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Contribution of sea surface carbon pool to organic matter enrichment in sea spray aerosol

Abstract

Breaking waves on the ocean surface generate air bubbles that scavenge organic matter from the surrounding sea water. When injected into the atmosphere, these bubbles burst, yielding sea spray aerosols enriched in organic matter, relative to the sea water. Downwind of plankton blooms, the organic carbon content of sea spray aerosol is weakly correlated with satellite-derived measurements of chlorophyll a levels, a measure of phytoplankton biomass. This correlation has been used in large-scale models to calculate the organic enrichment in sea spray aerosol. Here, we assess the relationship between the organic carbon content of sea water and freshly emitted sea spray aerosol in the presence and absence of plankton blooms in the North Atlantic Ocean and the coastal waters of California. The organic carbon content of freshly emitted sea spray aerosol was similar in all regions sampled, despite significant differences in seawater chlorophyll a levels. The proportion of freshly emitted aerosols that served as cloud condensation nuclei at a given supersaturation was also similar across sampling sites. The large reservoir of organic carbon in surface sea water remained relatively constant across the regions sampled, and independent of variations in chlorophyll a concentrations. We suggest that this reservoir is responsible for the organic carbon enrichment of freshly emitted sea spray aerosol, overwhelming any influence of local biological activity as measured by chlorophyll a levels.

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Figure 1: CalNex and WACS cruise tracks superimposed on maps of satellite-derived Chl a concentration.
Figure 2: Average mass fractions of organic carbon (OC) and sea salt in nascent sea spray aerosol generated by Sea Sweep.
Figure 3: CCN activity for the calibration aerosol and WACS Stations 1 and 2 for size-selected dry diameters (40, 50, 60, 80, and 100 nm).
Figure 4: Size-resolved Sea-Sweep-generated SSA organic volume fraction and hygroscopicity parameter (κ), derived from CCN activation curves.

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References

  1. Carlson, C. A. in Biogeochemistry of Marine Dissolved Organic Matter (eds Hansell, D. A. & Carlson, C. A.) 90–151 (Academic, (2002).

    Google Scholar 

  2. Mayer, L. M. The inertness of being organic. Mar. Chem. 92, 135–140 (2004).

    Google Scholar 

  3. Hansell, D. A., Carlson, C. A., Repeta, D. J. & Schlitzer, R. Dissolved organic matter in the ocean: New insights stimulated by a controversy. Oceanography 22, 52–61 (2009).

    Google Scholar 

  4. Hansell, D. A. & Carlson, C. A. Biogeochemistry of total organic carbon and nitrogen in the Sargasso Sea: Control by convective overturn. Deep-Sea Res. II 48, 1649–1667 (2001).

    Google Scholar 

  5. Spracklen, D. V., Arnold, S. R., Carslaw, K. S., Sciare, J. & Pio, C. Globally significant oceanic source of organic carbon aerosol. Geophys. Res. Lett. 35, L12811 (2008).

    Google Scholar 

  6. O’Dowd, C. D. et al. A combined organic-inorganic sea-spray source function. Geophys. Res. Lett. 35, L01801 (2008).

    Google Scholar 

  7. Sciare, J. et al. Long-term observations of carbonaceous aerosol in the Austral Ocean atmosphere: Evidence of a biogenic marine organic source. J. Geophys. Res. 114, D15302 (2009).

    Google Scholar 

  8. Langmann, S., Scannell, C. D. & O’Dowd, New directions: Organic matter contribution to marine aerosols and cloud condensation nuclei. Atmos. Environ. 42, 821–7822 (2008).

    Google Scholar 

  9. Vignatti, E. et al. Global scale emission and distribution of seaspray aerosol: Sea salt and organic enrichment. Atmos. Environ. 44, 670–677 (2010).

    Google Scholar 

  10. Rinaldi, M. et al. Is chlorophyll a the best surrogate for organic matter enrichment in submicron primary marine aerosol?. J. Geophys. Res. (2013)10.1002/jgrd.50417

  11. Gantt, B. et al. Wind speed dependent size-resolved parameterization for the organic mass fraction of seaspray aerosol. Atmos. Chem. Phys. 11, 8777–8790 (2011).

    Google Scholar 

  12. Zhou, X. et al. Photochemical production of hydroxyl radical and hydroperoxides in water extracts of nascent marine aerosols produced by bursting bubbles from Sargasso seawater. Geophys. Res. Lett. 35, L20803 (2008).

    Google Scholar 

  13. Turekian, V., Macko, S. A. & Keene, W. C. Concentrations, isotopic compositions, and sources of size-resolved, particulate organic carbon and oxalate in near-surface marine air at Bermuda during spring. J. Geophys. Res. 108, 4157 (2003).

    Google Scholar 

  14. Bates, T. S. et al. Measurements of ocean derived aerosol off the coast of California. J. Geophys. Res. 117 (2012)10.1029/2012JD017588

    Google Scholar 

  15. Chen, C. & Beardsley, R. C. Cross-frontal water exchange on Georges Bank: Some results from an U.S. GLOBEC/Georges Bank program model study. J. Ocean. 58, 403–420 (2002).

