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A STUDY ON THE IMPACTS OF LATENT HEAT PARAMETERIZATION SCHEME ON PREDICTION SKILL OF ENSO WITH A SIMPLE OCEAN-ATMOSPHERE COUPLED

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  • This study revises Weare’s latent heat parameterization scheme and conducts an associated theoretic analysis. The revised Weare’s scheme is found to present potentially better results than Zebiak’s scheme. The Zebiak-Cane coupled ocean-atmosphere model, initialized by the National Centers for Environmental Prediction and the National Center for Atmospheric Research (NCEP/NCAR) reanalysis of wind stress anomaly at 925 hPa, is referred to as the ZCW coupled model. The atmosphere models of the ZCW coupled model that use Zebiak’s scheme and the revised Weare’s scheme are referred to as the ZCW0 and ZCWN atmosphere models, respectively. The coupled ocean-atmosphere models that use Zebiak’s scheme and the revised Weare’s scheme are referred to as the ZCW0and ZCWN coupled models, respectively. The simulations between the ZCW0 and ZCWN atmosphere models and between the ZCW0 and ZCWN coupled models are analyzed. The results include: (1) The evolution of heat, meridional wind and divergence anomalies simulated by similar ZCW0 and ZCWN atmosphere models, although the magnitudes of the former are larger than those of the latter; (2) The prediction skill of the Niño3 index from 1982 to 1999 by the ZCWN coupled model shows improvement compared with those by the ZCW0 coupled model; (3) The analysis of El Niño events in 1982/1983, 1986/1987, and 1997/1998 and La Niña events in 1984/1985, 1988/1989, and 1998/2000 suggests that the ZCWN coupled model is better than the ZCW0 coupled model in predicting warm event evolution and cold event generation. The results also show the disadvantage of the ZCWN coupled model for predicting El Niño
  • [1] ZEBIAK S E, CANE M A. A model El Ni?o-SouthernOscillation [J]. Mon. Wea. Rev., 1987, 115: 2262-2278.
    [2] BLUMENTHAL M B. Predictability of a coupledocean-atmosphere model [J]. J. Climate, 1991, 4: 766-784.
    [3] MU Mu, DUAN Wan-suo, WANG Jia-cheng. Thepredictability problems in numerical weather and climateprediction [J]. Adv. Atmos. Sci., 2002, 19(2): 191-204.
    [4] CHEN D, ZEBIAK S E, BUSALACCHI A J, et al. Animproved procedure for El Ni?o forecasting: implications forpredictability [J]. Science, 1995, 269: 1699-1702.
    [5] CHEN D, ZEBIAK S E, CANE M A. Initialization andpredictability of a coupled ENSO forecast model [J]. Mon.Wea. Rev., 1997, 125: 773-788.
    [6] CHEN D, CANE M A, ZEBIAK S E, et al. The impact ofsea level data assimilation on the Lamont model prediction ofthe 1997/1998 El Ni?o [J]. Geophys. Res. Lett., 1998, 25:2837-2840.
    [7] CHEN D, CANE M A, ZEBIAK S E. The impact ofNSCAT winds on predicting the 1997/1998 El Ni?o: A studywith the Lamont model [J]. J. Geophys. Res., 1999, 104:11321-11327.
    [8] CHEN D, CANE M A, ZEBIAK S E, et al. Bias correctionof an ocean-atmosphere coupled model [J]. Geophys. Res.Lett., 2000, 27: 2585-2588.
    [9] QIAN Wei-hong, WANG Shao-wu. Multiplespatial-temporal scale of ocean-atmosphere interaction andimprovement of Zebiak-Cane model [J]. Sci. in China (Ser. D),1997, 27(6): 554-559.
    [10] QIAN Wei-hong, Li Li, WANG Shao-wu. An improvedZebiak-Cane model for simulating the spatial structure ofwind field [J]. Chin. J. Atmos. Sci., 1998, 22(3): 257-264.
    [11] LI Qing-quan, ZHAO Zong-ci, DING Yi-hui. Predictionand verification of the 1997-1999 El Ni?o and La Ni?a byusing an intermediate ocean-atmosphere coupled mode [J].Acta Meteor. Sin., 2001, 15(2): 144-159.
