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비축대칭 3차원 모조 소용돌이를 이용한 열대저기압의 진로 및 강도예측

Tropical Cyclone Track and Intensity Forecast Using Asymmetric 3-Dimensional Bogus Vortex

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초록

The bogussing method was further developed by incorporating the asymmetriccomponent into the symmetric bogus tropical cyclone of the Structure Adjustable BalancedVortex (SABV). The asymmetric component is separated from the disturbance field associatedwith the tropical cyclone by establishing local polar coordinates whose center is the location ofthe tropical cyclone. The relative importance of wave components in azimuthal direction wasevaluated, and only two or three wave components with large amplitude are added to the symmetriccomponents. Using the Weather Research and Forecast model (WRF), initialized withthe asymmetric bogus vortex, the track and central pressure of tropical cyclones were predicted. Nine tropical cyclones, which passed over Korean peninsula during 2010~2012 wereselected to assess the effect of asymmetric components. Compared to the symmetric bogustropical cyclone, the track forecast error was reduced by about 18.9% and 17.4% for 48 hoursand 72 hours forecast, while the central pressure error was not improved significantly. Theresults suggest that the inclusion of asymmetric component is necessary to improve the trackforecast of tropical cyclones.

Abstract

The bogussing method was further developed by incorporating the asymmetriccomponent into the symmetric bogus tropical cyclone of the Structure Adjustable BalancedVortex (SABV). The asymmetric component is separated from the disturbance field associatedwith the tropical cyclone by establishing local polar coordinates whose center is the location ofthe tropical cyclone. The relative importance of wave components in azimuthal direction wasevaluated, and only two or three wave components with large amplitude are added to the symmetriccomponents. Using the Weather Research and Forecast model (WRF), initialized withthe asymmetric bogus vortex, the track and central pressure of tropical cyclones were predicted. Nine tropical cyclones, which passed over Korean peninsula during 2010~2012 wereselected to assess the effect of asymmetric components. Compared to the symmetric bogustropical cyclone, the track forecast error was reduced by about 18.9% and 17.4% for 48 hoursand 72 hours forecast, while the central pressure error was not improved significantly. Theresults suggest that the inclusion of asymmetric component is necessary to improve the trackforecast of tropical cyclones.

참고문헌 (33)

