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The effects of a background of stationary, homogeneous, isotropic turbulence on barium releases in the F region of the ionosphere are found by inclusion of such turbulence in previously derived nonlinear model equations. An approach similar to quasi‐linear theory yields an enhanced diffusion coefficient for the release. It is shown that this turbulent diffusion can account for the large length scales observed in F region barium releases.
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Hansen et al. (1988) studied this question.
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