Seasonal updraft speeds change cloud droplet number concentrations in low level clouds over the Western North Atlantic

• Main Authors: Kirschler, Simon, Voigt, Christiane, Anderson, Bruce, Campos Braga, Ramon, Chen, Gao, Corral, Andrea F., Crosbie, Ewan, Dadashazar, Hossein, Ferrare, Richard F., Hahn, Valerian, Hendricks, Johannes, Kaufmann, Stefan, Moore, Richard, Pöhlker, Mira L., Robinson, Claire, Scarino, Amy J., Schollmayer, Dominik, Shook, Michael A., Thornhill, K. Lee, Winstead, Edward, Ziemba, Luke D., Sorooshian, Armin
• Format: Text
• Language: English
• Published: 2022
• Subjects: North Atlantic
• Online Access: https://doi.org/10.5194/acp-2022-171; https://acp.copernicus.org/preprints/acp-2022-171/

Low level clouds over the Western North Atlantic show a seasonal cycle in cloud properties which anticorrelates to aerosol concentrations. To determinate the impact of dynamic and aerosol processes within marine low clouds we examine the seasonal impact of updraft speed w and cloud condensation nuclei concentration at 0.43 % supersaturation (N CCN 0.43 % ) on the cloud droplet number concentration (N C ) of low level clouds over the Western North Atlantic Ocean. Aerosol and cloud properties were measured with instruments on board the NASA LaRC Falcon HU-25 during the ACTIVATE (Aerosol Cloud meTeorology Interactions oVer the western ATlantic Experiment) mission in summer (August) and winter (February-March) 2020. The data are grouped in different N CCN 0.43 % loadings and the density functions of N C and w near the cloud bases are compared. For low updrafts ( w < 1.3 m s -1 ), N C in winter are mainly limited by the updraft speed and in summer additionally by aerosols. At larger updrafts ( w > 3 m s -1 ), N C are impacted by the aerosol population, while at clean marine conditions cloud nucleation is aerosol limited and for high pollution it is influenced by aerosols and updraft. The aerosol size distribution in winter shows a bimodal distribution in clean marine environments, which transforms to a unimodal distribution in high pollution levels due to altering processes, whereas unimodal distributions prevail in summer with a significant difference in their aerosol concentration and composition. The increase in pollution level is accompanied with an increase of organic aerosol and sulfate compounds in both seasons. We demonstrate that N C can be explained by cloud condensation nuclei activation through upwards processed air masses with varying fractions of activated aerosols. The activation highly depends on w and thus supersaturation between the different seasons, while the aerosol size distribution additionally affects N C within a season. Our results quantify the seasonal influence of w and N CCN 0.43 % on N C and can be used to improve the representation of low marine clouds in models.