Article Contents

USE OF A NEW STEERING FLOW METHOD TO PREDICT TROPICAL CYCLONE MOTION

Funding:

  • A tropical cyclone is a kind of violent weather system that takes place in warmer tropical oceans and spins rapidly around its center and at the same time moves along surrounding flows. It is generally recognized that the large-scale circulation plays a major role in determining the movement of tropical cyclones and the effects of steering flows are the highest priority in the forecasting of tropical cyclone motion and track. This article adopts a new method to derive the steering flow and select a typical swerving track case (typhoon Dan, coded 9914) to illustrate the validity of the method. The general approach is to modify the vorticity, geostropical vorticity and divergence, investigate the change in the non-divergent stream function, geoptential and velocity potential, respectively, and compute a modified velocity field to determine the steering flow. Unlike other methods in regular use such as weighted average of wind fields or geopoential height, this method has the least adverse effects on the environmental field and could derive a proper steering flow which fits well with storm motion. Combined with other internal and external forcings, this method could have wide application in the prediction of tropical cyclone track.
  • [1] WANG Bin, ELSBERRY R L, WANG Yu-qing, et al.Dynamics in TC Motion: A review [J]. Sci. Atmos. Sinica.1998, 22: 535-547.
    [2] CHEN Lian-shou, DING Yi-hui. An Introduction to theWestern Pacific Typhoons [M]. Beijing: Science Press, 1979:491pp.
    [3] CHAN J C L, GRAY W M. TC movement and surroundingflow relationship [J]. Mon. Wea. Rev., 1982, 110:1354-1374.
    [4] GEORGE J E, GRAY W M. TC motion and surroundingparameter relationships [J]. J. Appl. Meteor., 1976, 15:1252-1264.
    [5] BRAND S, BUENAFE C A, HAMILTON H D.Comparison of TC motion and environmental steering [J].Mon. Wea. Rev., 1981, 109: 908-909
    [6] NEUMANN C J. On the use of deep-layer meangeopotential height fields in statistical prediction of TC motion[J]. 6th Conf. On Probability and Statistics in AtmosphericScience, Banff Alta: Amer. Meteor. Soc., 1979: 32-38.
    [7] KURIHARA Y, BENDER M A, ROSS R. An initializationscheme of hurricane models by vortex specification [J]. Mon.Wea. Rev., 1993, 121: 2030-2045.
    [8] DAVIS C A, LOWNAM S. The NCAR-AFWA TCBogussing Scheme [R]. A Report Prepared for the Air ForceWeather Agency (AFWA), 2001.
    [9] DING Yi-hui. The Diagnostic and Analysis Method inSynoptic Dynamics [M]. Beijing: Science Press, 1989: 293pp.
    [10] CHAN J C L. Definition of the steering flow for TCmotion [C]// Porc. 15th Conf. on Hurricanes and TropicalMeteorology, Boston: Amer. Meteor. Soc, 1984: 559-566.
    [11] VELDEN C S. The relationship between TC motion,intensity, and the vertical extent of the environmental steeringlayer in the Atlantic basin [C]// Preprints, 20th Conf. onHurricanes and Tropical Meteorology, Boston: Amer. Meteor.Soc., 1993: 31-34.
    [12] BELL G J, LAM C Y. Departures of TC movement fromgeostrophic steering [C]// WMO Symposium on Typhoons,Shanghai, 1980: 110-115.
    [13] HOLLAND G J. TC motion: a comparison of theory andobservation [J]. J. Atmos. Sci., 1984, 41: 68-75.
    [14] KEGIN D, CHARLES J N. The relationship between TCmotion and environmental geostrophic flows [J]. Mon. Wea.Rev., 1986, 14: 155-122.
    [15] CHEN Lian-shou, XU Xiang-de, LUO Zhe-xian, et al.Introduction to TC dynamics [M]. Beijing: ChinaMeteorological Press, 2002: 317pp.
    [16] XU Xiang-de, CHEN Lian-shou, XIE Yi-yang, et al. Theasymmetric and dynamic structure of the ‘β-TOP’ diploe and‘ventilation flow’ of the target typhoon Flo during TCM-90field experiment [J]. Acta Meteor. Sinica, 1996, 54(5):536-542.
    [17] GAO S, ZHOU Y. Effects of diurnal variation of solarzenith angle on a tropical coupling system: A two-dimensionalcoupled ocean-cloud resolving atmosphere modeling study [J].Geophys. Res. Lett., 2008, 35, L15815,doi:10.1029/2008GL034340.
    [18] GAO S, ZHOU Y, LI X. Effects of diurnal variations ontropical equilibrium states: A two-dimensional cloud-resolvingmodeling study [J]. J. Atmos. Sci., 2007, 64(2): 656-664.
    [19] CHEN Lian-shou, LUO Zhe-xian. Some connectionbetween asymmetric structure and typhoon motion, Typhoonscience, operation and experiment, and research on weatherdynamics [M]. Beijing: China Meteorological Press, 1995,371-375.
    [20] ZHOU Yu-shu, CAO Jie, GAO Shou-ting. The method ofdecomposing wind field in a limited area and its application totyphoon SAOMEI [J]. Acta Phys. Sinica, 2008, 57(10):6654-6665.
    [21] CHAN J C, WILLIAMS K T. Analysis and numericalstudies of beta-effect in TC motion [J]. J. Atmos. Sci., 1987,44: 1257-1265.

Get Citation+

WANG Yong, DING Zhi-ying, LI Xun. USE OF A NEW STEERING FLOW METHOD TO PREDICT TROPICAL CYCLONE MOTION [J]. Journal of Tropical Meteorology, 2010, 16(2): 154-159.
WANG Yong, DING Zhi-ying, LI Xun. USE OF A NEW STEERING FLOW METHOD TO PREDICT TROPICAL CYCLONE MOTION [J]. Journal of Tropical Meteorology, 2010, 16(2): 154-159.
Export:  

Share Article

Manuscript History

通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

USE OF A NEW STEERING FLOW METHOD TO PREDICT TROPICAL CYCLONE MOTION

Abstract: A tropical cyclone is a kind of violent weather system that takes place in warmer tropical oceans and spins rapidly around its center and at the same time moves along surrounding flows. It is generally recognized that the large-scale circulation plays a major role in determining the movement of tropical cyclones and the effects of steering flows are the highest priority in the forecasting of tropical cyclone motion and track. This article adopts a new method to derive the steering flow and select a typical swerving track case (typhoon Dan, coded 9914) to illustrate the validity of the method. The general approach is to modify the vorticity, geostropical vorticity and divergence, investigate the change in the non-divergent stream function, geoptential and velocity potential, respectively, and compute a modified velocity field to determine the steering flow. Unlike other methods in regular use such as weighted average of wind fields or geopoential height, this method has the least adverse effects on the environmental field and could derive a proper steering flow which fits well with storm motion. Combined with other internal and external forcings, this method could have wide application in the prediction of tropical cyclone track.

WANG Yong, DING Zhi-ying, LI Xun. USE OF A NEW STEERING FLOW METHOD TO PREDICT TROPICAL CYCLONE MOTION [J]. Journal of Tropical Meteorology, 2010, 16(2): 154-159.
Citation: WANG Yong, DING Zhi-ying, LI Xun. USE OF A NEW STEERING FLOW METHOD TO PREDICT TROPICAL CYCLONE MOTION [J]. Journal of Tropical Meteorology, 2010, 16(2): 154-159.
Reference (21)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return