4.6 Article

Submicron NE Atlantic marine aerosol chemical composition and abundance: Seasonal trends and air mass categorization

Journal

JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
Volume 119, Issue 20, Pages 11850-11863

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1002/2013JD021330

Keywords

seasonal trends; marine aerosol; primary organic matter; aerosol mass spectrometry

Funding

  1. Science Foundation Ireland [08/RFP/GEO1233]
  2. HEA-PRTLI4 Environment and Climate: Impact and Responses programme
  3. European Commission IP EUCAARI
  4. EPA-Ireland
  5. European Space Agency
  6. EC ACTRIS Research Infrastructure Action under the Seventh Framework Programme
  7. Department of Energy and Climate Change (DECC) [GA0201]
  8. Science Foundation Ireland (SFI) [08/RFP/GEO1233] Funding Source: Science Foundation Ireland (SFI)

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Three years of continuous Aerosol Mass Spectrometry measurements at the Mace Head Global Atmosphere Watch research station revealed seasonal patterns in the chemical composition of submicron NE Atlantic marine aerosol as well as distinct chemical signatures associated with marine air masses of different origin (i.e., polar, Arctic, or tropical). Concentrations of secondary inorganic aerosol species and both primary and secondary organic compounds were closely related to oceanic biological activity and ranged from low median mass concentrations during winter to high median values during summer as follows: 0.025-0.9 mu gm(-3) for nonsea-salt sulfate (nss-sulfate), 0.025-0.4 mu gm(-3) for organic matter, 0-0.09 mu gm(-3) for methanesulfonic acid (MSA). Sea-salt concentrations illustrated an opposite pattern with the highest median value being observed during winter (0.74 mu gm(-3)) and lowest during summer (0.08 mu gm(-3)). Maritime polar air masses typically featured the highest concentrations of sea salt and marine organics, particularly enhanced under primary organic plumes during periods of high biological activity. MSA and nss-sulfate were more prominent in tropical air masses. The oxidation of organic matter increased with increasing ozone concentration and wintertime (low biological activity) organic matter displayed a different fragmentation pattern from that of summertime organic compounds.

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