Primary marine aerosol-cloud interactions off the coast of California

  • R. L. Modini
  • , A. A. Frossard
  • , L. Ahlm
  • , L. M. Russell
  • , C. E. Corrigan
  • , G. C. Roberts
  • , L. N. Hawkins
  • , J. C. Schroder
  • , A. K. Bertram
  • , R. Zhao
  • , A. K.Y. Lee
  • , J. P.D. Abbatt
  • , J. Lin
  • , A. Nenes
  • , Z. Wang
  • , A. Wonaschütz
  • , A. Sorooshian
  • , K. J. Noone
  • , H. Jonsson
  • , J. H. Seinfeld
  • D. Toom-Sauntry, A. M. Macdonald, W. R. Leaitch

Research output: Contribution to journalArticlepeer-review

Abstract

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 reportedmeasurements of PMA size distributions, a constrained lognormal-mode-fitting procedure was devised to isolate PMA number size distributions fromtotal aerosol size distributions and applied to E-PEACEmeasurements. 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/s1) lasting 8 days, and 71 cm-3 during a period of higher wind speeds (average 16m/s1) 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 0.2 ± 0.04% during E-PEACE and 0.05-0.1% during SOLEDAD. The availablemeasurements show that cloud droplet number concentrations increased with > 100 nmparticles in E-PEACE but decreased in the three SOLEDAD cloud events.

Original languageEnglish (US)
Pages (from-to)4282-4303
Number of pages22
JournalJournal of geophysical research
Volume120
Issue number9
DOIs
StatePublished - 2015

ASJC Scopus subject areas

  • Condensed Matter Physics
  • Physical and Theoretical Chemistry
  • Polymers and Plastics
  • Materials Chemistry

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