Estimating nucleation rates from apparent particle formation rates and vice versa: Revised formulation of the Kerminen–Kulmala equation

By K. Lehtinen, Miikka Dal Maso, Markku Kulmala, V. Kerminen. 2007

209 citations recorded by the source corpus.

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

View Paper: https://www.semanticscholar.org/paper/ac9f00aae80aa4440f84ca2de6bbb17929142212

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Citations in the corpus

Cloud condensation nuclei production associated with atmospheric nucleation: a synthesis based on existing literature and new results (2012, methodology): “An updated version of this formula was introduced later by Lehtinen et al. (2007).”
The role of relative humidity in continental new particle formation (2011, background): “The following equation [Lehtinen et al., 2007] describes the connection between the actual nucleation rate at 1.”
Determination of cloud condensation nuclei production from measured new particle formation events (2009, methodology): “... deplete n y , and Fcoag is a source term representing all collisions of smaller particles that yield larger particles with sizes equal to the diameter trajectory Dp . To determine the size distribution for 100 nm particles (n y = n100), equation (3) is evaluated at a time t along the diameter tr”
Sub-10 nm particle growth by vapor condensation – effects of vapor molecule size and particle thermal speed (2010, background): “Finally, for global modelling purposes, if semi-empirical particle formation rates are sought after, accurate and consistent ways to estimate growth rates and times are crucial since formation rates depend strongly on growth rates (Lehtinen et al., 2007).”
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).”