Journal of the Atmospheric Sciences · 1982 · 59 citations · 0 references
Natural SciencesEarth SciencesMeteorologyAtmospheric ScienceMesoscale MeteorologyRadar MeteorologyMesoscale DynamicsStratospheric MeteorologyTurbulenceMesoscale Wind DynamicsPower Spectra Of TurbulenceStratospheric WindsTemporal Power SpectrumTurbulence Spectra
Zonal and meridional wind measurements made with the Poker Flat MST radar over a 40-day period are used to calculate the frequency power spectra at heights between 5.99 and 14.69 km. The winds used in the analysis are 1 h averages of samples taken every 4 min. We find that the spectra follow an f−5/3 power law in the range of periods from 2 to 50 h. If the Taylor transformation is valid in this frequency range, this would imply a k−5/3 wavenumber spectrum, corresponding to an inertial subrange for two-dimensional turbulence at the atmospheric mesoscale. These observations support and extend earlier studies which also show a −5/3 power law behavior in the atmospheric mesoscale.