Articles | Volume 17, issue 5
Atmos. Chem. Phys., 17, 3699–3712, 2017
https://doi.org/10.5194/acp-17-3699-2017
Atmos. Chem. Phys., 17, 3699–3712, 2017
https://doi.org/10.5194/acp-17-3699-2017

Research article 16 Mar 2017

Research article | 16 Mar 2017

Wintertime enhancements of sea salt aerosol in polar regions consistent with a sea ice source from blowing snow

Jiayue Huang and Lyatt Jaeglé

Data sets

NOAA Regional Aerosol Sampling Stations P. K. Quinn, T. L. Miller, T. S. Bates, J. A. Ogren, E. Andrews, and G. E. Shaw https://saga.pmel.noaa.gov/data/stations/

Environment and Climate Change Canada Government of Canada http://www.ec.gc.ca/donneesnatchem-natchemdata/

European Monitoring and Evalution Programme WMO/GAW http://ebas.nilu.no/

Trace elements in the aerosol at Neumayer Station R. Weller, J. Wöltjen, C. Piel, R. Resenberg, D. Wagenbach, G. König-Langlo, and M. Kriews https://doi.org/10.1594/PANGAEA.691456

CESOA M. Legrand, V. Gros, S. Preunkert, R. Sarda-Estève, A.-M. Thierry, G. Pépy, and B. Jourdain http://www-lgge.obs.ujf-grenoble.fr/CESOA/spip.php?rubrique2

ICEALOT: International Chemistry Experiment in the Arctic LOwer Troposphere NOAA PMEL https://saga.pmel.noaa.gov/Field/icealot

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Short summary
The emissions and distribution of wintertime sea salt aerosol (SSA) are poorly constrained in polar regions, despite their potentially significant roles in halogen release, cloud formation and climate. We implement a blowing snow and a frost flower emission scheme in the model, and find that inclusion of blowing snow is necessary to simulate the observed winter and spring SSA levels. We estimate that inclusion of blowing snow increases submicron SSA emissions by factors of 2–3 in polar regions.
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