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The physical and chemical characteristics of marine primary organic aerosol: A review

by B. Gantt, N. Meskhidze
Atmospheric Chemistry and Physics ()
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Knowledge of the physical characteristics and chemical composition of marine organic aerosols is needed for the quantification of their effects on solar radiation trans- fer and cloud processes. This review examines research per- tinent to the chemical composition, size distribution, mixing state, emission mechanism, photochemical oxidation and cli- matic impact of marine primary organic aerosol (POA) asso- ciated with sea-spray. Numerous measurements have shown that both the ambient mass concentration of marine POA and size-resolved organic mass fraction of sea-spray aerosol are related to surface ocean biological activity. Recent studies have also indicated that fine mode (smaller than 200nm in diameter) marine POA can have a size distribution indepen- dent from sea-salt, while coarse mode aerosols (larger than 1000nm in diameter) are more likely to be internally mixed with sea-salt. Modelling studies have estimated global sub- micron marine POA emission rates of∼10±5 Tgyr−1, with a considerable fraction of these emissions occurring over regions most susceptible to aerosol perturbations. Climate studies have found that marine POA can cause large local increases in the cloud condensation nuclei concentration and have a non-negligible influence on model assessments of the anthropogenic aerosol forcing of climate. Despite these signs of climate-relevance, the source strength, chemical composi- tion, mixing state, hygroscopicity, cloud droplet activation potential, atmospheric aging and removal of marine POA remain poorly quantified. Additional laboratory, field, and modelling studies focused on the chemistry, size distribution and mixing state of marine POA are needed to better under- stand

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