Articles | Volume 15, issue 9
Ann. Geophys., 15, 1187–1197, 1997
https://doi.org/10.1007/s00585-997-1187-7

Special issue: Wind Measurements

Ann. Geophys., 15, 1187–1197, 1997
https://doi.org/10.1007/s00585-997-1187-7

  30 Sep 1997

30 Sep 1997

SMLTM simulations of the diurnal tide: comparison with UARS observations

R. A. Akmaev1, V. A. Yudin2, and D. A. Ortland3 R. A. Akmaev et al.
  • 1Department of Aerospace Engineering Sciences, Campus Box 429, University of Colorado, Boulder, CO 80309-0429, USA
  • 2Institute for Terrestrial and Planetary Atmospheres, State University of New York at Stony Brook, Stony Brook, NY 11794-5000, USA
  • 3Space Physics Research Laboratory, University of Michigan, 2455 Hayward Street, Ann Arbor, MI 48109-2143, USA

Abstract. Wind and temperature observations in the mesosphere and lower thermosphere (MLT) from the Upper Atmosphere Research Satellite (UARS) reveal strong seasonal variations of tides, a dominant component of the MLT dynamics. Simulations with the Spectral mesosphere/lower thermosphere model (SMLTM) for equinox and solstice conditions are presented and compared with the observations. The diurnal tide is generated by forcing specified at the model lower boundary and by in situ absorption of solar radiation. The model incorporates realistic parameterizations of physical processes including various dissipation processes important for propagation of tidal waves in the MLT. A discrete multi-component gravity-wave parameterization has been modified to account for seasonal variations of the background temperature. Eddy diffusion is calculated depending on the gravity-wave energy deposition rate and stability of the background flow. It is shown that seasonal variations of the diurnal-tide amplitudes are consistent with observed variations of gravity-wave sources in the lower atmosphere.

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