Growth rates of freshly nucleated atmospheric particles in Atlanta

By M. Stolzenburg, P. Mcmurry, H. Sakurai, James N. Smith, R. Mauldin, F. Eisele, C. Clement. 2005

178 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Health, Toxicology and Mutagenesis

View Paper: https://www.semanticscholar.org/paper/14cd175d7eb78824f3e6a2c0b208826d0b1b0c00

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In Atmospheric Science

1. C. Kuang
2. P. Mcmurry
3. Markku Kulmala
4. A. Mccormick
5. V. Kerminen
6. K. Lehtinen
7. Tuomo Nieminen
8. J. Smith

In Global and Planetary Change

1. Markku Kulmala
2. C. Kuang
3. V. Kerminen
4. P. Mcmurry
5. K. Lehtinen
6. Tuomo Nieminen
7. A. Mccormick
8. I. Riipinen

In Health, Toxicology and Mutagenesis

1. Markku Kulmala
2. C. Kuang
3. P. Mcmurry
4. A. Mccormick
5. V. Kerminen
6. K. Lehtinen
7. I. Riipinen
8. J. Smith

Citations in the corpus

• Size and time-resolved growth rate measurements of 1 to 5 nm freshly formed atmospheric nuclei (2012, methodology): “2 % supersaturation) have frequently been made at both sites during the summer (Stolzenburg et al., 2005; Kuang et al., 2009).”
• An improved criterion for new particle formation in diverse atmospheric environments (2010, background): “agulation was observed in Atlanta (Stolzenburg et al., 2005) and Mexico City (Kuang et al.”
• Sub-10 nm particle growth by vapor condensation – effects of vapor molecule size and particle thermal speed (2010, background): “In situations of very high nucle- Correspondence to: T. Nieminen (tuomo.nieminen@helsinki.fi) ation mode particle concentrations also intramodal coagulation of the nucleated particles can contribute to the observed particle growth rates (Stolzenburg et al., 2005; Kulmala and Kerminen, 2008).”
• Aerosol size distribution measurements at four Nordic field stations: identification, analysis and trajectory analysis of new particle formation bursts (2007, result): “The growth and formation rates obtained agree well with other observations found in the literature (see for example Kulmala et al. (2004a), Stolzenburg et al. (2005)).”
• Determination of cloud condensation nuclei production from measured new particle formation events (2009, background): “formed particles grow, they undergo processes that enhance and deplete the growing population, such as coagulation production and scavenging by the pre-existing aerosol, respectively [Stolzenburg et al., 2005].”
• A criterion for new particle formation in the sulfur-rich Atlanta atmosphere (2005, result): “Our analyses suggest that in Atlanta, nanoparticle growth can often be explained by the condensation of sulfuric acid and its associated ammonia [Stolzenburg et al., 2005], a result that is consistent with our independent observations that freshly nucleated nanoparticles were composed mostly of ammo”
• Dependence of nucleation rates on sulfuric acid vapor concentration in diverse atmospheric locations (2008, unknown): “by Stolzenburg et al. [2005]. D10209 KUANG ET AL.”