Atmospheric Chemistry and Physics, vol. 13, issue 4 (2013) pp. 1913-1926
Secondary organic aerosols (SOA) exert a significant influence on ambient air quality and regional climate. Recent field, laboratorial and modeling studies have confirmed that in-cloud processes contribute to a large fraction of SOA production with large space-time heterogeneity. This study evaluates the key factors that govern the production of cloud-process SOA (SOA(cld)) on a global scale based on the GFDL coupled chemistry-climate model AM3 in which full cloud chemistry is employed. The association between SOA(cld) production rate and six factors (i.e., liquid water content (LWC), total carbon chemical loss rate (TCloss), temperature, VOC/NOx, OH, and O-3) is examined. We find that LWC alone determines the spatial pattern of SOA(cld) production, particularly over the tropical, subtropical and temperate forest regions, and is strongly correlated with SOA(cld) production. TCloss ranks the second and mainly represents the seasonal variability of vegetation growth. Other individual factors are essentially uncorrelated spatiotemporally to SOA(cld) production. We find that the rate of SOA(cld) production is simultaneously determined by both LWC and TCloss, but responds linearly to LWC and nonlinearly (or concavely) to TCloss. A parameterization based on LWC and TCloss can capture well the spatial and temporal variability of the process-based SOA(cld) formation (R-2 = 0.5) and can be easily applied to global three dimensional models to represent the SOA production from cloud processes.
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