    [12] LI Qing-quan, ZHAO Zong-ci. The development of NCCintermediate ocean-atmosphere coupled model and numericalsimulation [J]. Acta Meteor. Sin., 2000, 58(Suppl.): 790-803.
    [13] DUAN Yi-hong, LIANG Xu-dong, LI Yong-ping, et al.Application of the four dimensional variational dataassimilation technique on optimizing the initial conditions ofZ-C model [J]. Acta Meteor. Sin., 2000, 58(5): 524-533.
    [14] YUE Cai-jun, LU Wei-song, LI Qing-quan, et al. Theadvances on the research of Zebiak-Cane ocean-atmospherecoupled model [J]. J. Trop. Meteor., 2004, 20(6): 723-730.
    [15] YUE Cai-jun, LU Wei-song, LI Qing-quan. The effect ofinitialization impact wind on Zebiak-Cane coupledocean-atmosphere model predictability [J]. J. Trop. Meteor.,2005, 21(5): 506-516.
    [16] YUE Cai-jun, LU Wei-song, TAO Li. Evaluation of theprediction performance of a simple coupled ocean-atmospheremodel [J]. J. Nanjing Inst. Meteor., 2005, 28(5): 704-709.
    [17] ZHOU Z X, CARTON J A. Latent heat flux andinterannual variability of the coupled atmosphere-oceansystem [J]. J. Atmos. Sci., 1998, 55: 494-501.
    [18] GILL A E. Some simple solutions for heat-inducedtropical circulation [J]. Quart. J. Roy. Meteor. Soc., 1980, 106:447-462.
    [19] ZEBIAK S E. Tropical atmosphere-ocean interaction and the El Ni?o/Southern Oscillation phenomenon [D]. Ph. D.thesis, Mass, Inst. of Technol., Cambridge, 1984, 26-27.
    [20] ZEBIAK S E. Atmospheric convergence feedback in asimple model for El Ni?o [J]. Mon. Wea. Rev., 1986, 114:1263-1271.
    [21] NEWELL R E, KIDSON J W, VINCENT D G, et al. TheGeneral Circulation of the Tropical Atmosphere andInteractions with Extra-Tropical Latitudes [M]. MIT Press,1974, 371.
    [22] CORNEJO-GARRIDO A G, STONE P H. On the heatbalance of the Walker circulation [J]. J. Atmos. Sci., 1977, 34:1152-1162.
    [23] RAMAGE C S. Sea surface temperature and localweather [J]. Mon. Wea. Rev., 1977, 105: 540-544.
    [24] SCHNEIDER E K, LINDZEN R S. Axially symmetricsteady-state models of the basic state for instability andclimate studies. Part I: linearized calculations [J]. J. Atmos.Sci., 1977, 34: 263-179.
    [25] SCHNEIDER E K. Axially symmetric steady-state modelsof the basic state for instability and climate studies. Part II:Nonlinear calculations [J]. J. Atmos. Sci., 1977, 34: 280-296.
    [26] STEVENS D E, LINDZEN R S, SHAPRIO L J. A newmodel of tropical waves incorporating momentum mixing bycumulus convection [J]. Dyn. Atmos. Oceans. 1977, 1:365-425.
    [27] STEVENS D E, LINDZEN R S. Tropical Wave-CISKwith a moisture and cumulus friction [J]. J. Atmos. Sci., 1978,35: 940-961.
    [28] KLEEMAN R. A simple model of the atmosphericresponse to ENSO sea surface temperature anomalies [J]. J.Atmos. Sci., 1991, 48: 3-18.
    [29] PERIGAUD C, DEWITTE B. El Ni?o-La Ni?a eventssimulated with Cane and Zebiak’s model and observed withsatellite and in situ data. Part I: Model data comparison [J]. J.Climate, 1996, 9: 66-84.
    [30] WANG C. On the atmospheric responses to tropicalPacific heating during the mature phase of El Ni?o [J]. J.Atmos. Sci., 2000, 57: 3767-3781.
    [31] KUG J S, KANG I S, ZEBIAK S E. The impacts of themodel assimilated wind stress data in the initialization of anintermediate ocean and the ENSO predictability [J]. Geophys.Res. Lett., 2001, 28(19): 3713-3716.
    [32] WEARE B C. A simple model of the tropical atmospheredriven by a circulation dependent forcing [J]. Quart. J. Roy.Meteor. Soc., 1986, 112: 409-429.
