Impact Of The Variability In Vertical Separation Between Biomass Burning Aerosols And Marine Stratocumulus On Cloud Microphysical Properties Over The Southeast Atlantic

Marine stratocumulus cloud properties over the Southeast Atlantic Ocean are impacted by contact between above-cloud biomass burning aerosols and cloud tops. Different vertical separations (0 to 2000 m) between the aerosol layer and cloud tops were observed on six research flights in September 2016 during the NASA ObseRvations of Aerosols above CLouds and their intEractionS (ORACLES) field campaign. There were 30 contact profiles, where an aerosol layer with aerosol concentration (N-a) > 500 cm(-3) was within 100m of cloud tops, and 41 separated profiles, where the aerosol layer with N-a > 500 cm(-3) was located more than 100m above cloud tops. For contact profiles, the average cloud droplet concentration (N-c) in the cloud layer was up to 68 cm(-3) higher, the effective radius (R-e) up to 1.3 mu m lower, and the liquid water content (LWC) within 0.01 gm(-3) compared to separated profiles. Free-tropospheric humidity was higher in the presence of biomass burning aerosols, and contact profiles had a smaller decrease in humidity (and positive buoyancy) across cloud tops with higher median above-cloud N-a (895 cm(-3)) compared to separated profiles (30 cm(-3)). Due to droplet evaporation from entrainment mixing of warm, dry free-tropospheric air into the clouds, the median N-c and LWC for contact profiles decreased with height by 21 and 9% in the top 20% of the cloud layer. The impact of droplet evaporation was stronger during separated profiles as a greater decrease in humidity (and negative buoyancy) across cloud tops led to greater decreases in median N-c (30 %) and LWC (16 %) near cloud tops.Below-cloud N-a was sampled during 61 profiles, and most contact profiles (20 out of 28) were within high-N-a (> 350 cm(-3)) boundary layers, while most separated profiles (22 out of 33) were within low-N-a (< 350 cm(-3)) boundary layers. Although the differences in below-cloud Na were statistically insignificant, contact profiles within low-N-a boundary layers had up to 34.9 cm(-3) higher N-c compared to separated profiles. This is consistent with a weaker impact of droplet evaporation in the presence of biomass burning aerosols within 100m above cloud tops. For contact profiles within high-N-a boundary layers, the presence of biomass burning aerosols led to higher below-cloud N-a (up to 70.5 cm(-3)) and additional droplet nucleation above the cloud base along with weaker droplet evaporation. Consequently, the contact profiles in high-N-a boundary layers had up to 88.4 cm(-3) higher N-c compared to separated profiles. These results motivate investigations of aerosol-cloud-precipitation interactions over the Southeast Atlantic since the changes in N-c and R-e induced by the presence of above-cloud biomass burning aerosols are likely to impact precipitation rates, liquid water path, and cloud fraction, and modulate closed-to-open-cell transitions.