Estimation of the intensity of sources of wave motions according to meteorological data

Details Estimation of the intensity of sources of wave motions according to meteorological data Estimation of the intensity of sources of wave motions according to meteorological data

Jun 1984

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1984ge%26ae..24..510g&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 24, May-June 1984, p. 510-512. In Russian.

Mathematics

Logic

Airglow, Gravity Waves, Meteorological Charts, Meteorological Parameters, Oxygen Spectra, Tropospheric Waves, Atmospheric Pressure, Atmospheric Temperature, Internal Waves, Wind Measurement

Scientific paper

A general expression for the intensity (Phi) of sources of wave motions during the adaptation of meteorological fields to a state of quasi-geostrophic equilibrium was derived previously (Gavrilov, 1982, 1983). The present paper proposes a simple method for estimating values of Phi which are averaged over the entire depth of the atmosphere on the basis of measurements of surface pressure, temperature, and wind. As an example, attention is given to the use of averaged-intensity maps to interpret internal-gravity-wave observations in the lower thermosphere from measurements of intensity variations of the 5577-A oxygen line.

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