象学报, 2005, (5): 506-516.
引用本文: 岳彩军, 陆维松, 李清泉. 初始强迫风场对Zebiak-Cane海气耦合模式预报能力的影响研究[J]. 热带气象学报, 2005, (5): 506-516.
YUE Cai-jun, LU Wei-song, LI Qing-quan. THE EFFECT OF INITIALIZATION IMPACT WIND ON ZEBIAK-CANE COUPLED OCEAN-ATMOSPHERE MODEL PREDICTABILITY[J]. Journal of Tropical Meteorology, 2005, (5): 506-516.
Citation: YUE Cai-jun, LU Wei-song, LI Qing-quan. THE EFFECT OF INITIALIZATION IMPACT WIND ON ZEBIAK-CANE COUPLED OCEAN-ATMOSPHERE MODEL PREDICTABILITY[J]. Journal of Tropical Meteorology, 2005, (5): 506-516.

初始强迫风场对Zebiak-Cane海气耦合模式预报能力的影响研究

基金项目: 国家自然科学基金项目(40275016);上海市气象局科研开发项目(0301)联合资助

THE EFFECT OF INITIALIZATION IMPACT WIND ON ZEBIAK-CANE COUPLED OCEAN-ATMOSPHERE MODEL PREDICTABILITY

  • 摘要: 结合观测的海表温度距平(SSTA)对925 hPa NCEP/NCAR再分析风应力距平(以下简称NCEP风应力距平)资料与FSU风应力距平资料进行了比较分析。对比分析了分别以NCEP、FSU风应力距平作为初始强迫风场时的Zebiak-Cane海气耦合模式(简称ZC耦合模式)的预报能力。结果表明:1980、1990年代NCEP风应力距平较FSU风应力距平与观测SSTA匹配更为合理。NCEP风应力距平不仅较FSU风应力距平对ZC海洋模式初始化效果好,尤其在1990年代更为显著,而且在1980、1990年代以N

     

  • [1] ZEBIAK S E, CANE M A. A model El Nino-Southern oscillation[J].Mon Wea Rev, 1987, 115(10): 2262-2278.
    [2] CANE M A, ZEBIAK S E, DOLAN S C. Experimental forecasts of El Nino[J].Nature, 1986, 321(26): 827-832.
    [3] BATTISTI D S. Dynamics and thermodynamics of a warming event in a coupled tropical atmosphere-ocean model[J].J Atmos Sci, 1988, 45(20): 2889-2819.
    [4] GOSWAMI B N, SHUKLA J. Predictability of a coupled ocean-atmosphere model[J].J Climate, 1991, 4(1): 3-22.
    [5] CHEN D, ZEBIAK S E, CANE M A. Initialization and predictability of a coupled ENSO forecast model[J].Mon Wea Rev, 1997, 125(5): 773-788.
    [6] CHEN D, CANE M A, ZEBIAK S E, et al. The impact of sea level data assimilation on the Lamont model prediction of the 1997/1998 El Nino[J].Geophys Res Lett, 1998, 25(15): 2837-2840.
    [7] CHEN D, CANE M A, ZEBIAK S E. The impact of NSCAT winds on predicting the 1997/1998 El Nino: A study with the Lamont model[J].J Geophys Res, 1999, 104(C5): 11321-11327.
    [8] 张祖强, 赵宗慈, 于占江. 简化ENSO预测模式的改进试验[J].热带气象学报, 2004, 20(4): 337-345.
    [9] 岳彩军, 陆维松, 李清泉, 等. Zebiak-Cane海气耦合模式研究进展[J].热带气象学报, 2004, 20(5): 723-730.
    [10] LI Q Q, ZHAO Z C, DING Y H. Prediction and verification of the 1997-1999 El Nino and La Nina by using an intermediate ocean-atmosphere coupled mode[J].Acta Meteor Sinica, 2001, 15(2): 144-159.
    [11] KALNAY E, COAUTHORS. The NCEP/NCAR 40-year reanalysis project[J].Bull Amer Meteorol Soc, 1996, 77(3): 437-472.
    [12] KUG J S, KANG I S, ZEBIAK S E. The impacts of the model assimilated wind stress data in the initialization of anintermediate ocean and the ENSO predictability[J].Geophys Res Lett, 2001, 28(19): 3713-3716.
    [13] KANG I S, KUG J S. An El Nino prediction system using an intermediate ocean and a statistical atmosphere[J].Geophys Res Lett, 2000, 27(8): 1167-1170.
    [14] ZEBIAK S E. Tropical atmosphere-ocean interaction and the El Nino/Southern Oscillation phenomenon[D].Ph.D. thesis, Mass, Inst. of Technol., Cambridge, 1984.
    [15] WANG C, WEISBERG R H. The 1997-98 El Nino evolution relative to previous El Nino events[J].J Climate, 2000, 13(2): 488-501.
    [16] BLUMENTHAL M B. Predictability of a coupled ocean-atmosphere model[J].J Climate, 1991, 4(8): 766-784.
    [17] MU M, DUAN W S, WAN J C. The predictability problems in numerical weather and climate prediction[J].Advance in Atmospheric Sciences, 2002, 19(2): 191-204.
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  • 收稿日期:  2004-05-24
  • 修回日期:  2004-12-18

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