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The Relationships Between Cloud Top Radiative Cooling Rates, Surface Latent Heat Fluxes, and Cloud‐Base Heights in Marine Stratocumulus
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2018
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Source: Journal of Geophysical Research: Atmospheres, 123(20)
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Journal Title:Journal of Geophysical Research: Atmospheres
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Description:Cloud top radiative cooling (CTRC) drives turbulence in marine boundary layers (MBLs) topped by stratocumulus clouds. This study examines the role of CTRC in regulating the surface-cloud coupling,surface latent heat fluxes, and cloud base height by exploiting a 6-month worth of shipborne observations over the subtropical northeast Paci fic in combination with geostationary satellite data. We find that owning to the prevailing equatorward flow that advects stratocumulus clouds over warmer sea surfaces, the vast majority of the decoupled stratocumulus decks are fed by divergence from the tops of underlying cumulus, forming cumulus-coupled MBL. The cumulus-coupled and well-mixed MBL dominate the subtropical MBL regimes. We find that strong CTRC favors greater (smaller) occurrence frequency of well-mixed
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Source:Journal of Geophysical Research: Atmospheres, 123(20)
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ISSN:2169-897X;2169-8996;
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Rights Information:Other
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