Global distribution and climate forcing of marine organic aerosol-Part 1. Model improvements and evaluation

• Published in: Atmospheric Chemistry and Physics
• Main Authors: Meskhidze, N., Xu, J., Gantt, B., Zhang, Y., Nenes, Athanasios, Ghan, S. J., Liu, X., Easter, R., Zaveri, R.
• Format: Text
• Language: unknown
• Published: 2018
• Subjects: Pacific; Southern Ocean
• Online Access: http://infoscience.epfl.ch/record/257462; https://doi.org/10.5194/acp-11-11689-2011; https://infoscience.epfl.ch/record/257462/files/11-11689-2011-acp-11-11689-2011.pdf

Marine organic aerosol emissions have been implemented and evaluated within the National Center of Atmospheric Research (NCAR)'s Community Atmosphere Model (CAM5) with the Pacific Northwest National Laboratory's 7-mode Modal Aerosol Module (MAM-7). Emissions of marine primary organic aerosols (POA), phytoplankton-produced isoprene-and monoterpenes-derived secondary organic aerosols (SOA) and methane sulfonate (MS-) are shown to affect surface concentrations of organic aerosols in remote marine regions. Global emissions of submicron marine POA is estimated to be 7.9 and 9.4 Tg yr-1, for the Gantt et al. (2011) and Vignati et al. (2010) emission parameterizations, respectively. Marine sources of SOA and particulate MS-(containing both sulfur and carbon atoms) contribute an additional 0.2 and 5.1 Tg y-1, respectively. Widespread areas over productive waters of the Northern Atlantic, Northern Pacific, and the Southern Ocean show marine-source submicron organic aerosol surface concentrations of 100 ng m-3, with values up to 400 ng mg-3 over biologically productive areas. Comparison of long-term surface observations of water insoluble organic matter (WIOM) with POA concentrations from the two emission parameterizations shows that despite revealed discrepancies (often more than a factor of 2), both Gantt et al. (2011) and Vignati et al. (2010) formulations are able to capture the magnitude of marine organic aerosol concentrations, with the Gantt et al. (2011) parameterization attaining better seasonality. Model simulations show that the mixing state of the marine POA can impact the surface number concentration of cloud condensation nuclei (CCN). The largest increases (up to 20%) in CCN (at a supersaturation (S) of 0.2%) number concentration are obtained over biologically productive ocean waters when marine organic aerosol is assumed to be externally mixed with sea-salt. Assuming marine organics are internally-mixed with sea-salt provides diverse results with increases and decreases in the concentration of CCN over ...