A study on the Responsibility of the Atmospheric Numerical Model on Turbulence induced by Orography

대기환경모형에 대한 지형성 난류의 의존성에 관한 연구

  • Lee Soon-Hwan (Japan Atomic Energy Research Institute) ;
  • Lee Hwa-Woon (Department of Atmospheric Science, Pusan National University) ;
  • Kim Yoo-Keun (Department of Atmospheric Science, Pusan National University)
  • Published : 1999.12.01

Abstract

The flow of non-rotation atmosphere with uniform stratification and wind past an isolated three dimensional topography obstacle is investigated with three-dimensional hydrostatic and non- hydrostatic numerical model. The characteristic of turbulence created the back of topography obstacle is usually defined by Froude number which is the function of upstream wind speed, the height of topography obstacle, and atmospheric stability. Turbulence tends to be formed more easily at the non-hydrostatic model than hydrostatic model. Especially, the difference between flow patterns of two models generated by isolated obstacle is more clear under low Froude number. The difference of flow patterns can be only seen at relatively low altitude, but at high altitude the patterns of two models are almost same. In this research, wind velocity in the parameters related with Froude number have great sensitivity at responsibility of numerical models. and slop of obstacle is also important factor at the flow pattern regardless of the species of numerical model

Keywords

References

  1. J. Atmos. Sci. v.38 The quasi-hydrostatic approximation Oranski, I.
  2. Mon. Wea. Rev. v.111 A compressible model for the simulation of moisture mountain wave Durran, D.;J. Klemp
  3. J. Geophys. Res. v.99 Gravity-wave breaking in two and three dimensions. part2: Three-dimensional evolution and instability structure Fritts, D.C.;J.R. Isler;O. Andreassen
  4. J. Atmos. Sci. v.45 Numerical study of orographic-convective precipitation over the eastern Arabian sea and the Grat mountains during the summer monsoon Ogura, Y.;M. Yoshizaki
  5. Bound. Lay. Meteor. v.44 Blocking in periodic valleys Kimura, F.;P. Manins
  6. Meso-Scale Atmospheric Circulations Atkison, B.W.
  7. Advances in Geophysics v.16 Atmospheric and oceanic flow problems introduced by islands Chopra, K.P.
  8. J. Atmos. Sci. v.22 Mesoscale eddies in wakes of islands Chopra, K.P.;L.F. Hubert
  9. J. Atmos. Sci. v.46 Low Froude number flow past three dimensional obstacles. Part I: Baroclinically generated lee vortices Smolarkiewicz, P.K.;R. Routuno
  10. Tellus v.45A Stagnation points and bifurcation in 3-D mountain airflow Smith, R.B.;S. Gronas
  11. Ann. Meteor. v.30 High resolution of low-level flow features in the Alpine region Aebischer, U.;C. Schar
  12. J. Atmos. Sci. v.53 Nonlinear flow past an elliptic mountain ridge Olafasson, H.;P. Bougeault
  13. J. Meteor. Soc. Japan v.66 Comparison of some schemes for nonhydroststic model with orography Iwasaki, M.
  14. J. Meteor. Soc. Japan v.59 A numerical experiment of the nocturnal low level jet over Kanto plain Kimura, F.;S. Arakawa
  15. Numerical studies on the impacts of topography and heterogeneous surface moisture estimated by satellite data on the local circulations Lee, S H