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On the factors modulating the stratocumulus to cumulus transitions.

MPS-Authors
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Sandu,  I.
The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society;

/persons/resource/persons37347

Stevens,  B.
The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society;
Director’s Research Group AES, The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society;
A 2 - Climate Processes and Feedbacks, Research Area A: Climate Dynamics and Variability, The CliSAP Cluster of Excellence, External Organizations;

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http://journals.ametsoc.org/doi/pdf/10.1175/2011JAS3614.1
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2011jas3614.1.pdf
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Citation

Sandu, I., & Stevens, B. (2011). On the factors modulating the stratocumulus to cumulus transitions. Journal of the Atmospheric Sciences, 68, 1865-1881. doi:10.1175/2011JAS3614.1.


Cite as: https://hdl.handle.net/11858/00-001M-0000-0012-2D49-5
Abstract
Large-eddy simulation (LES) is used to explore the role of various processes in regulating the stratocumulus to cumulus transition (SCT). Simulations are based on a composite case derived from a Lagrangian analysis of 2 yr of data from the northeastern Pacific. The simulations reproduce well the observed transition from a compact stratocumulus layer to more broken fields of cumulus, simply as a response to increasing sea surface temperatures (SSTs) along the transition. In so doing they support earlier theoretical work that argued that the SCT was a response of boundary layer circulations to increased forcing by surface latent heat fluxes. Although the basic features of the SCT imposed by the increase in SST are robust, a variety of other factors affect the detailed character of the SCT. For example, enhanced precipitation or increased downwelling longwave radiative fluxes can accelerate the reduction in cloud cover that accompanies the SCT, while a gradual decrease in the large-scale divergence can make changes in cloud cover that accompany the SCT relatively more modest. The simulations also demonstrate that the pace of the SCT is mainly set by the strength of the temperature inversion capping the initial stratocumulus-topped boundary layer.