The External Scale of Clear Air Turbulence Derived from the Vertical Ozone Profile: Application to Vertical Transport Measurement

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  • 1 Service d' Aéronomie du CNRS, 91370 Verrières le Buisson, France
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Abstract

Using a high-resolution stratospheric ozonometer it has been possible to obtain vertical ozone profiles in which microfluctuations may be interpreted as the consequence of eddy diffusion. Applying Kolmogoroff's theory to the signal, one can deduce values of the main parameters of stratospheric turbulence.

Abstract

Using a high-resolution stratospheric ozonometer it has been possible to obtain vertical ozone profiles in which microfluctuations may be interpreted as the consequence of eddy diffusion. Applying Kolmogoroff's theory to the signal, one can deduce values of the main parameters of stratospheric turbulence.

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