Research Article
Ocean Emission Effects on Aerosol-Cloud Interactions: Insights from Two Case Studies
Table 2
Statistical summary of the ACIr analysis shown in Figure 3. The numbers reported below represent ratios of a particular parameter between periods of relatively high chlorophyll A (0.3 mg m-3; October–February) versus low chlorophyll A (0.3 mg m-3; April–August). The average and standard deviation calculations are based on 11 values representing individual LWP bins between 50 and 350 g m-2. These results represent 27 months of data starting in June 2006 for the Southern Ocean region (42° S–60° S, 180° W–180° E). (AI = aerosol index; AOD = aerosol optical depth; ANG = Ångstrom exponent; = cloud drop effective radius; min = minimum value; max = maximum value).
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