Wintertime Arctic Ocean sea water properties and primary marine aerosol concentrations

Sea spray aerosols are an important part of the climate system through their direct and indirect effects. Due to the diminishing sea ice, the Arctic Ocean is one of the most rapidly changing sea spray aerosol source areas. However, the influence of these changes on primary particle production is not...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Zábori, J., Krejci, R., Ekman, A. M. L., Mårtensson, E. M., Ström, J., Leeuw, G., Nilsson, E. D.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/acp-12-10405-2012
https://www.atmos-chem-phys.net/12/10405/2012/
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spelling ftcopernicus:oai:publications.copernicus.org:acp15516 2023-05-15T14:54:15+02:00 Wintertime Arctic Ocean sea water properties and primary marine aerosol concentrations Zábori, J. Krejci, R. Ekman, A. M. L. Mårtensson, E. M. Ström, J. Leeuw, G. Nilsson, E. D. 2018-01-15 application/pdf https://doi.org/10.5194/acp-12-10405-2012 https://www.atmos-chem-phys.net/12/10405/2012/ eng eng doi:10.5194/acp-12-10405-2012 https://www.atmos-chem-phys.net/12/10405/2012/ eISSN: 1680-7324 Text 2018 ftcopernicus https://doi.org/10.5194/acp-12-10405-2012 2019-12-24T09:55:45Z Sea spray aerosols are an important part of the climate system through their direct and indirect effects. Due to the diminishing sea ice, the Arctic Ocean is one of the most rapidly changing sea spray aerosol source areas. However, the influence of these changes on primary particle production is not known. In laboratory experiments we examined the influence of Arctic Ocean water temperature, salinity, and oxygen saturation on primary particle concentration characteristics. Sea water temperature was identified as the most important of these parameters. A strong decrease in sea spray aerosol production with increasing water temperature was observed for water temperatures between −1°C and 9°C. Aerosol number concentrations decreased from at least 1400 cm −3 to 350 cm −3 . In general, the aerosol number size distribution exhibited a robust shape with one mode close to dry diameter D p 0.2 μm with approximately 45% of particles at smaller sizes. Changes in sea water temperature did not result in pronounced change of the shape of the aerosol size distribution, only in the magnitude of the concentrations. Our experiments indicate that changes in aerosol emissions are most likely linked to changes of the physical properties of sea water at low temperatures. The observed strong dependence of sea spray aerosol concentrations on sea water temperature, with a large fraction of the emitted particles in the typical cloud condensation nuclei size range, provide strong arguments for a more careful consideration of this effect in climate models. Text Arctic Arctic Ocean Sea ice Copernicus Publications: E-Journals Arctic Arctic Ocean Atmospheric Chemistry and Physics 12 21 10405 10421
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language English
description Sea spray aerosols are an important part of the climate system through their direct and indirect effects. Due to the diminishing sea ice, the Arctic Ocean is one of the most rapidly changing sea spray aerosol source areas. However, the influence of these changes on primary particle production is not known. In laboratory experiments we examined the influence of Arctic Ocean water temperature, salinity, and oxygen saturation on primary particle concentration characteristics. Sea water temperature was identified as the most important of these parameters. A strong decrease in sea spray aerosol production with increasing water temperature was observed for water temperatures between −1°C and 9°C. Aerosol number concentrations decreased from at least 1400 cm −3 to 350 cm −3 . In general, the aerosol number size distribution exhibited a robust shape with one mode close to dry diameter D p 0.2 μm with approximately 45% of particles at smaller sizes. Changes in sea water temperature did not result in pronounced change of the shape of the aerosol size distribution, only in the magnitude of the concentrations. Our experiments indicate that changes in aerosol emissions are most likely linked to changes of the physical properties of sea water at low temperatures. The observed strong dependence of sea spray aerosol concentrations on sea water temperature, with a large fraction of the emitted particles in the typical cloud condensation nuclei size range, provide strong arguments for a more careful consideration of this effect in climate models.
format Text
author Zábori, J.
Krejci, R.
Ekman, A. M. L.
Mårtensson, E. M.
Ström, J.
Leeuw, G.
Nilsson, E. D.
spellingShingle Zábori, J.
Krejci, R.
Ekman, A. M. L.
Mårtensson, E. M.
Ström, J.
Leeuw, G.
Nilsson, E. D.
Wintertime Arctic Ocean sea water properties and primary marine aerosol concentrations
author_facet Zábori, J.
Krejci, R.
Ekman, A. M. L.
Mårtensson, E. M.
Ström, J.
Leeuw, G.
Nilsson, E. D.
author_sort Zábori, J.
title Wintertime Arctic Ocean sea water properties and primary marine aerosol concentrations
title_short Wintertime Arctic Ocean sea water properties and primary marine aerosol concentrations
title_full Wintertime Arctic Ocean sea water properties and primary marine aerosol concentrations
title_fullStr Wintertime Arctic Ocean sea water properties and primary marine aerosol concentrations
title_full_unstemmed Wintertime Arctic Ocean sea water properties and primary marine aerosol concentrations
title_sort wintertime arctic ocean sea water properties and primary marine aerosol concentrations
publishDate 2018
url https://doi.org/10.5194/acp-12-10405-2012
https://www.atmos-chem-phys.net/12/10405/2012/
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic Ocean
Sea ice
op_source eISSN: 1680-7324
op_relation doi:10.5194/acp-12-10405-2012
https://www.atmos-chem-phys.net/12/10405/2012/
op_doi https://doi.org/10.5194/acp-12-10405-2012
container_title Atmospheric Chemistry and Physics
container_volume 12
container_issue 21
container_start_page 10405
op_container_end_page 10421
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