Impact of the variability in vertical separation between biomass burning aerosols and marine stratocumulus on cloud microphysical properties over the Southeast Atlantic
Authors: Gupta Siddhant , McFarquhar Greg M. , O'Brien Joseph R. , Delene David J. , Poellot Michael R. , Dobracki Amie , Podolske James R. , Redemann Jens , LeBlanc Samuel E. , Segal-Rozenhaimer Michal , Pistone Kristina 
Published: March 2021

Abstract. 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 (Na) > 500 cm−3 was within 100 m of cloud tops, and
41 separated profiles, where the aerosol layer with Na > 500 cm−3 was located more than 100 m above
cloud tops. For contact profiles, the average cloud droplet concentration (Nc) in the cloud layer was up to
68 cm−3 higher, the effective radius (Re) up to 1.3 µm lower, and the liquid water content (LWC) within
0.01 g m−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
Na (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 Nc 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 Nc (30 %) and LWC
(16 %) near cloud tops. Below-cloud Na was sampled during 61 profiles, and most contact profiles (20 out of 28) were within high-Na
(> 350 cm−3) boundary layers, while most separated profiles (22 out of 33) were within low-Na
(< 350 cm−3) boundary layers. Although the differences in below-cloud Na were statistically insignificant,
contact profiles within low-Na boundary layers had up to 34.9 cm−3 higher Nc compared to
separated profiles. This is consistent with a weaker impact of droplet evaporation in the presence of biomass burning aerosols within
100 m above cloud tops. For contact profiles within high-Na boundary layers, the presence of biomass burning
aerosols led to higher below-cloud Na (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-Na boundary layers had up to 88.4 cm−3
higher Nc compared to separated profiles. These results motivate investigations of aerosol–cloud–precipitation interactions
over the Southeast Atlantic since the changes in Nc and Re 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.