Observational evidence for the formation of DMS-derived aerosols during Arctic phytoplankton blooms
The connection between marine biogenic dimethyl sulfide (DMS) and the formation of aerosol particles in the Arctic atmosphere was evaluated by analyzing atmospheric DMS mixing ratio, aerosol particle size distribution and aerosol chemical composition data that were concurrently collected at Ny-Å...
Main Authors: | , , , , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2017-08-01
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Series: | Atmospheric Chemistry and Physics |
Online Access: | https://www.atmos-chem-phys.net/17/9665/2017/acp-17-9665-2017.pdf |
Summary: | The connection between marine biogenic dimethyl sulfide (DMS) and the
formation of aerosol particles in the Arctic atmosphere was evaluated by
analyzing atmospheric DMS mixing ratio, aerosol particle size distribution
and aerosol chemical composition data that were concurrently collected at
Ny-Ålesund, Svalbard (78.5° N, 11.8° E), during April
and May 2015. Measurements of aerosol sulfur (S) compounds showed distinct
patterns during periods of Arctic haze (April) and phytoplankton blooms
(May). Specifically, during the phytoplankton bloom period the contribution
of DMS-derived SO<sub>4</sub><sup>2−</sup> to the total aerosol SO<sub>4</sub><sup>2−</sup>
increased by 7-fold compared with that during the proceeding Arctic haze
period, and accounted for up to 70 % of fine SO<sub>4</sub><sup>2−</sup> particles
(< 2.5 µm in diameter). The results also showed that the
formation of submicron SO<sub>4</sub><sup>2−</sup> aerosols was significantly
associated with an increase in the atmospheric DMS mixing ratio. More
importantly, two independent estimates of the formation of DMS-derived
SO<sub>4</sub><sup>2−</sup> aerosols, calculated using the stable S-isotope ratio and
the non-sea-salt SO<sub>4</sub><sup>2−</sup> ∕ methanesulfonic acid ratio,
respectively, were in close agreement, providing compelling evidence that the
contribution of biogenic DMS to the formation of aerosol particles was
substantial during the Arctic phytoplankton bloom period. |
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ISSN: | 1680-7316 1680-7324 |