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Volume 13, issue 14
Atmos. Chem. Phys., 13, 7263-7278, 2013
https://doi.org/10.5194/acp-13-7263-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: VAMOS Ocean-Cloud-Atmosphere-Land Study (VOCALS) (ACP/OS inter-journal...

Atmos. Chem. Phys., 13, 7263-7278, 2013
https://doi.org/10.5194/acp-13-7263-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 30 Jul 2013

Research article | 30 Jul 2013

Ultrafine sea spray aerosol over the southeastern Pacific: open-ocean contributions to marine boundary layer CCN

R. Blot1, A. D. Clarke1,2, S. Freitag2, V. Kapustin1, S. G. Howell1, J. B. Jensen3, L. M. Shank1,*, C. S. McNaughton1,**, and V. Brekhovskikh1 R. Blot et al.
  • 1Department of Oceanography, University of Hawaii at Manoa, Hawaii, HI 96816, USA
  • 2Department of Meteorology, University of Hawaii at Manoa, Hawaii, HI 96816, USA
  • 3NCAR/EOL, Boulder, CO, USA
  • *now at: Pearl Harbor Naval Shipyard, Quality Assurance Division, JBPHH, HI 96860, USA
  • **now at: Golder Associates Ltd., Saskatoon, SK, Canada

Abstract. Accurate measurements of natural aerosol emissions over the ocean are needed to estimate the anthropogenic impact on the environment. In this study, we measured sea spray aerosol (SSA) concentrations with diameters larger than 0.040 μm produced by open-ocean breaking waves over the SEP (southeastern Pacific). Robust statistics were established through repeated airborne flights over 1000 km along 20° S from the coastline of Chile to 85° W during VOCALS-REx (VAMOS Ocean-Cloud-Atmosphere-Land-Study Regional Experiment). Non-volatile SSA number concentrations were inferred using a thermally resolved technique constrained for clean conditions with an Ångström exponent below 0.5, black carbon mass concentration at values lower than 15 ng m−3 and organic aerosol concentration less than 0.02 μg m−3. We found that number concentrations of SSAs active as cloud condensation nuclei (CCN) for a supersaturation of 0.25% varied between 17 and 36 cm−3, but these did not increase with the increasing mean wind speed typically observed further offshore along 20° S. Concurrent increases in mean offshore precipitation rate in excess of about 1 mm d−1 indicate that scavenging of SSAs by precipitation exceeds increases in production at wind speeds above about 8 m s−1. This demonstrates the critical role of precipitation as a major sink of SSA over the remote ocean. Finally, we found that under clean conditions and for estimated stratus supersaturations between 0.20 and 0.43%, SSA represented about 20% of the total potential CCN along 20° S.

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