Numerical Study on the Formation and Maintenance Mechanisms of Cloud Street in the East Sea during Cold Air Outbreak

Kang, Sung-Dae;Ahn, Joong-Bae

  • Published : 2008.04.10

Abstract

The formation and maintenance mechanisms of cloud strets in the East Sea of the Korean Peninsula are studied using MM5 (ver. 3.7) with real topography, NCEP reanalysis data, and weekly OISST (Optimum Interpolation of Sea Surface Temperature). Well-organized cloud streets are simulated in to the numerical results, the formation mechanisms of cloud strets and their maintenance mechanisms are found to be different depending on their downstream distance from Baekdu Mountain. Specifically, the following seven results have been obtained. For the formation of the cloud strets at both regions: (1) both strong static instability and topographically induced mechanical disturbances are important for the formation of cloud streets near the coastal line. However, the cloud streets observed far from the coastal line can be formed only under strong static instability; (2) the strong heat fluxes (sensible and latent heat) from warm ocean surface are the main source of the formation of stratus clouds near the coastal line; (3) the buoyancy caused by the condensation process in the cloud is the main source of the convective rolls at far regions from the coastal line; (4) the positive SST forcing (which corresponds to the approaching Kuroshio Curent) enhan-ces the formation of the thin cloud streets, and negative SST-forcing generates the thick cloud streets at the far region disturbance is the main source keeping the long line-shaped cloud streets near the coastal line; (6) both vertical difusion of moisture from warm ocean surface and release of latent heat in the cloud are the main sources at the far region from the coastal line, and; (7) the radiative coling in the cloud is negligibly small at the entire region.

Keywords

References

  1. Dudhia, J., 1989: Numerical study of convection observed during the winter Monsoon experiment using a mesoscale two-dimensional model. J. Atmos. Sci., 46, 3077-3107 https://doi.org/10.1175/1520-0469(1989)046<3077:NSOCOD>2.0.CO;2
  2. Grell, G. A., J. Dudhia, and D. R. Stauffer, 1993: A description of the fifth generation Penn State/NCAR mesoscale model. NCAR Tech. Note, 398+IA, 122pp.
  3. Hong, S. Y., and H. L. Pan, 1996: Nonlocal boundary layer vertical diffusion in a medium-range forecast model. Mon. Wea. Rev., 124, 2322-2339 https://doi.org/10.1175/1520-0493(1996)124<2322:NBLVDI>2.0.CO;2
  4. Kang, S.-D., and F. Kimura, 1997: A numerical study on the mechanism of cloud-street formation in the lee of an isolated mountain near a coast. J. Meteor. Soc. Japan, 75, 955-968 https://doi.org/10.2151/jmsj1965.75.5_955
  5. Kondo, J., 1976: Heat balance of the East China Sea during the air-mass transformation experiment. J. Meteor. Soc. Japan, 54, 382-393 https://doi.org/10.2151/jmsj1965.54.6_382
  6. Nagata, M., 1993: Meso-beta-scale vortices developing along the Japan-Sea polar-airmass convergence zone cloud: Numerical simulation. J. Meteor. Soc. Japan, 71, 43-57 https://doi.org/10.2151/jmsj1965.71.1_43
  7. Ninomiya, K., 1968: Heat and water budget over the Japan Sea and the Japan Islands in winter season. J. Meteor. Soc. Japan, 46, 343-372 https://doi.org/10.2151/jmsj1965.46.5_343
  8. Ninomiya, K., 1972: Heat and water vapor budget over the East China Sea in the winter season. J. Meteor. Soc. Japan, 50, 1-17 https://doi.org/10.2151/jmsj1965.50.1_1
  9. Ninomiya, K., 1975: Large-scale aspects of air-mass transformation over the East China Sea during AMTEX74. J. Meteor. Soc. Japan, 53, 285-303 https://doi.org/10.2151/jmsj1965.53.5_285
  10. Ninomiya, K., 1977: Heat budget of polar airmass transformed over Kuroshio region under the situation of strong subsidence. J. Meteor. Soc. Japan, 55, 431-441 https://doi.org/10.2151/jmsj1965.55.4_431
  11. Ninomiya, K., 1989: Polar/comma-cloud lows over the Japan Sea and the Northwestern Pacific in winter. J. Meteor. Soc. Japan, 67, 83-97 https://doi.org/10.2151/jmsj1965.67.1_83
  12. Ninomiya, K., and T. Akiyama, 1976: Structure and heat energy budget of mixed layer capped by inversion during the period of polar outbreak over Kuroshio. J. Meteor. Soc. Japan, 54, 160-174 https://doi.org/10.2151/jmsj1965.54.3_160
  13. Ninomiya, K., and K. Hoshino, 1990: Evolution process and multi- scale structure of a polar low developed over the Japan Sea on 11-12 December 1989. Part 2. J. Meteor. Soc. Japan, 68, 307-318 https://doi.org/10.2151/jmsj1965.68.3_307
  14. Ninomiya, K., and T. Nishimura, T. Suzuki, and S. Matsumura, 2006: Polar-Air Outbreak and Air-Mass Transformation over the East Coast of Asia as Simulated by an AGCM, J. Meteor. Soc. Japan, 84, 47-68 https://doi.org/10.2151/jmsj.84.47
  15. Nitta, T., 1976: Large-scale heat and moisture budget during the Air-Mass Transformation Experiment. J. Meteor. Soc. Japan, 54, 1-14 https://doi.org/10.2151/jmsj1965.54.1_1
  16. Nitta, T., and S. S. So, 1980: Structure and heat, moisture and momentum budgets of a convective mixing layer during AMTEX75. J. Meteor. Soc. Japan, 58, 378-393 https://doi.org/10.2151/jmsj1965.58.5_378
  17. Yamagishi, Y., 1980: Some characteristics of the stable layer over the Japan Sea during winter season. Tenki, 27, 322-329.(in Japanese)
  18. Yoshizaki, M., T. Kato., H. Eito, S. Hayashi, and W.-K. Tao, 2004: An overview of the field experiment "Winter Mesoscale Convective Systems over the Japan Sea in 2001", and comparisons of the cold-air outbreak case (14 January) between analysis and a nonhydrostatic cloud-resolving model. J. Meteor. Soc. Japan, 82, 1365-1387 https://doi.org/10.2151/jmsj.2004.1365