A criterion for new particle formation in the sulfur-rich Atlanta atmosphere

By P. Mcmurry, Melissa A. Fink, H. Sakurai, M. Stolzenburg, R. Mauldin, J. Smith, F. Eisele, K. Moore, S. Sjostedt, D. Tanner and 4 more. 2005

230 citations recorded by the source corpus.

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

View Paper: https://www.semanticscholar.org/paper/4ce7354298c615c08fe5038340a7f38bd82455b1

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

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

In Global and Planetary Change

1. C. Kuang
2. Markku Kulmala
3. P. Mcmurry
4. V. Kerminen
5. Tuukka Petäjä
6. A. Mccormick
7. I. Riipinen
8. Xuemeng Chen

In Health, Toxicology and Mutagenesis

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

Citations in the corpus

• Dependence of nucleation rates on sulfuric acid vapor concentration in diverse atmospheric locations (2008, methodology): “The analyses of Sihto et al. [2006] and Riipinen et al. [2007] use a similar expression connecting J1 and J3 [K nandKulmala,2002]inwhich thequantityCS’ behaves analogously asAFuchs.Ourre-analysis oftheirpublishedresultsmakesuseofthefollowingrelationship between CS’andAFuchs as described by McMurry ”
• Atmospheric new particle formation and growth: review of field observations (2018, methodology): “Based on the pioneering theoretical work by McMurry and Friedlander (1979) andMcMurry (1983),McMurry et al (2005) developed a parameter ‘L’ to distinguish the days with NPF from those without NPF in a sulfur-rich environment.”
• Size and time-resolved growth rate measurements of 1 to 5 nm freshly formed atmospheric nuclei (2012, background): “This probability is usually parameterized assuming a constant growth rate as the nucleated particles grow to 3 nm (Weber et al., 1997; Kerminen and Kulmala, 2002; McMurry et al., 2005; Lehtinen et al., 2007).”
• Aerosol size distribution measurements at four Nordic field stations: identification, analysis and trajectory analysis of new particle formation bursts (2007, background): “This has prompted increasing activity in this field of study, both in trying to understand the physical and chemical pathways causing the formation of new particles (Kulmala et al., 2000, 2004b; McMurry et al., 2005), and assessing the climatic importance of the particles formed (see for example Kur”