Measurements of the Aerosol Size Distribution to Investigate Aerosol Nucleation and Initial Growth During the GoAmazon 2014/5 Campaign

 

Authors

Jian Wang — Washington University in St. Louis
Scot T. Martin — Harvard University
James Smith — University of California, Irvine
Chongai Kuang — Brookhaven National Laboratory
Markku Kulmala — University of Helsinki
Rodrigo Augusto Souza — Universidade do Estado do Amazonas
Tuukka Taneli Petaja — University of Helsinki
Saewung Kim — University of California, Irvine
Roger Seco — University of California Irvine
John Carl Gustav Backman — University of Helsinki
Paulo Artaxo — University of Sao Paulo

Category

New Particle Formation

Description

Atmospheric particle nucleation is an important environmental nano-scale process, with field measurements and modeling studies indicating that freshly nucleated particles are a significant source of global cloud condensation nuclei. However, our understanding of atmospheric nucleation and its influence on climate is limited as few ambient measurements have been made of either the nucleation rate (at 1 nm) or the initial growth rate of newly formed clusters (from 1 to 3 nm), both of which are necessary to constrain and investigate the nucleation mechanism and to develop process-level models. Aerosol nucleation and initial growth were investigated during the Green Ocean Amazon (GoAmazon) campaign spanning the wet and dry seasons of 2014 downwind of the city of Manaus, Brazil. Aerosol measurement was accomplished through the deployment of a condensation particle counter-based electrical mobility spectrometer, optimized for the detection of aerosol down to 1 nm in diameter. An electrometer-based neutral air ion spectrometer was also deployed at the same location to measure the neutral and charged fraction of aerosol down to 1.5 nm in diameter. From these size distribution measurements, periods of particle formation and growth were identified, and the resulting formation rates and growth rates were estimated. Concurrent and co-located measurements of gas-phase sulfuric acid provided the opportunity to investigate the functional contribution of sulfuric acid to the observed formation and growth rates.