Contribution of particle formation to global cloud condensation nuclei concentrations

By Dominick V. Spracklen, K. Carslaw, Markku Kulmala, V. Kerminen, Sanna‐Liisa Sihto, I. Riipinen, J. Merikanto, G. Mann, Martyn P. Chipperfield, A. Wiedensohler and 2 more. 2008

429 citations recorded by the source corpus.

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

View Paper: https://www.semanticscholar.org/paper/3d648541d21ceb4490d46fbf9026bed9efd27b85

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. G. Luo
2. Fangqun Yu
3. C. Kuang
4. K. Carslaw
5. Minghuai Wang
6. Jing Jiang
7. Modi Chen
8. M. Attoui

In Global and Planetary Change

1. G. Luo
2. Fangqun Yu
3. K. Carslaw
4. C. Kuang
5. Minghuai Wang
6. J. Smith
7. Steven J. Pickering
8. P. Mcmurry

In Health, Toxicology and Mutagenesis

1. C. Kuang
2. J. Smith
3. P. Mcmurry
4. G. Luo
5. J. Merikanto
6. J. Penner
7. Minghuai Wang
8. Fangqun Yu

Citations in the corpus

• Electrical Mobility Spectrometer Using a Diethylene Glycol Condensation Particle Counter for Measurement of Aerosol Size Distributions Down to 1 nm (2011, background): “Nucleation can lead to the widespread formation of new particles and the enhanced concentrations of cloud condensation nuclei (CCN) in the atmosphere (Spracklen et al. 2008; Chang et al. 2009; Kuang et al. 2009).”
• Size and time-resolved growth rate measurements of 1 to 5 nm freshly formed atmospheric nuclei (2012, background): “…first time, realistic growth rate inputs when modeling the nucleated particle survival probability in aerosol microphysical modules used in regional and chemical transport models (Pierce and Adams, 2007; Spracklen et al., 2008; Pierce and Adams, 2009; Wang and Penner, 2009; Spracklen et al., 2010).”
• Simulation of particle size distribution with a global aerosol model: contribution of nucleation to aerosol and CCN number concentrations (2009, methodology): “The global aerosol simulations reported in Spracklen et al. (2006, 2008), Makkonen et al. (2008), and Pierce and Adams (2009), based on an empirically parameterized activation-type nucleation mechanism (linear dependence of nucleation rateJ on sulfuric acid gas concentration:J=A [H2SO4] with A as…”
• Impact of nucleation on global CCN (2009, methodology): “But even with UTN the ground level CN concentrations in the model are often far less than observed (Spracklen et al., 2006, 2009), and BLN needs to be included to match the observations.”
• Aerosol indirect forcing in a global model with particle nucleation (2008, background): “Spracklen et al. (2005a, 2006) did not include any primary-emitted sulfate particles, while Stier et al. (2006), Pierce et al. (2007) and Spracklen et al. (2008) included these particles, but assumed different amounts and sizes for the emitted particulate sulfate.”