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NUMERICAL EXPERIMENTS ON THE IMPACTS OF SEA SPRAY ON TROPICAL CYCLONES

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  • The latest version of sea spray flux parameterization scheme developed by Andreas is coupled with the PSU/NCAR model MM5 in this paper. A western Pacific tropical cyclone named Nabi in 2005 is simulated using this coupled air-sea spray modeling system to study the impacts of sea spray evaporation on the evolution of tropical cyclones. The results demonstrate that sea spray can lead to a significant increase of heat fluxes in the air-sea interface, especially the latent heat flux, the maximum of which can increase by up to about 35% - 80% The latent heat flux seems to be more important than the sensible heat flux for the evolution of tropical cyclones. Regardless of whether sea spray fluxes have been considered, the model can always simulate the track of Nabi well, which seems to indicate that sea spray has little impact on the movement of tropical cyclones. However, with sea spray fluxes taken into account in the model, the intensity of a simulated tropical cyclone can have significant increase. Due to the enhancement of water vapor and heat from the sea surface to the air caused by sea spray, the warm core structure is better-defined, the minimum sea level pressure decreases and the vertical speed is stronger around the eye in the experiments, which is propitious to the development and evolution of tropical cyclones.
  • [1] ANDREAS E L, EDSON J B, MONAHAN E C, et al. Thespray contribution to net evaporation from the sea: A review ofrecent progress [J]. Bound. Layer Meter, 1995, 72: 3-52.
    [2] ANDREAS E L, EMANUEL K A. Effects of sea spray ontropical cyclone intensity [J]. J. Atmos. Sci., 2001, 58: 3 741-3751.
    [3] LI W, PERRIE W, ANDREAS E L, et al. Impact of seaspray on numerical simulation of extratropical hurricanes[C/DK]. Preprints, 12th Conference on Interactions of the Seaand Atmosphere, Long Beach: Am. Meteor. Soc., 2003,CD-ROM 2.5: 9.
    [4] PERRIE W, ANDREAS E L, ZHANG W, et al. Sea sprayimpacts on intensifying midlatitude cyclones [J]. J. Atmos. Sci.,2005, 62: 1867-1883.
    [5] WANG Yu-qing, KEPERT J D, HOLLAND G J. Theimpact of sea spray evaporation on tropical cyclone boundarylayer structure and intensity [J]. Mon. Wea. Rev., 2001, 129:2481-2500.
    [6] BAO J W, WILCZAK J M, CHOI J K, et al. Numericalsimulation of air-sea interaction under high wind conditionsusing a coupled model: a study of hurricane development [J].Mon. Wea. Rev., 2000, 128: 2190-2209.
    [7] FAIRALL C W, KEPERT J D, HOLLAND G J. The effectof sea spray on the surface energy transports over the ocean [J].The Global Atmos. and Ocean Sys., 1994, 2: 121-142.
    [8] FAIRALL C W, BRADLEY E F, ROGERS D P, et al.Bulk parameterization of air-sea fluxes for TropicalOcean-Global Atmosphere Coupled-Ocean AtmosphereResponse Experiment [J]. J. Geophys. Res., 1996, 101:3747-3764.
    [9] ANDREAS E L. Sea spray and the turbulent air-sea heatfluxes [J]. J. Geophys. Res., 1992, 97: 11429-11441.
    [10] ANDREAS E L. The temperature of evaporating seaspray droplets [J]. J. Atmos. Sci., 1995, 52: 852-862.
    [11] ANDREAS E L, DECOSMO J. Sea spray production andinfluence on air-sea heat and moisture fluxes over the openocean [M]// GEERNAERT G, Air-Sea Exchange: Physics,Chemistry and Dynamics, Kluwer, Dordrecht, 1999: 327-362.
    [12] ANDREAS E L, DECOSMO J. The signature of sea sprayin the HEXOS turbulent heat flux data [J]. Bound. LayerMeteor., 2002, 103: 303-333.
    [13] ANDREAS E L. An algorithm to predict the turbulentair-sea fluxes in high-wind, spray conditions [C/DK].Preprints, 12th Conference on Interactions of the Sea andAtmosphere, Long Beach: Am. Meteor. Soc., 9-13, Feb., 2003,CD-ROM 3.4: 7.
    [14] ANDREAS E L. Spray stress revisited [J]. J. Phys.Oceanogr., 2004, 34: 1429-1440.
    [15] ANDREAS E L. A bulk air-sea flux algorithm forhigh-wind, spray conditions, Version 2.0 [C/DK]. Preprints,13th Conference on Interactions of the Sea and Atmosphere,Portland: Am. Meteor. Soc., 9-13 August 2004, CD-ROM P1.5:8.
    [16] ANDREAS E L. Approximation formulas for themicrophysical properties of saline droplets [J]. Am. MeteorSoc, 2005, 75: 323-345.
    [17] ANDREAS E L, WANG S. Predicting signature waveheight off the northeast coast of the United States [C/DK].Preprints, 14th Conf on Interaction of the Sea and Atmosphere,Atlanta: Am. Meteor. Soc., 29 Jan. - 2 Feb., 2006, CD-ROMP4.1: 8.
    [18] LI Wei-biao. Modeling air-sea fluxes during a westernPacific typhoon: Role of sea spray [J]. Adv. Atmos. Sci., 2004,21(2): 269-276.
    [19] LI Wei-biao, HE Xi-cheng, TANG Jie. Numericalsimulation of typhoon “Sinlaku”: Roles of sea spray [J]. J.Trop. Oceanogr., 2004, 23(3): 58-65.
    [20] PERSSON P O G, HARE J E, FAIRALL C W, et al.Air-sea interaction processes in warm and cold sectors ofextratropical cyclonic storms observed during FASTEX [J].Quart. J. Roy. Meteor. Soc., 2005, 131: 877-912.
    [21] HUANG Xiao-gang, FEI Jian-fang, LU Han-cheng. Acontrast test of the methods to remove the analyzed typhoon [J].J. Appl. Meteor. Sci., 2006, 17(1): 81-86.

