Organic aerosol formation via sulphate cluster activation
By Markku Kulmala, V. Kerminen, T. Anttila, Ari Laaksonen, C. O’Dowd. 2004
245 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/0d835f044baa10318c4452ea5c77067bda5cc336
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
- Markku Kulmala
- Tuukka Petäjä
- V. Kerminen
- Tuomo Nieminen
- K. Lehtinen
- I. Riipinen
- Heikki Lihavainen
- Lauri Laakso
In Global and Planetary Change
- Markku Kulmala
- V. Kerminen
- Tuomo Nieminen
- Tuukka Petäjä
- K. Lehtinen
- I. Riipinen
- Lauri Laakso
- J. Smith
Citations in the corpus
- Aerosol size distribution measurements at four Nordic field stations: identification, analysis and trajectory analysis of new particle formation bursts (2007, background): “Measurements of submicrometer aerosol size distributions have shown that new tropospheric aerosol formation and growth bursts are widespread, and at least at some sites a frequent phenomenon in the Earth’s atmosphere (Kulmala et al., 2004a).”
- Multicomponent aerosol dynamics model UHMA: model development and validation (2004, result): “Furthermore, its prediction of the organic volume fraction in newly formed particles, suggesting values as high as 0.5 for 3–4 nm particles and approximately 0.8 for 10 nm particles, agrees with recent indirect composition measurements.”
- Initial steps of aerosol growth (2004, unknown): “According to a recent overview (Kulmala et al., 2004a), the measured growth rate of nucleation mode particles is typically remarkably constant above the size of about 5–8 nm in particle diameter.”
- The role of relative humidity in continental new particle formation (2011, background): “…organics have not participated in the growth of the nuclei from 1 nm, it is likely that they start speeding up the growth at some later size when the Kelvin effect has decreased sufficiently, that is, with so‐called nano‐Köhler mechanisms or via heterogeneous nucleation [Kulmala et al., 2004b].”
- Annual and size dependent variation of growth rates and ion concentrations in boreal forest (2005, background): “The growth rate (GR) of particles and air ions can be estimated from size distribution measurements (Lehtinen and Kulmala 2003, Kulmala et al. 2004c).”