4.6 Article

Primary marine aerosol-cloud interactions off the coast of California

Journal

JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
Volume 120, Issue 9, Pages 4282-4303

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1002/2014JD022963

Keywords

sea spray aerosol; marine aerosol; cloud condensation nuclei; stratocumulus clouds; supersaturations; aerosol-cloud interactions

Funding

  1. NSF [AGS-1360645, NSF AGS-1013423, NSF AGS-1008848]
  2. DOE [DE-SC0006679]
  3. ONR [N00014-11-1-0783, N00014-10-1-0200, N00014-10-1-0811]
  4. Scripps Postdoctoral Scholars program
  5. U.S. Department of Energy (DOE) [DE-SC0006679] Funding Source: U.S. Department of Energy (DOE)
  6. Div Atmospheric & Geospace Sciences
  7. Directorate For Geosciences [1360645] Funding Source: National Science Foundation

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Primary marine aerosol (PMA)-cloud interactions off the coast of California were investigated using observations of marine aerosol, cloud condensation nuclei (CCN), and stratocumulus clouds during the Eastern Pacific Emitted Aerosol Cloud Experiment (E-PEACE) and the Stratocumulus Observations of Los-Angeles Emissions Derived Aerosol-Droplets (SOLEDAD) studies. Based on recently reported measurements of PMA size distributions, a constrained lognormal-mode-fitting procedure was devised to isolate PMA number size distributions from total aerosol size distributions and applied to E-PEACE measurements. During the 12 day E-PEACE cruise on the R/V Point Sur, PMA typically contributed less than 15% of total particle concentrations. PMA number concentrations averaged 12 cm(-3) during a relatively calmer period (average wind speed 12m/s(1)) lasting 8 days, and 71cm(-3) during a period of higher wind speeds (average 16m/s(1)) lasting 5 days. On average, PMA contributed less than 10% of total CCN at supersaturations up to 0.9% during the calmer period; however, during the higher wind speed period, PMA comprised 5-63% of CCN (average 16-28%) at supersaturations less than 0.3%. Sea salt was measured directly in the dried residuals of cloud droplets during the SOLEDAD study. The mass fractions of sea salt in the residuals averaged 12 to 24% during three cloud events. Comparing the marine stratocumulus clouds sampled in the two campaigns, measured peak supersaturations were 0.20.04% during E-PEACE and 0.05-0.1% during SOLEDAD. The available measurements show that cloud droplet number concentrations increased with >100 nm particles in E-PEACE but decreased in the three SOLEDAD cloud events.

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