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On the derivation of particle nucleation rates from experimental formation rates
Atmospheric particle formation rates are usually measured at sizes larger than the critical size where nucleation occurs. Due to loss of particles during their growth to the detection threshold, the measured formation rate is often substantially smaller than the nucleation rate. For this reason a co...
| Autores principales: | , , , , |
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| Lenguaje: | eng |
| Publicado: |
2015
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| Materias: | |
| Acceso en línea: | https://dx.doi.org/10.5194/acpd-14-27233-2014 https://dx.doi.org/10.5194/acp-15-4063-2015 http://cds.cern.ch/record/1972023 |