The
Arctic is experiencing the greatest warming on Earth, as most
evident by rapid sea ice loss. Delayed sea ice freeze-up in the Alaskan
Arctic is decreasing wintertime sea ice extent and changing marine
biological activity. However, the impacts of newly open water on wintertime
sea spray aerosol (SSA) production and atmospheric composition are
unknown. Herein, we identify SSA, produced locally from open sea ice
fractures (leads), as the dominant aerosol source in the coastal Alaskan
Arctic during winter, highlighting the year-round nature of Arctic
SSA emissions. Nearly all of the individual SSA featured thick organic
coatings, consisting of marine saccharides, amino acids, fatty acids,
and divalent cations, consistent with exopolymeric secretions produced
as cryoprotectants by sea ice algae and bacteria. In contrast, local
summertime SSA lacked these organic carbon coatings, or featured thin
coatings, with only open water nearby. The individual SSA composition
was not consistent with frost flowers or surface snow above sea ice,
suggesting that neither hypothesized frost flower aerosolization nor
blowing snow sublimation resulted in the observed SSA. These results
further demonstrate the need for inclusion of lead-based SSA production
in modeling of Arctic atmospheric composition. The identified connections
between changing sea ice, microbiology, and SSA point to the significance
of sea ice lead biogeochemistry in altering Arctic atmospheric composition,
clouds, and climate feedbacks during winter.