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  4. A treatment for the stratocumulus-to-cumulus transition in GCMs
 
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A treatment for the stratocumulus-to-cumulus transition in GCMs

Journal
Climate Dynamics
Journal Volume
39
Journal Issue
12
Pages
3075-3089
Date Issued
2012
Author(s)
Xiao, H.
CHIEN-MING WU  
Mechoso, C.R.
Ma, H.-Y.
DOI
10.1007/s00382-012-1342-z
URI
http://www.scopus.com/inward/record.url?eid=2-s2.0-84869507394&partnerID=MN8TOARS
http://scholars.lib.ntu.edu.tw/handle/123456789/370607
Abstract
Numerical models of climate have great difficulties with the simulation of marine low clouds in the subtropical Pacific and Atlantic Oceans. It has been especially difficult to reproduce the observed geographical distributions of the different cloud regimes in those regions. The present study discusses mechanisms proposed in previous works for changing one regime into another. One criterion is based on the theory of stratocumulus destruction through cloud top entrainment instability due to buoyancy reversal-situations in which the mixture of two air parcels becomes denser than either of the original parcels due to evaporation of cloud water. Another criterion is based on the existence of decoupling in the boundary layer. When decoupled, the stratocumulus regime changes to another in which these clouds can still exist together with cumulus. In a LES study, the authors have suggested that a combination of those two criteria can be used to diagnose whether, at a location, the cloud regime corresponds to a well-mixed stratocumulus regime, a shallow cumulus regime, or to a transitional regime where the boundary layer is decoupled. The concept is tested in the framework of an atmospheric general circulation model (GCM). It is found that several outstanding features of disagreement between simulation and observation can be interpreted as misrepresentations of the cloud regimes by the GCM. A novel criterion for switching among regimes is proposed to alleviate the effects of these misrepresentations. © 2012 Springer-Verlag.
Subjects
Boundary layer; General circulation models; Marine low clouds; Stratocumulus; Stratocumulus-to-cumulus transition
SDGs

[SDGs]SDG13

[SDGs]SDG14

Other Subjects
atmospheric general circulation model; boundary layer; buoyancy; climate modeling; cloud microphysics; cloud water; entrainment; evaporation; geographical distribution; large eddy simulation; numerical model; stratocumulus; Atlantic Ocean; Atlantic Ocean (Subtropical); Pacific Ocean; Pacific Ocean (Subtropical)
Type
journal article

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