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• W2315676722 abstract "Abstract Vertical diffusion coefficients in the stratosphere are estimated from data obtained in the High Altitude Clear Air Turbulence (HICAT) investigation. The HICAT data sample was obtained from 285 flights of over 800,000 km distance, containing 24,000 flight kilometers of turbulence between 14 and 21 km MSL, and is the only such collection of fine-scale, true gust velocities in the stratosphere. One of the HICAT program objectives was to compute power spectral densities from each of the gust velocity component measurements over the wavelength range 30–15,000 m. The square roots of the integrals of these spectra for wavelengths <610 m, designated vi (for the ith component of velocity), were computed and related to the dissipation of kinetic energy, ϵ by use of the inertial range assumption in the form ϵ = [2υi2/(3ai)]½k.Here k is the lower wavenumber limit of the spectral integration (2π/610 m), and ai is equal to 0.5 for the longitudinal component and 0.65 for the lateral and vertical components, or..." @default.
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• W2315676722 date "1973-06-11" @default.
• W2315676722 modified "2023-09-23" @default.
• W2315676722 title "Stratospheric mixing estimated from high altitude turbulence measurements" @default.
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• W2315676722 doi "https://doi.org/10.2514/6.1973-497" @default.
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