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The key parameters controlling cumulus cloud-cover extent are derived by formulating a simple theory of the inversion-capped, convectionally unstable planetary boundary layer. The theory provides a predictive parameter which is found statistically to distinguish significantly between days of different cumulus cloud-cover formation.
The key parameters controlling cumulus cloud-cover extent are derived by formulating a simple theory of the inversion-capped, convectionally unstable planetary boundary layer. The theory provides a predictive parameter which is found statistically to distinguish significantly between days of different cumulus cloud-cover formation.
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