Height-latitude structure of the vertical component of the migrating semidiurnal tide in the upper mesosphere and lower thermosphere region (80

Height-latitude structure of the vertical component of the migrating semidiurnal tide in the upper mesosphere and lower thermosphere region (80–100 km)

Published:2011-02 Issue:1 Volume:47 Page:108-118
ISSN:0001-4338
Container-title:Izvestiya, Atmospheric and Oceanic Physics
language:en
Short-container-title:Izv. Atmos. Ocean. Phys.

Author:

Portnyagin Yu. I.,Merzlyakov E. G.,Solov’eva T. V.,Pogorel’tsev A. I.,Suvorova E. V.,Mukhtarov P.,Pancheva D.

Publisher

Pleiades Publishing Ltd

Subject

Atmospheric Science,Oceanography

Link

http://link.springer.com/content/pdf/10.1134/S0001433811010117.pdf

Reference19 articles.

1. Yu. I. Portnyagin and T. V. Solovjova, “Empirical Semidiurnal Tide Model for the Upper Mesosphere/Lower Thermosphere,” Adv. Space Res. 31(6), 811–815 (1998).

2. Ch. Jacobi, Yu. I. Portnyagin, T. V. Solovjova, et al., “Climatology of the Semidiurnal Tide at 52–56° N from Ground-Based Radar Wind Measurements 1985–1995,” J. Atm. Sol.-Terr. Phys. 61(13), 975–991 (1999).

3. Y. I. Portnyagin, T. V. Solovjova, N. A. Makarov, et al., “Monthly Mean Climatology of the Prevailing Winds and Tides in the Arctic Mesosphere/Lower Thermosphere,” Ann. Geophys. 22(10), 3395–3410 (2004).

4. M. J. Miller, T. N. Palmer, and R. Swinbank, “Parameterization and Influence of Subgridscale Orography in General Circulation and Weather Prediction Models,” Meteorol. Atmos. Phys. 40(8–11), 84–109 (1989).

5. D. Marsh and R. Roble, “TIME-GSM Simulations of Lower-Thermosphere Nitric Oxide Seen by the Halogen Occultation Experiment,” J. Atm. Sol.-Terr. Phys. 64(8–11), 889–895 (2002).

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