The saturated-cascade model for atmospheric gravity wave spectra, and the wavelength-period (W-P) relations

Details The saturated-cascade model for atmospheric gravity wave spectra, and the wavelength-period (W-P) relations The saturated-cascade model for atmospheric gravity wave spectra, and the wavelength-period (W-P) relations

May 1994

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994georl..21..817d&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 21, no. 9, p. 817-820

Physics

40

Atmospheric Turbulence, Earth Atmosphere, Gravity Waves, Internal Waves, Power Spectra, Mathematical Models, Optical Radar, Predictions, Tables (Data)

Scientific paper

The case will be presented for the hypothesis that over a certain wave
number range all the atmospheric gravity wave spectra (and the
Wavelength-Period Relations as well) are a direct consequence of a
'saturated-cascade' of the waves.

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