4.7 Article

Size-resolved aerosol and cloud condensation nuclei (CCN) properties in the remote marine South China Sea - Part 1: Observations and source classification

Journal

ATMOSPHERIC CHEMISTRY AND PHYSICS
Volume 17, Issue 2, Pages 1105-1123

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/acp-17-1105-2017

Keywords

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Funding

  1. NRL 6.1 Base Program via an Office of Naval Research (ONR) Global grant
  2. Office of Naval Research [N00014-16-1-2040]
  3. Naval Research Enterprise Internship Program (NREIP)
  4. NRL Base Program
  5. Colorado State University Center for Geosciences/Atmospheric Research (CG/AR)
  6. [ONR 35]

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Ship-based measurements of aerosol and cloud condensation nuclei (CCN) properties are presented for 2 weeks of observations in remote marine regions of the South China Sea/East Sea during the southwestern monsoon (SWM) season. Smoke from extensive biomass burning throughout the Maritime Continent advected into this region during the SWM, where it was mixed with anthropogenic continental pollution and emissions from heavy shipping activities. Eight aerosol types were identified using a k-means cluster analysis with data from a size-resolved CCN characterization system. Interpretation of the clusters was supplemented by additional onboard aerosol and meteorological measurements, satellite, and model products for the region. A typical bimodal marine boundary layer background aerosol population was identified and observed mixing with accumulation mode aerosol from other sources, primarily smoke from fires in Borneo and Sumatra. Hygroscopicity was assessed using the kappa parameter and was found to average 0.40 for samples dominated by aged accumulation mode smoke; 0.65 for accumulation mode marine aerosol; 0.60 in an anthropogenic aerosol plume; and 0.22 during a short period that was characterized by elevated levels of volatile organic compounds not associated with biomass burning impacts. As a special subset of the background marine aerosol, clean air masses substantially scrubbed of particles were observed following heavy precipitation or the passage of squall lines, with changes in observed aerosol properties occurring on the order of minutes. Average CN number concentrations, size distributions, and kappa values are reported for each population type, along with CCN number concentrations for particles that activated at supersaturations between 0.14 and 0.85%.

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