    Google Scholar 

  16. Townsend, D. W. & Thomas, M. Springtime nutrient and phytoplankton dynamics on Georges Bank. Mar. Ecol. Prog. Ser. 228, 57–74 (2002).

    Google Scholar 

  17. Hoffman, E. J. & Duce, R. A. Factors influencing the organic carbon content of marine aerosols: A laboratory study. J. Geophys. Res. 81, 3667–3670 (1976).

    Google Scholar 

  18. Keene, W. C. et al. Chemical and physical characteristics of nascent aerosols produced by bursting bubbles at a model air–sea interface. J. Geophys. Res. 112, D21202 (2007).

    Google Scholar 

  19. Facchini, M. C. et al. Primary submicron marine aerosol dominated by insoluble organic colloids and aggregates. Geophys. Res. Lett. 35, L17814 (2008).

    Google Scholar 

  20. Fuentes, E., Coe, H., Gree, D. & McFiggans, G. On the impacts of phytoplankton-derived organic matter on the properties of primary marine aerosol – Part 2: Composition, hygroscopicity and cloud condensation activity. Atm. Chem. Phys. 11, 2585–2602 (2011).

    Google Scholar 

  21. Cruz, C. N. & Pandis, S. N. Deliquescence and hygroscopic growth of mixed inorganic-organic atmospheric aerosol. Environ. Sci. Tech. 34, 4313–4319 (2000).

    Google Scholar 

  22. Long, M. S., Keene, W. C., Kieber, D. J., Erickson, D. J. & Maring, H. A sea-state based source function for size- and composition-resolved marine aerosol production. Atm. Chem. Phys. 11, 1203–1216 (2011).

    Google Scholar 

  23. Bates, T. S., Coffman, D. J., Covert, D. S. & Quinn, P. K. Regional marine boundary layer aerosol size distributions in the Indian, Atlantic, and Pacific Oceans: A comparison of INDOEX measurements with ACE-1, ACE-2, and Aerosols99. J. Geophys. Res. 107, 8026–8039 (2002).

    Google Scholar 

  24. Berner, A., Lurzer, C., Pohl, F., Preining, O. & Wagner, P. The size distribution of the urban aerosol in Vienna. Sci. Total Environ. 13, 245–261 (1979).

    Google Scholar 

  25. Quinn, P. K., Coffman, D. J., Kapustin, V. N., Bates, T. S. & Covert, D. S. Aerosol optical properties in the marine boundary layer during ACE 1 and the underlying chemical and physical aerosol properties. J. Geophys. Res. 103, 16547–16563 (1998).

    Google Scholar 

  26. Holland, H. D. The Chemistry of the Atmosphere and Oceans 154 (John Wiley, (1978).

    Google Scholar 

  27. Bates, T. S. et al. Marine boundary layer dust and pollution transport associated with the passage of a frontal system over eastern Asia. J. Geophys. Res. 109, D19S19 (2004).

    Google Scholar 

  28. Frossard, A. A. & Russell, L. M. Removal of sea salt hydrate water from seawater-derived samples by dehydration. Environ. Sci. Tech. 46 (2012)10.1021/es3032083

  29. Takahama, S., Johnson, A. & Russell, L. M. Quantification of carboxylic and carbonyl functional groups in organic aerosol infrared absorbance spectra. Aerosol Sci. Tech. (2012)10.1080/02786826.2012.752065

  30. Roberts, G. C. & Nenes, A. A continuous-flow streamwise thermal gradient CCN chamber for atmospheric measurements. Aerosol Sci. Tech. 39, 206–221 (2005).

    Google Scholar 

  31. Lance, S., Medina, J., Smith, J. N. & Nenes, A. Mapping the operation of the DMT continuous flow CCN counter. Aerosol Sci. Tech. 40, 242–254 (2006).

    Google Scholar 

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Acknowledgements

This work was supported in part by the NOAA Atmospheric Composition and Climate Program and the National Science Foundation Chemical Oceanography Program (1129896 to DJK, 1129836 to WCK and 1129580 to LMR) and Atmospheric Dynamics Program (1013423 to LMR). We thank D. Hamilton, J. Johnson, I. Tyssebotn, J. Kinsey and M. Haserodt for their assistance in sample collection and analysis; V. Trainer for the loan and calibration of the fluorometer; the captain and crew of the NOAA R/V Ronald H. Brown for support at sea; M. Rinaldi and C. Facchini for MAP data and helpful comments; and S. Gasso for discussions on satellite images of Chl a. This is PMEL contribution 4046.

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All authors contributed extensively to the work presented in this paper. P.K.Q., T.S.B., W.C.K., D.J.K., L.M.R., and A.A.F. designed and performed the experiments, analysed data and wrote the paper. D.J.C. and K.S.S. performed the experiments and analysed data.

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Correspondence to Patricia K. Quinn.

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The authors declare no competing financial interests.

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Quinn, P., Bates, T., Schulz, K. et al. Contribution of sea surface carbon pool to organic matter enrichment in sea spray aerosol. Nature Geosci 7, 228–232 (2014). https://doi.org/10.1038/ngeo2092

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