An Efficient Solution Method for the Buoyancy Wave Equation at Variable Wind and Temperature

Rein Rõõm Tartu University, Tartu, Estonia

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Marko Zirk Tartu University, Tartu, Estonia

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Abstract

To solve a horizontally spectral, vertically discrete buoyancy wave equation in conditions of arbitrary wind and temperature distribution with height, a novel method is applied, which consists of a presentation of the solution in the form of a cumulative product of complex decrease factors. For decrease factors, a nonlinear, inhomogeneous, two-member recurrence formula follows that is initiated, assuming the radiative condition at the top. Singularities of the wave equation, corresponding to a critical layer in the vicinity of evanescent wind, are eliminated by turbulent friction. The estimation of minimal vertical resolution is derived, enabling solution stability and accuracy. The areas of application of the developed numerical scheme are the high-precision modeling of orographic waves for arbitrary orography in general atmospheric stratification conditions and testing of adiabatic kernels of numerical weather prediction models.

Corresponding author address: Rein Rõõm, Institute of Environmental Physics, Tartu University, Ülikooli 18, Tartu 50090, Estonia. Email: rein.room@ut.ee

Abstract

To solve a horizontally spectral, vertically discrete buoyancy wave equation in conditions of arbitrary wind and temperature distribution with height, a novel method is applied, which consists of a presentation of the solution in the form of a cumulative product of complex decrease factors. For decrease factors, a nonlinear, inhomogeneous, two-member recurrence formula follows that is initiated, assuming the radiative condition at the top. Singularities of the wave equation, corresponding to a critical layer in the vicinity of evanescent wind, are eliminated by turbulent friction. The estimation of minimal vertical resolution is derived, enabling solution stability and accuracy. The areas of application of the developed numerical scheme are the high-precision modeling of orographic waves for arbitrary orography in general atmospheric stratification conditions and testing of adiabatic kernels of numerical weather prediction models.

Corresponding author address: Rein Rõõm, Institute of Environmental Physics, Tartu University, Ülikooli 18, Tartu 50090, Estonia. Email: rein.room@ut.ee

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  • Baines, P. G., 1995: Topographic Effects in Stratified Flows. Cambridge University Press, 482 pp.

  • Broutman, D., J. W. Rottman, and S. D. Eckermann, 2003: A simplified Fourier method for nonhydrostatic mountain waves. J. Atmos. Sci., 60 , 26862696.

    • Search Google Scholar
    • Export Citation
  • Eliassen, A., 1968: On the meso-scale mountain waves on the rotating Earth. Geofys. Publ., 27 , (6). 115.

  • Grubiŝić, V., and P. K. Smolarkiewicz, 1997: The effect of critical levels on 3D orographic flows: Linear regime. J. Atmos. Sci., 54 , 19431960.

    • Search Google Scholar
    • Export Citation
  • Hazel, P., 1967: The effect of viscosity and heat conduction on internal gravity waves at a critical level. J. Fluid Mech., 30 , 775783.

    • Search Google Scholar
    • Export Citation
  • Jones, W. L., 1967: Propagation of internal gravity waves in fluids with shear flow and rotation. J. Fluid Mech., 30 , 439488.

  • Lin, C. C., 1955: The Theory of Hydrodynamic Stability. Cambridge University Press, 155 pp.

  • Miller, M. J., 1974: On the use of pressure as vertical co-ordinate in modelling convection. Quart. J. Roy. Meteor. Soc., 100 , 155162.

    • Search Google Scholar
    • Export Citation
  • Miller, M. J., and R. P. Pearce, 1974: A three-dimensional primitive equation model of cumulonimbus convection. Quart. J. Roy. Meteor. Soc., 100 , 133154.

    • Search Google Scholar
    • Export Citation
  • Miller, M. J., and A. A. White, 1984: On the nonhydrostatic equations in pressure and sigma coordinates. Quart. J. Roy. Meteor. Soc., 110 , 515533.

    • Search Google Scholar
    • Export Citation
  • Miranda, P. M. A., and M. A. Valente, 1997: Critical level resonance in three-dimensional flow past isolated mountains. J. Atmos. Sci., 54 , 15741588.

    • Search Google Scholar
    • Export Citation
  • Queney, P., 1948: The problem of airflow over mountains. A summary of theoretical studies. Bull. Amer. Meteor. Soc., 29 , 1626.

  • Rõõm, R., 1998: Acoustic filtering in nonhydrostatic pressure-coordinate dynamics: A variational approach. J. Atmos. Sci., 55 , 654668.

    • Search Google Scholar
    • Export Citation
  • Rõõm, R., and A. Männik, 1999: Response of different nonhydrostatic, pressure-coordinate models to orographic forcing. J. Atmos. Sci., 56 , 25532578.

    • Search Google Scholar
    • Export Citation
  • Scorer, R. S., 1949: Theory of waves in the lee of mountains. Quart. J. Roy. Meteor. Soc., 75 , 4156.

  • Shen, B-W., and Y-L. Lin, 1999: Effects of critical levels on two-dimensional back-sheared flow over an isolated mountain ridge. J. Atmos. Sci., 56 , 32863302.

    • Search Google Scholar
    • Export Citation
  • Shutts, G. J., 1998: Stationary gravity wave structure in flows with directional wind shear. Quart. J. Roy. Meteor. Soc., 124 , 14211442.

    • Search Google Scholar
    • Export Citation
  • Shutts, G. J., 2003: Inertia-gravity wave and neutral Eady wave trains forced by directionally sheared flow over isolated hills. J. Atmos. Sci., 60 , 593606.

    • Search Google Scholar
    • Export Citation
  • Shutts, G. J., and A. Gadian, 1999: Numerical simulations of orographic gravity waves in flows which back with height. Quart. J. Roy. Meteor. Soc., 125 , 27432765.

    • Search Google Scholar
    • Export Citation
  • Smith, R. B., 1980: Linear theory of stratified hydrostatic flows past an isolated mountain. Tellus, 32 , 348364.

  • Smith, R. B., S. Skubis, J. D. Doyle, A. Broad, C. Kiemle, and H. Volkert, 2002: Mountain waves over Mont Blanc: Influence of a stagnant boundary layer. J. Atmos. Sci., 59 , 20732092.

    • Search Google Scholar
    • Export Citation
  • White, A. A., 1989: An extended version of a nonhydrostatic, pressure coordinate model. Quart. J. Roy. Meteor. Soc., 115 , 12431251.

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