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  • Author or Editor: P. Aimedieu x
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J. Barat and P. Aimedieu

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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