  1. Bender, M. A., "Improvements in tropical cyclone track and intensityfForecasts using the GFDL initialization system", Mon. Wea. Rev., 121, pp.2046~2061 (1993)
  2. Carr, L. E, "Objective diagnosis of binary tropical cyclone interactions for the western North Pacific Basin", Mon. Wea. Rev., 126, pp.1734~1740 (1998)
  3. Chan, J. C. L., "Tropical cyclone movement and surrounding flow relationships", Mon. Wea. Rev., 110, pp.1354~1374 (1982)
  4. Chan, J. C. L., "Analytical and numerical studies of the beta-effect in tropical cyclone motion. Part I: Zero Mean flow", J. Atmos. Sci., 44, pp.1257~1265 (1987)
  5. Cheong, H. -B., "High-order harmonic spectral filter with the double Fourier series on a sphere", J. Comput. Phys., 177, pp.313~335 (2002)
  6. Cheong, H. -B., "Further study on the high-order double Fourier series spectral filtering on a sphere", J. Comput. Phys., 193, pp.180~197 (2004)
  7. 정형빈, "Tropical Cyclone Track and Intensity Prediction with a Structure Adjustable Balanced Vortex", 한국기상학회지, 47(3), pp.293~303 (2011), 한국기상학회
  8. Fiorino, M., "Some aspects of vortex structure related to tropical cyclone motion", J. Atmos. Sci., 46, pp.975~990 (1989)
  9. Frank, W. M., "Effects on environmental flow upon tropical cyclone structure", Mon. Wea. Rev., 127, pp.2044~2061 (1999)
  10. Frank, W. M., "Effects of vertical wind shear on hurricane intensity and structure", Mon. Wea. Rev., 129, pp.2249~2269 (2001)
  11. Fujiwara, S., "The natural tendency towards symmetry of motion and its application as a principle in meteorology", Quart. J. Roy. Meteor. Soc., 47, pp.287~293 (1921)
  12. Gray, W. M., "The formation of tropical cyclones", Meteor. Atmos. Phys., 67, pp.37~69 (1998)
  13. 홍성유, "The WRF Single-Moment 6-Class Microphysics Scheme (WSM6)", 한국기상학회지, 42(2), pp.129~151 (2006), 한국기상학회
  14. Hong, S. -Y., "A new vertical diffusion package with an explicit treatment of entrainment processes", Mon. Wea. Rev., 134, pp.2318~2341 (2006)
  15. Kain, J. S., "The Kain-Fritsch convective parameterization:An update", J. Appl. Meteor., 43, pp.170~181 (2004)
  16. Kang, M. -K., "Oscillation of separation distance between paired typhoon-scale vortices", J. Meteor. Soc. Japan, 79, pp.967~983 (2001)
  17. Kim, S. -H., "Beta gyres in global analysis fields", Adv. Atmos. Sci., 26, pp.984~994 (2009)
  18. Kurihara, Y., "An initialization scheme of hurricane models by vortex specification", Mon. Wea. Rev., 121, pp.2030~2045 (1993)
  19. Kwon, I. -H., "Tropical cyclone initialization with a spherical high-order filter and an idealized three-dimensional bogus vortex", Mon. Wea. Rev., 138, pp.1344~1367 (2010)
  20. Lewis J., "A dynamical method for building continuity into the deep layer mean", Mon. Wea. Rev., 115, pp.885~893 (1987)
  21. Möller, J. D., "Vortex Rossby waves and hurricane intensification in barotropic model", J. Atmos. Sci., 56, pp.1674~1687 (1999)
  22. Maclay, K. S., "Tropical cyclone inner-core kinetic energy evolution", Mon. Wea. Rev., 136, pp.4882~4898 (2008)
  23. Park, J. -R., "Highorder spectral filter for the spherical-surface limited area", Mon. Wea. Rev., 139, pp.1256~1278 (2011)
  24. Peng, M. S., "A numerical study on tropical cyclone intensification. Part I: Beta effect and mean flow effect", J. Atmos. Sci., 56, pp.1404~1423 (1999)
  25. Reeder, M. J., "The detection of flow asymmetries in the tropical cyclone environment", Mon. Wea. Rev., 119, pp.848~855 (1991)
  26. "A description of the advanced research WRF version 3. NCAR Tech. Note, NCAR/TN-475+STR" (2008)[URL]
  27. Ueno, M., "A study on the impact of asymmetric components around tropical cyclone center on the accuracy of bogus data and the track forecast", Quart. J. Roy. Meteor. Soc, 47, pp.287~292 (1995)
  28. Thomas J. Galarneau Jr., "Diagnosing forecast errors in tropical cyclone motion", Mon. Wea. Rev., 141, pp.405~430 (2013)
  29. Wang, Y., "Vortex rossby waves in a numerically simulated tropical cyclone. Part I: Overall structure, potential vorticity, and kinetic energy budgets*", J. Atmos. Sci., 59, pp.1213~1238 (2002)
  30. Wang, Y., "Vortex rossby waves in a numerically simulated tropical cyclone. Part II: The role in tropical cyclone structure and intensity changes*", J. Atmos. Sci., 59, pp.1239~1262 (2002)
  31. Williams, R. T., "Numerical studies of the beta effect in tropical cyclone motion. Part II: Zonal mean flow effects", J. Atmos. Sci., 51, pp.1065~1076 (1994)
  32. Willoughby, H. E., "Nonlinear motion of a shallowwater barotropic vortex", J. Atmos. Sci., 51, pp.3722~3744 (1994)
  33. Zhong Zhong, "The Possible Mechanism on the Formation and Intensificationof the Maximum Wind Core in Tropical Cyclone", 한국기상학회지, 43(2), pp.185~194 (2007), 한국기상학회

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