Atmospheric water-soluble organic nitrogen (WSON) over marine environments: A global perspective

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Abstract

To obtain a comprehensive picture of the spatial distribution of water-soluble organic nitrogen (WSON) in marine aerosols, samples were collected during research cruises in the tropical and southern Atlantic Ocean and also in the southern Indian Ocean (Amsterdam Island) for a 1-year period (2005). Samples were analyzed for both organic and inorganic forms of nitrogen, and the factors controlling their levels were examined. Fine-mode WSON was found to play a significant role in the remote marine atmosphere with enhanced biogenic activity, with concentrations of WSON (11.3 ± 3.3 nmol Nm -3) accounting for about 84 % of the total dissolved nitrogen (TDN). Such concentrations are similar to those observed in the polluted marine atmosphere of the eastern Mediterranean (11.6 ± 14.0 nmol N m -3). Anthropogenic activities were found to be an important source of atmospheric WSON as evidenced by the levels in the Northern Hemisphere (NH) being 10 times higher than in the remote Southern Hemisphere (SH). Furthermore, the higher contribution of fine-mode WSON to TDN (51%) in the SH, compared to the NH (13%), underlines the important role of organic nitrogen in remote marine areas. Finally, there was a strong association of WSON with dust in coarse-mode aerosols in the NH.

Figures

  • Figure 1. Sampling sites around the world during this study. Finokalia station is used for comparison purposes.
  • Figure 2. Temporal variation in nitrogen species and nss-SO2− 4 and nss-Ca2+concentration in coarse particles (Da > 2 µm) over the tropical North Atlantic atmosphere. The frame defines the air mass back trajectory with dust mixed with anthropogenic sources (19 July 2006).
  • Figure 4. Temporal variation in nitrogen species concentration in fine particles (Da < 2 µm) over the tropical North Atlantic atmosphere.
  • Figure 3. Five-day air mass back trajectories for 19 July (a) and 3 August 2006 (b). The color indicates the pressure level (hPa).
  • Figure 6. Temporal variation in WSON and DMS concentration in fine particles (PM2.5) together with BC concentration during the cruise in South Atlantic atmosphere. The frames define the marine areas with intense biogenic activity (episodes A and B).
  • Figure 5. Two distinct phytoplankton bloom episodes are presented on a SeaWiFS chlorophyll a map of the South Atlantic Ocean during January 2007 along with the cruise track (http://disc.sci.gsfc. nasa.gov/giovanni). Episode A was encountered by the ship over 2 days (30–31 January 2007, n= 4) and episode B began on 1 February and was followed until the end of the cruise (n= 5). Remote marine conditions with low biogenic activity lasted 4 days (26–29 January 2007, n= 5), while marine conditions mixing with continental influence lasted 6 days (21–25 January 2007, n= 9).
  • Figure 7. Five-day air mass back trajectories for 30 January 2007 (a) and 31 January 2007 (b) during episode A. The color indicates the pressure level (hPa).
  • Figure 10. Chlorophyll map obtained for January (SeaWiFS data) for the Indian sector of the Austral Ocean. The white frame corresponds to the source region, which could contribute to the levels of marine organics at Amsterdam Island.

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CITATION STYLE

APA

Violaki, K., Sciare, J., Williams, J., Baker, A. R., Martino, M., & Mihalopoulos, N. (2015, May 29). Atmospheric water-soluble organic nitrogen (WSON) over marine environments: A global perspective. Biogeosciences. Copernicus GmbH. https://doi.org/10.5194/bg-12-3131-2015

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