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).

AI
(min)
AI
(max)
AI
(range)
AOD
(min)
AOD
(max)
AOD
(range)
ANG
(min)
ANG
(max)
ANG
(range)

(min)

(max)

(range)

Average3.461.691.551.511.201.192.571.391.331.150.990.94
Std. Dev.0.770.380.390.470.370.391.180.340.340.380.030.14