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Elemental composition of fog interstitial particle size fractions and hydrophobic fractions related to fog droplet nucleation scavenging

Martinsson, Bengt G. LU ; Swietlicki, Erik LU orcid ; Hansson, Hans-Christen ; Wiedensohler, Alfred ; Noone, Kevin J. ; Ogren, John A. and Hallberg, Anneli (1992) In Tellus. Series B: Chemical and Physical Meteorology 44(5). p.593-603
Abstract

The cloud nucleation scavenging process was studied during a joint campaign of the EUROTRAC sub‐project Ground‐based Cloud Experiment. It was found that the particle size has a strong influence on the partitioning of particles between the cloud droplet and the interstitial aerosol reservoirs. A new aerosol sampling unit, the relative humidity processing system, was employed for the extraction of particles with a low growth‐ability with respect to increased relative humidity. The system supplied tracer elements on the particle growth‐ability. These elements could be used to identify a factor related to particle hygroscopic properties, which was in effect as a selector of cloud condensation nuclei.

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author
; ; ; ; ; and
organization
publishing date
type
Contribution to journal
publication status
published
subject
in
Tellus. Series B: Chemical and Physical Meteorology
volume
44
issue
5
pages
11 pages
publisher
Taylor & Francis
external identifiers
  • scopus:84982733170
ISSN
0280-6509
DOI
10.1034/j.1600-0889.1992.t01-1-00012.x
language
English
LU publication?
yes
id
b7bc478d-a9fa-4cbb-90e2-ae15da7fa7ba
date added to LUP
2019-05-16 09:20:40
date last changed
2021-01-03 09:51:40
@article{b7bc478d-a9fa-4cbb-90e2-ae15da7fa7ba,
  abstract     = {{<p>The cloud nucleation scavenging process was studied during a joint campaign of the EUROTRAC sub‐project Ground‐based Cloud Experiment. It was found that the particle size has a strong influence on the partitioning of particles between the cloud droplet and the interstitial aerosol reservoirs. A new aerosol sampling unit, the relative humidity processing system, was employed for the extraction of particles with a low growth‐ability with respect to increased relative humidity. The system supplied tracer elements on the particle growth‐ability. These elements could be used to identify a factor related to particle hygroscopic properties, which was in effect as a selector of cloud condensation nuclei.</p>}},
  author       = {{Martinsson, Bengt G. and Swietlicki, Erik and Hansson, Hans-Christen and Wiedensohler, Alfred and Noone, Kevin J. and Ogren, John A. and Hallberg, Anneli}},
  issn         = {{0280-6509}},
  language     = {{eng}},
  number       = {{5}},
  pages        = {{593--603}},
  publisher    = {{Taylor & Francis}},
  series       = {{Tellus. Series B: Chemical and Physical Meteorology}},
  title        = {{Elemental composition of fog interstitial particle size fractions and hydrophobic fractions related to fog droplet nucleation scavenging}},
  url          = {{http://dx.doi.org/10.1034/j.1600-0889.1992.t01-1-00012.x}},
  doi          = {{10.1034/j.1600-0889.1992.t01-1-00012.x}},
  volume       = {{44}},
  year         = {{1992}},
}