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Turbulence in the stratocumulus-topped boundary layer is powered mostly by radiative cooling at the top of the cloud. This work investigate how concentrated this cooling has to be to maintian stratocumulus clouds.

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This page is a summary of: How finely do we need to represent the stratocumulus radiative effect?, Quarterly Journal of the Royal Meteorological Society, June 2016, Wiley,
DOI: 10.1002/qj.2828.
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