Highly Hygroscopic Aerosols Facilitate Summer and Early-Autumn Cloud Formation at Extremely Low Concentrations Over the Central Arctic Ocean
(2024) In Journal of Geophysical Research: Atmospheres 129(2).- Abstract
Arctic clouds are sensitive to atmospheric particles since these are sometimes in such low concentrations that clouds cannot always form under supersaturated water vapor conditions. This is especially true in the late summer, when aerosol concentrations are generally very low in the high Arctic. The environment changes rapidly around freeze-up as the open waters close and snow starts accumulating on ice. We investigated droplet formation during eight significant fog events in the central Arctic Ocean, north of 80°, from August 12 to 19 September 2018 during the Arctic Ocean 2018 expedition onboard the icebreaker Oden. Calculated hygroscopicity parameters (κ) for the entire study were very high (up to κ = 0.85 ± 0.13), notably after... (More)
Arctic clouds are sensitive to atmospheric particles since these are sometimes in such low concentrations that clouds cannot always form under supersaturated water vapor conditions. This is especially true in the late summer, when aerosol concentrations are generally very low in the high Arctic. The environment changes rapidly around freeze-up as the open waters close and snow starts accumulating on ice. We investigated droplet formation during eight significant fog events in the central Arctic Ocean, north of 80°, from August 12 to 19 September 2018 during the Arctic Ocean 2018 expedition onboard the icebreaker Oden. Calculated hygroscopicity parameters (κ) for the entire study were very high (up to κ = 0.85 ± 0.13), notably after freeze-up, suggesting that atmospheric particles were very cloud condensation nuclei (CCN)-active. At least one of the events showed that surface clouds were able to form and persist for at least a couple hours at aerosol concentrations less than 10 cm−3, which was previously suggested to be the minimum for cloud formation. Among these events that were considered limited in CCN, effective radii were generally larger than in the high CCN cases. In some of the fog events, droplet residuals particles did not reactivate under supersaturations up to 0.95%, suggesting either in-droplet reactions decreased hygroscopicity, or an ambient supersaturation above 1%. These results provide insight into droplet formation during the clean late-summer and fall of the high Arctic with limited influence from continental sources.
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- author
- Duplessis, P. ; Karlsson, L. ; Baccarini, A. ; Wheeler, M. ; Leaitch, W. R. ; Svenningsson, B. LU ; Leck, C. ; Schmale, J. ; Zieger, P. and Chang, R. Y.W.
- organization
- publishing date
- 2024-01-28
- type
- Contribution to journal
- publication status
- published
- subject
- keywords
- aerosol hygroscopicity, aerosol-cloud interactions, Arctic aerosols, cloud condensation nuclei, fog, Groundbased counterflow virtual impactor
- in
- Journal of Geophysical Research: Atmospheres
- volume
- 129
- issue
- 2
- article number
- e2023JD039159
- publisher
- Wiley-Blackwell
- external identifiers
-
- scopus:85182464862
- ISSN
- 2169-897X
- DOI
- 10.1029/2023JD039159
- language
- English
- LU publication?
- yes
- id
- 870c30c6-f186-406a-8030-97a601050d0c
- date added to LUP
- 2024-03-01 14:03:56
- date last changed
- 2024-03-01 14:05:21
@article{870c30c6-f186-406a-8030-97a601050d0c,
abstract = {{<p>Arctic clouds are sensitive to atmospheric particles since these are sometimes in such low concentrations that clouds cannot always form under supersaturated water vapor conditions. This is especially true in the late summer, when aerosol concentrations are generally very low in the high Arctic. The environment changes rapidly around freeze-up as the open waters close and snow starts accumulating on ice. We investigated droplet formation during eight significant fog events in the central Arctic Ocean, north of 80°, from August 12 to 19 September 2018 during the Arctic Ocean 2018 expedition onboard the icebreaker Oden. Calculated hygroscopicity parameters (κ) for the entire study were very high (up to κ = 0.85 ± 0.13), notably after freeze-up, suggesting that atmospheric particles were very cloud condensation nuclei (CCN)-active. At least one of the events showed that surface clouds were able to form and persist for at least a couple hours at aerosol concentrations less than 10 cm<sup>−3</sup>, which was previously suggested to be the minimum for cloud formation. Among these events that were considered limited in CCN, effective radii were generally larger than in the high CCN cases. In some of the fog events, droplet residuals particles did not reactivate under supersaturations up to 0.95%, suggesting either in-droplet reactions decreased hygroscopicity, or an ambient supersaturation above 1%. These results provide insight into droplet formation during the clean late-summer and fall of the high Arctic with limited influence from continental sources.</p>}},
author = {{Duplessis, P. and Karlsson, L. and Baccarini, A. and Wheeler, M. and Leaitch, W. R. and Svenningsson, B. and Leck, C. and Schmale, J. and Zieger, P. and Chang, R. Y.W.}},
issn = {{2169-897X}},
keywords = {{aerosol hygroscopicity; aerosol-cloud interactions; Arctic aerosols; cloud condensation nuclei; fog; Groundbased counterflow virtual impactor}},
language = {{eng}},
month = {{01}},
number = {{2}},
publisher = {{Wiley-Blackwell}},
series = {{Journal of Geophysical Research: Atmospheres}},
title = {{Highly Hygroscopic Aerosols Facilitate Summer and Early-Autumn Cloud Formation at Extremely Low Concentrations Over the Central Arctic Ocean}},
url = {{http://dx.doi.org/10.1029/2023JD039159}},
doi = {{10.1029/2023JD039159}},
volume = {{129}},
year = {{2024}},
}