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ZHENG Jing, FEI Jian-fang, WANG Yuan, et al. NUMERICAL EXPERIMENTS ON THE IMPACTS OF SEA SPRAY ON TROPICAL CYCLONES [J]. Journal of Tropical Meteorology, 2009, 15(1): 54-58.
ZHENG Jing, FEI Jian-fang, WANG Yuan, et al. NUMERICAL EXPERIMENTS ON THE IMPACTS OF SEA SPRAY ON TROPICAL CYCLONES [J]. Journal of Tropical Meteorology, 2009, 15(1): 54-58.
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NUMERICAL EXPERIMENTS ON THE IMPACTS OF SEA SPRAY ON TROPICAL CYCLONES

Abstract: The latest version of sea spray flux parameterization scheme developed by Andreas is coupled with the PSU/NCAR model MM5 in this paper. A western Pacific tropical cyclone named Nabi in 2005 is simulated using this coupled air-sea spray modeling system to study the impacts of sea spray evaporation on the evolution of tropical cyclones. The results demonstrate that sea spray can lead to a significant increase of heat fluxes in the air-sea interface, especially the latent heat flux, the maximum of which can increase by up to about 35% - 80% The latent heat flux seems to be more important than the sensible heat flux for the evolution of tropical cyclones. Regardless of whether sea spray fluxes have been considered, the model can always simulate the track of Nabi well, which seems to indicate that sea spray has little impact on the movement of tropical cyclones. However, with sea spray fluxes taken into account in the model, the intensity of a simulated tropical cyclone can have significant increase. Due to the enhancement of water vapor and heat from the sea surface to the air caused by sea spray, the warm core structure is better-defined, the minimum sea level pressure decreases and the vertical speed is stronger around the eye in the experiments, which is propitious to the development and evolution of tropical cyclones.

ZHENG Jing, FEI Jian-fang, WANG Yuan, et al. NUMERICAL EXPERIMENTS ON THE IMPACTS OF SEA SPRAY ON TROPICAL CYCLONES [J]. Journal of Tropical Meteorology, 2009, 15(1): 54-58.
Citation: ZHENG Jing, FEI Jian-fang, WANG Yuan, et al. NUMERICAL EXPERIMENTS ON THE IMPACTS OF SEA SPRAY ON TROPICAL CYCLONES [J]. Journal of Tropical Meteorology, 2009, 15(1): 54-58.
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