Scale-independent diffusive filtering theory of gravity wave spectra in the atmosphere

Research output: Chapter in Book/Report/Conference proceedingChapter

Abstract

Shear and convective instabilities, Doppler spreading and non-linear wave-wave interactions are mechanisms which have been proposed to explain the form of the gravity wave vertical wave number spectrum of horizontal winds. In this paper we present an alternative explanation by assuming that the damping effects of molecular viscosity, turbulence and off-resonance wave-wave interactions can all be characterized in terms of a scale-independent diffusivity (D) which increases with altitude. The components of the gravity wave source spectrum are assumed to grow exponentially with altitude in response to decreasing atmospheric density until they are removed by diffusive damping. A wave of intrinsic frequency ω and vertical wave number m is assumed to be completely damped when the effective vertical velocity of momentum diffusion (mD) exceeds the vertical phase velocity of the wave (ω/m). Only waves satisfying mD < ω/m, or equivalently m2D < ω and m < (ω/D)1/2 are permitted to grow in amplitude as they propagate upward in the atmosphere. If the gravity wave temporal spectrum varies as ω−P, we show that the vertical wave number spectrum must vary as m−2p+l and the zonal (or meridional) wave number spectrum must vary as k−(2p+ 1)/3. For p near 2, the diffusion theory predicts that the spectra are proportional to ω−2, m−3 and k−5/3. Because the joint (m, ω) intrinsic spectrum for scale-independent diffusive filtering is not separable, the theory predicts that the m-spectrum of vertical winds is proportional to m5-2p. The model spectra compare favorably with recent lidar and radar observations of middle atmosphere density, temperature and horizontal wind fluctuations.

Original languageEnglish (US)
Title of host publicationThe Upper Mesosphere and Lower Thermosphere
Subtitle of host publicationA Review of Experiment and Theory, 1995
EditorsR.M. Johnson, T.L. Killeen
PublisherBlackwell Publishing Ltd.
Pages153-175
Number of pages23
ISBN (Electronic)9781118664247
ISBN (Print)9780875900445
DOIs
StatePublished - Jan 1 1995

Publication series

NameGeophysical Monograph Series
Volume87
ISSN (Print)0065-8448
ISSN (Electronic)2328-8779

ASJC Scopus subject areas

  • Geophysics

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  • Cite this

    Gardner, C. S. (1995). Scale-independent diffusive filtering theory of gravity wave spectra in the atmosphere. In R. M. Johnson, & T. L. Killeen (Eds.), The Upper Mesosphere and Lower Thermosphere: A Review of Experiment and Theory, 1995 (pp. 153-175). (Geophysical Monograph Series; Vol. 87). Blackwell Publishing Ltd.. https://doi.org/10.1029/GM087p0153