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Title: Frequency spectra of vertical velocity from Flatland VHF radar data

Journal Article · · Journal of Geophysical Research; (United States)
DOI:https://doi.org/10.1029/90JD02220· OSTI ID:5600502
;  [1];  [2]
  1. National Oceanic and Atmospheric Administration, Boulder, CO (USA)
  2. St. Cloud State Univ., MN (USA)

The vertical wind velocity over very flat terrain was observed every 153 s in the troposphere and lower stratosphere by the Flatland radar, near Champaign-Urbana, Illinois. By stratifying the spectra in various ways, the authors find the following: (1) the spectra were independent of altitude within the troposphere or lower stratosphere, but the spectra in the two regions differed in amplitude and frequency; (2) at a given altitude the spectra were independent of the wind shear d{bar u}/dz, the buoyancy frequency N, and the maximum wind speed below 16 km; (3) the change of spectral shape and amplitude with increasing background wind speed {bar u} was much less than at stations near mountains. The variance of the spectra, equal to twice the vertical kinetic energy per unit mass, roughly doubled as {bar u} increased by 10 m/s; (4) the spectra were consistent with being due to a spectrum of gravity waves, as indicated by the sharp drop in spectral amplitude near N at small {bar u} and by the fact that the observed change of shape with increasing {bar u} was quite consistent with the change of shape of model Doppler-shifted gravity wave spectra; (5) the results of comparison between the observed and model spectra are consistent with an intrinsic gravity wave spectrum that is invariant with {bar u}, d{bar u}/dz, etc., contrary to expectations from gravity wave theory; (6) the results are insensitive to the azimuthal distribution of gravity wave energy, as long as the distribution is roughly symmetrical relative to the mean flow; (7) the resulting characteristic horizontal phase velocity c{sub *} of the intrinsic frequency spectrum was about 6 m/s in both the troposphere and the stratosphere.

OSTI ID:
5600502
Journal Information:
Journal of Geophysical Research; (United States), Vol. 96:D2; ISSN 0148-0227
Country of Publication:
United States
Language:
English