Article Contents

PRELIMINARY ANALYSIS ON THE INTENSITY AND STRUCTURE OF TYPHOON MORAKOT (2009) DURING ITS LANDING PROCESS

Funding:

  • NCEP GFS (Global Forecast System) analytical data (available 4 times per day), satellite cloud image data and real-time observations of path and intensity of Typhoon Morakot are employed to investigate the variation of synoptic dynamics in its intensity and structure before and after the landing. This study intends to offer some hints for the forecast of intensity and structure of typhoons. Results show that in the tangential direction, the averaged asymmetry amplitude of wind on the radius of a large-value center of the low-level wind can be used as an important parameter for diagnosing the intensity of typhoons. Besides, the maximum of the upper dry potential vorticity in Morakot’s center tends to extend downward along the intensive gradient of tangential wind situated on the inner side of a large-value center of the low-level tangential wind. Additionally, the radial advection of the tangential wind determines the variation of tangential wind in conjunction with the vertical transmission of the tangential wind, the inertial centrifugal force and the Coriolis force. These four items are dominant in the motion equation of tangential wind based on a cylindrical coordinate without the effects of friction and turbulence. Moreover, the low-level convergence center of the typhoon has a tendency of shifting and developing along the intensive gradient of the tangential wind in the tangential direction.
  • [1] SHAPIRO L J, FRANKLIN J L. Potential vorticity in hurricane Gloria [J]. Mon. Wea. Rev., 1995, 123: 1465-1475.
    [2] MOLLER J D, SHAPIRO L J. Balanced contributions to the intensification of Hurricane Opal as diagnosed from a GFDL model forecast [J]. Mon. Wea. Rev., 2002, 130: 1866-1881.
    [3] CHEN Y S, YAU M K. Asymmetric Structure in a Simulated Landfalling Hurricane [J]. J. Atmos. Sci., 2003, 60: 2293-2312.
    [4] MALLEN K J, MONTGOMERY M T, WANG B. Reexamining the near-core radial structure of the tropical cyclone primary circulation: Implications for vortex resiliency [J]. J. Atmos. Sci., 2005, 62: 408-424.
    [5] STERN D P, NOLAN D S. Reexamining the vertical structure of tangential winds in tropical cyclones: Observations and theory [J]. J. Atmos. Sci., 2009, 66: 3579-3600.
    [6] XU J, WANG Y Q. Sensitivity of tropical cyclone inner-core size and intensity to the radial distribution of surface entropy flux [J]. J. Atmos. Sci., 2010, 67: 1831-1852.
    [7] WANG Y Q. How do outer spiral rainbands affect tropical cyclone structure and intensity [J]. J. Atmos. Sci., 2009, 66: 1250-1273.
    [8] WU L G, BRAUN S A. Effects of environmentally induced asymmetries on hurricane intensity: A numerical study [J]. J. Atmos. Sci., 2004, 61: 3065-3081.
    [9] XU Ya-mei, WU Rong-sheng. The numerical simulation of the genesis of tropical cyclone Bills (2000): The evolution and transformation of asymmetric momentum [J]. Chin. J. Atmos. Sci., 2005, 29(1): 79-80 (in Chinese).
    [10] HAN Ying, WU Rong-sheng. On the spiral structure of typhoon [J]. J. Nanjing Univ. (Nat. Sci.), 2007, 43(6): 572-580.
    [11] YU Jin-hua. Numerical study on vortex Rossby-waves propagation and typhoon tangential velocity changes [J]. J. Nanjing Inst. Meteor., 2003, 26(2): 172-179.
    [12] LI Jiang-nan, WU Guo-qiang, WANG Gang, et al. Numerical study of the inner-core structures and the mechanism for inshore strengthening during the landfalling of Typhoon Vongfong (2002) in the South China Sea [J]. J. Trop. Meteor., 2008, 24(5): 441-448 (in Chinese).
    [13] SHEN Xin-yong, MING Jie, FANG Ke. The properties of wave in typhoon and its numerical simulation [J]. J. Meteor. Sci., 2007, 27(2): 176-186.
    [14] LI Ying, QIAN Chuan-hai, CHEN Lian-shou. A study on the eyewall expansion of Typhoon Sepat (2009) during its landfall process [J]. Acta Meteor. Sinica, 2009, 67(5): 799-810 (in Chinese).
    [15] LIU Y, ZHANG D L, YAU M K. A multiscale numerical study of Hurricane Andrew (1992) Part II: Kinematics and inner core structures [J]. Mon. Wea. Rev., 1999, 147: 2597-2616.

Get Citation+

WANG Yong, DING Zhi-ying, LI Xun, et al. PRELIMINARY ANALYSIS ON THE INTENSITY AND STRUCTURE OF TYPHOON MORAKOT (2009) DURING ITS LANDING PROCESS [J]. Journal of Tropical Meteorology, 2014, 20(1): 35-44.
WANG Yong, DING Zhi-ying, LI Xun, et al. PRELIMINARY ANALYSIS ON THE INTENSITY AND STRUCTURE OF TYPHOON MORAKOT (2009) DURING ITS LANDING PROCESS [J]. Journal of Tropical Meteorology, 2014, 20(1): 35-44.
Export:  

Share Article

Manuscript History

Manuscript received: 04 March 2013
Manuscript revised: 15 January 2014
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

PRELIMINARY ANALYSIS ON THE INTENSITY AND STRUCTURE OF TYPHOON MORAKOT (2009) DURING ITS LANDING PROCESS

Abstract: NCEP GFS (Global Forecast System) analytical data (available 4 times per day), satellite cloud image data and real-time observations of path and intensity of Typhoon Morakot are employed to investigate the variation of synoptic dynamics in its intensity and structure before and after the landing. This study intends to offer some hints for the forecast of intensity and structure of typhoons. Results show that in the tangential direction, the averaged asymmetry amplitude of wind on the radius of a large-value center of the low-level wind can be used as an important parameter for diagnosing the intensity of typhoons. Besides, the maximum of the upper dry potential vorticity in Morakot’s center tends to extend downward along the intensive gradient of tangential wind situated on the inner side of a large-value center of the low-level tangential wind. Additionally, the radial advection of the tangential wind determines the variation of tangential wind in conjunction with the vertical transmission of the tangential wind, the inertial centrifugal force and the Coriolis force. These four items are dominant in the motion equation of tangential wind based on a cylindrical coordinate without the effects of friction and turbulence. Moreover, the low-level convergence center of the typhoon has a tendency of shifting and developing along the intensive gradient of the tangential wind in the tangential direction.

WANG Yong, DING Zhi-ying, LI Xun, et al. PRELIMINARY ANALYSIS ON THE INTENSITY AND STRUCTURE OF TYPHOON MORAKOT (2009) DURING ITS LANDING PROCESS [J]. Journal of Tropical Meteorology, 2014, 20(1): 35-44.
Citation: WANG Yong, DING Zhi-ying, LI Xun, et al. PRELIMINARY ANALYSIS ON THE INTENSITY AND STRUCTURE OF TYPHOON MORAKOT (2009) DURING ITS LANDING PROCESS [J]. Journal of Tropical Meteorology, 2014, 20(1): 35-44.
Reference (15)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return