    [33] WEARE B C. A simple model of the tropical atmospherewith circulation dependent heating and specific humidity [J]. J.Atmos. Sci., 1986, 43(19): 2001-2016.
    [34] DAVID N J, HELD I M. Modeling tropical convergencebased on the moist static energy budget [J]. Mon. Wea. Rev.,1987, 115: 3-12.
    [35] MOORE A M, KLEEMAN R. Stochastic forcing of ENSOby the intraseasonal oscillation [J]. J. Climate, 1999, 12(5):1199-1220.
    [36] DING Yi-hui. Diagnostic and Analytical Methods inSynoptic Dynamics [M]. Beijing: Science Press, 1989,114-116.
    [37] LI Xiao-yan, ZHAI Pan-mao. On indices and indicators ofENSO episodes [J]. Acta Meteor. Sinica, 2000, 58(1):102-109.

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YUE Cai-jun, LU Wei-song, Xiaofan LI. A STUDY ON THE IMPACTS OF LATENT HEAT PARAMETERIZATION SCHEME ON PREDICTION SKILL OF ENSO WITH A SIMPLE OCEAN-ATMOSPHERE COUPLED [J]. Journal of Tropical Meteorology, 2010, 16(1): 10-19.
YUE Cai-jun, LU Wei-song, Xiaofan LI. A STUDY ON THE IMPACTS OF LATENT HEAT PARAMETERIZATION SCHEME ON PREDICTION SKILL OF ENSO WITH A SIMPLE OCEAN-ATMOSPHERE COUPLED [J]. Journal of Tropical Meteorology, 2010, 16(1): 10-19.
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A STUDY ON THE IMPACTS OF LATENT HEAT PARAMETERIZATION SCHEME ON PREDICTION SKILL OF ENSO WITH A SIMPLE OCEAN-ATMOSPHERE COUPLED

Abstract: This study revises Weare’s latent heat parameterization scheme and conducts an associated theoretic analysis. The revised Weare’s scheme is found to present potentially better results than Zebiak’s scheme. The Zebiak-Cane coupled ocean-atmosphere model, initialized by the National Centers for Environmental Prediction and the National Center for Atmospheric Research (NCEP/NCAR) reanalysis of wind stress anomaly at 925 hPa, is referred to as the ZCW coupled model. The atmosphere models of the ZCW coupled model that use Zebiak’s scheme and the revised Weare’s scheme are referred to as the ZCW0 and ZCWN atmosphere models, respectively. The coupled ocean-atmosphere models that use Zebiak’s scheme and the revised Weare’s scheme are referred to as the ZCW0and ZCWN coupled models, respectively. The simulations between the ZCW0 and ZCWN atmosphere models and between the ZCW0 and ZCWN coupled models are analyzed. The results include: (1) The evolution of heat, meridional wind and divergence anomalies simulated by similar ZCW0 and ZCWN atmosphere models, although the magnitudes of the former are larger than those of the latter; (2) The prediction skill of the Niño3 index from 1982 to 1999 by the ZCWN coupled model shows improvement compared with those by the ZCW0 coupled model; (3) The analysis of El Niño events in 1982/1983, 1986/1987, and 1997/1998 and La Niña events in 1984/1985, 1988/1989, and 1998/2000 suggests that the ZCWN coupled model is better than the ZCW0 coupled model in predicting warm event evolution and cold event generation. The results also show the disadvantage of the ZCWN coupled model for predicting El Niño

YUE Cai-jun, LU Wei-song, Xiaofan LI. A STUDY ON THE IMPACTS OF LATENT HEAT PARAMETERIZATION SCHEME ON PREDICTION SKILL OF ENSO WITH A SIMPLE OCEAN-ATMOSPHERE COUPLED [J]. Journal of Tropical Meteorology, 2010, 16(1): 10-19.
Citation: YUE Cai-jun, LU Wei-song, Xiaofan LI. A STUDY ON THE IMPACTS OF LATENT HEAT PARAMETERIZATION SCHEME ON PREDICTION SKILL OF ENSO WITH A SIMPLE OCEAN-ATMOSPHERE COUPLED [J]. Journal of Tropical Meteorology, 2010, 16(1): 10-19.
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