High number concentrations of transparent exopolymer particles in ambient aerosol particles and cloud water – a case study at the tropical Atlantic Ocean
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Published:2022-05-02
Issue:8
Volume:22
Page:5725-5742
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
van Pinxteren ManuelaORCID, Robinson Tiera-Brandy, Zeppenfeld Sebastian, Gong XiandaORCID, Bahlmann Enno, Fomba Khanneh Wadinga, Triesch Nadja, Stratmann Frank, Wurl Oliver, Engel AnjaORCID, Wex HeikeORCID, Herrmann HartmutORCID
Abstract
Abstract. Transparent exopolymer particles (TEPs) exhibit the properties of gels and
are ubiquitously found in the world oceans. TEPs may enter the
atmosphere as part of sea-spray aerosol. Here, we report number concentrations of TEPs with a diameter > 4.5 µm, hence covering a part of the supermicron particle range, in ambient aerosol and
cloud water samples from the tropical Atlantic Ocean as well as in generated aerosol particles using a plunging waterfall tank that was filled with the ambient seawater. The ambient TEP concentrations ranged between 7×102 and 3×104 #TEP m−3 in the aerosol particles and correlations with sodium (Na+) and calcium (Ca2+) (R2=0.5) suggested some contribution via bubble bursting. Cloud water TEP concentrations were between 4×106 and 9×106 #TEP L−1 and, according to the
measured cloud liquid water content, corresponding to equivalent air
concentrations of 2–4×103 #TEP m−3. Based on Na+ concentrations in seawater and in the atmosphere, the enrichment factors for TEPs in the atmosphere were calculated. The tank-generated TEPs were enriched by a factor of 50 compared with seawater and, therefore, in-line with published enrichment factors for supermicron organic matter in general and TEPs specifically. TEP enrichment in the ambient atmosphere was on average 1×103 in cloud water and
9×103 in ambient aerosol particles and therefore about two orders of magnitude higher than the corresponding enrichment from the tank study. Such high enrichment of supermicron particulate organic constituents in the
atmosphere is uncommon and we propose that atmospheric TEP concentrations
resulted from a combination of enrichment during bubble bursting transfer
from the ocean and a secondary TEP in-situ formation in atmospheric phases.
Abiotic in-situ formation might have occurred from aqueous reactions of
dissolved organic precursors that were present in particle and cloud water
samples, whereas biotic formation involves bacteria, which were abundant in
the cloud water samples. The ambient TEP number concentrations were two orders of magnitude higher
than recently reported ice nucleating particle (INP) concentrations measured at the same location. As TEPs likely possess good properties to act as INPs, in future experiments it is worth studying if a certain part of TEPs
contributes a fraction of the biogenic INP population.
Funder
Leibniz-Institut für Troposphärenforschung
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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