Vertical structure of resonant gravity waves in the atmosphere

Details Vertical structure of resonant gravity waves in the atmosphere Vertical structure of resonant gravity waves in the atmosphere

Oct 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986ge%26ae..26..860g&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 26, Sept.-Oct. 1986, p. 860-862. In Russian.

Physics

Atmospheric Circulation, Gravity Waves, Internal Waves, Vertical Distribution, Winds Aloft, Harmonic Generations, Mesosphere, Resonant Frequencies, Troposphere, Wind Effects

Scientific paper

The vertical structure of resonant gravity waves is studied on the basis of the Iudin-Gavrilov (1985) numerical simulation algorithm, involving a harmonic source located at a height of 10 km in the troposphere. It is demonstrated that the background wind in the stratosphere and mesosphere produces changes in the horizontal phase velocity of the waves and in the energy of resonant IGW modes, as well as a change in their vertical structure.

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