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Switching cloud cover and dynamical regimes from open to closed Benard cells in response to the suppression of precipitation by aerosols

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Academic year: 2021

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Fig. 1. Cloud cover fraction (CF, blue lines with circles) and drop effective radius (DER, denoted as R eff , red lines with rhombs) of shallow clouds as a function of aerosol optical depth (AOD) for 4 zones over the Atlantic Ocean during August 2002, as d
Fig. 2. A schematic illustration of the proposed mechanism for transition from non precipitating closed Benard cells to precipitating open cells and onward to nearly complete rainout and elimination of the clouds
Fig. 4. Same MODIS image as in Fig. 3, but for the MODIS prod- prod-uct of effective radius at 1-km resolution over a larger domain
Fig. 5. The cloud drop effective radius and cloud optical thickness from the center of the scene shown in Figs
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