Abstract
The DMS flux from the open ocean ranged from 1.3 μmol/m2/d in winter to 5-10 μmol/m2/d in late summer and fall. The annual DMS flux from the WNAO area is estimated to be 0.1 Tg S/yr. SO2 and nss-SO42- concentrations varied strongly with wind direction. SO2 levels were as low as 10 pptv in marine air and reached several ppbv in continentally derived air. Relatively weak and statistically not significant seasonal variations were observed for MSA, NO -3, and MSA/nss-SO42- and NO3-/nss-SO42- ratios. In contrast, NH4+ concentrations showed a clear seasonal variation with a maximum in late summer/early fall and a minimum in winter. Oceanic ammonia emissions may be important for marine background levels of ammonia and NH4+ in the WNAO atmosphere. Aerosol particles were predominantly acidic with NH4+/nss-SO42- ratios of 1-2 mol/mol. -from Authors
Original language | English |
---|---|
Pages (from-to) | 353-372 |
Number of pages | 20 |
Journal | Tellus, Series B |
Volume | 43 B |
Issue number | 5 |
Publication status | Published - 1991 |
Externally published | Yes |