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The importance of vertical velocity variability for estimates of the indirect aerosol effects

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Figure

Table 1. Configuration of the GLOMAP-mode aerosol scheme, with component species: sulfate (SO4), sea salt (SS), black carbon (BC),organic carbon (OC), and dust (DU)
Table 2. Definitions of vertical velocity pdfs in HadGEM-UKCAconfigurations.
Table 3. Details of flight campaigns through marine stratiform clouds used for model evaluation.
Fig. 2c. An increase of σw = 0.1 to σw = 0.4ms− leads to aglobal area-weighted mean increase in CDNC of 21.8cm−3but the magnitude of the increase is less than half as large
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