Importance of submicron surface‐active organic aerosols for pristine Arctic clouds

ABSTRACT Recent results from summer measurement campaigns over the partly ice covered central Arctic Ocean show that the high Arctic aerosol has a larger organic fraction than previously thought. We use a Lagrangian parcel model to infer the properties of the unexplained organic aerosol fraction tha...

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Bibliographic Details
Published inTellus. Series B, Chemical and physical meteorology Vol. 57; no. 3; pp. 261 - 268
Main Authors LOHMANN, ULRIKE, LECK, CAROLINE
Format Journal Article
LanguageEnglish
Published Oxford, UK Blackwell Publishing Ltd 01.07.2005
Blackwell
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Summary:ABSTRACT Recent results from summer measurement campaigns over the partly ice covered central Arctic Ocean show that the high Arctic aerosol has a larger organic fraction than previously thought. We use a Lagrangian parcel model to infer the properties of the unexplained organic aerosol fraction that is necessary for reproducing the observed concentrations of cloud condensation nuclei (CCN). With increasing distance from the open ocean a highly surface‐active Aitken mode, associated with particles found in the open lead surface microlayer, becomes increasingly important for cloud droplet formation. The presence of such an Aitken mode population increases the high Arctic indirect aerosol effect (added cooling) relative to just a marine source of CCN from oxidation products of dimethyl sulfide (DMS) released from phytoplankton.
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ISSN:0280-6509
1600-0889
DOI:10.1111/j.1600-0889.2005.00144.x