Size-resolved aerosol and cloud condensation nuclei (CCN) properties in the remote marine South China Sea, Part 1: Observations and source classification — Samuel A. Atwood (2016) | RDL Network
Size-resolved aerosol and cloud condensation nuclei (CCN) properties in the remote marine South China Sea, Part 1: Observations and source classification
Preprint 2016 en
Authors
SA
Samuel A. Atwood
JR
Jeffrey S. Reid
SK
Sonia M. Kreidenweis
Abstract
1 min read
Abstract. Ship-based measurements of aerosol and cloud condensation nuclei (CCN) properties are presented for two 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, additional onboard aerosol and meteorological measurements, and satellite and model products for the region. A typical bimodal marine boundary layer background aerosol population was identified that was observed mixing with accumulation mode aerosol from other sources, primarily smoke from fires in Borneo and Sumatra. Hygroscopicity was assessed using the 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 values are reported for each population type, along with CCN number concentrations for particles that activated at supersaturations between 0.14 % and 0.85 %.
Samuel A. Atwood, Jeffrey S. Reid, Sonia M. Kreidenweis, Donald R Blake, Haflidi H. Jonsson, Nofel Lagrosas, Peng Xian, Elizabeth A. Reid, W. R. Sessions, James Bernard Simpas
Samuel A. Atwood, Jeffrey S. Reid, Sonia M. Kreidenweis, Donald R Blake, Haflidi H. Jonsson, Nofel Lagrosas, P. Lynch, Elizabeth A. Reid, W. R. Sessions, James Bernard Simpas
Jeffrey S. Reid, Nofel Lagrosas, Haflidi H. Jonsson, Elizabeth A. Reid, Samuel A. Atwood, Thomas J. Boyd, Virendra P. Ghate, Peng Xian, Derek J. Posselt, James Bernard Simpas, Sherdon Niño Uy, Kimo Zaiger, Donald R Blake, Anthony Bucholtz, James R. Campbell, Boon Ning Chew, Steven S. Cliff, B. N. Holben, Robert E. Holz, E. J. Hyer, Sonia M. Kreidenweis,
Jeffrey S. Reid, Nofel Lagrosas, Haflidi H. Jonsson, Elizabeth A. Reid, Samuel A. Atwood, Thomas J. Boyd, Virendra P. Ghate, P. Lynch, Derek J. Posselt, James Bernard Simpas, Sherdon Niño Uy, Kimo Zaiger, Donald R Blake, Anthony Bucholtz, James R. Campbell, Boon Ning Chew, Steven S. Cliff, B. N. Holben, Robert E. Holz, E. J. Hyer, Sonia M. Kreidenweis, Arunas P. Kuciaskas,
Gordon A. Novak, Charles H. Fite, Christopher D. Holmes, Patrick R. Veres, J. A. Neuman, I. C. Faloona, Joel A. Thornton, Glenn M. Wolfe, Michael P. Vermeuel, Christopher M. Jernigan, Jeff Peischl, Thomas B. Ryerson, Chelsea R. Thompson, Ilann Bourgeois, C. Warneke, Georgios I. Gkatzelis, Matthew M. Coggon, Kanako Sekimoto, T. P. Bui, Jonathan M. Dean‐Day, Glenn S. Diskin, Joshua P. DiGangi, ,
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