Buoyancy reversal, decoupling and the transition from stratocumulus to shallow cumulus topped marine boundary layers
نویسندگان
چکیده
منابع مشابه
Cloud transitions and decoupling in shear-free stratocumulus-topped boundary layers
Large-eddy simulations of shear-free stratocumulus-topped layers tend strongly toward a two-layer structure as the negative area in the buoyancy flux profile that would be necessary to maintain a mixed layer increases to more than 10% of the positive area. In addition to identifying a threshold for what amounts to a convective transition, the simulations provide further evidence that a commonly...
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ژورنال
عنوان ژورنال: Climate Dynamics
سال: 2010
ISSN: 0930-7575,1432-0894
DOI: 10.1007/s00382-010-0882-3