Center for Aerosol Science and Engineering, Department of Energy,
Environmental and Chemical Engineering, Washington University in St. Louis, St. Louis, Missouri, USA
Environmental and Climate Science Department, Brookhaven National
Laboratory, Upton, New York, USA
Chongai Kuang
Environmental and Climate Science Department, Brookhaven National
Laboratory, Upton, New York, USA
Center for Aerosol Science and Engineering, Department of Energy,
Environmental and Chemical Engineering, Washington University in St. Louis, St. Louis, Missouri, USA
Environmental and Climate Science Department, Brookhaven National
Laboratory, Upton, New York, USA
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Total article views: 5,440 (including HTML, PDF, and XML)
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4,542
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5,440
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BibTeX: 73
EndNote: 135
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466
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Viewed (geographical distribution)
Total article views: 6,200 (including HTML, PDF, and XML)
Thereof 6,200 with geography defined
and 0 with unknown origin.
Total article views: 5,440 (including HTML, PDF, and XML)
Thereof 5,440 with geography defined
and 0 with unknown origin.
Total article views: 760 (including HTML, PDF, and XML)
Thereof 760 with geography defined
and 0 with unknown origin.
Condensational growth of Aitken-mode particles is a major source of cloud condensation nuclei in the remote marine boundary layer. It has been long thought that over remote oceans, condensation growth is dominated by sulfate that derives from ocean-emitted dimethyl sulfide. In this study, we present the first long-term observational evidence that, contrary to conventional thinking, organics play an even more important role than sulfate in particle growth over remote oceans throughout the year.
Condensational growth of Aitken-mode particles is a major source of cloud condensation nuclei in...
