Ice nucleating particles in the marine boundary layer in the Canadian Arctic during summer 2014

Ice nucleating particles (INPs) in the Arctic can influence climateand precipitation in the region; yet our understanding of the concentrations and sourcesof INPs in this region remain uncertain. In the following, we (1) measured concentrationsof INPs in the immersion mode in the Canadian Arctic mar...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Irish, Victoria E., Hanna, Sarah J., Willis, Megan D., China, Swarup, Thomas, Jennie L., Wentzell, Jeremy J. B., Cirisan, Ana, Si, Meng, Leaitch, W. Richard, Murphy, Jennifer G., Abbatt, Jonathan P. D., Laskin, Alexander, Girard, Eric, Bertram, Allan K.
Language:unknown
Published: 2023
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1501757
https://www.osti.gov/biblio/1501757
https://doi.org/10.5194/acp-19-1027-2019
id ftosti:oai:osti.gov:1501757
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spelling ftosti:oai:osti.gov:1501757 2023-07-30T04:01:10+02:00 Ice nucleating particles in the marine boundary layer in the Canadian Arctic during summer 2014 Irish, Victoria E. Hanna, Sarah J. Willis, Megan D. China, Swarup Thomas, Jennie L. Wentzell, Jeremy J. B. Cirisan, Ana Si, Meng Leaitch, W. Richard Murphy, Jennifer G. Abbatt, Jonathan P. D. Laskin, Alexander Girard, Eric Bertram, Allan K. 2023-06-29 application/pdf http://www.osti.gov/servlets/purl/1501757 https://www.osti.gov/biblio/1501757 https://doi.org/10.5194/acp-19-1027-2019 unknown http://www.osti.gov/servlets/purl/1501757 https://www.osti.gov/biblio/1501757 https://doi.org/10.5194/acp-19-1027-2019 doi:10.5194/acp-19-1027-2019 54 ENVIRONMENTAL SCIENCES 2023 ftosti https://doi.org/10.5194/acp-19-1027-2019 2023-07-11T09:32:03Z Ice nucleating particles (INPs) in the Arctic can influence climateand precipitation in the region; yet our understanding of the concentrations and sourcesof INPs in this region remain uncertain. In the following, we (1) measured concentrationsof INPs in the immersion mode in the Canadian Arctic marine boundary layer duringsummer 2014 on board the CCGS Amundsen , (2) determined ratios of surface areasof mineral dust aerosol to sea spray aerosol, and (3) investigated the source region ofthe INPs using particle dispersion modelling. Average concentrations of INPs at -15 , -20 , and -25 - C were 0.005, 0.044, and 0.154 L -1 ,respectively. These concentrations fall within the range of INP concentrations measuredin other marine environments. For the samples investigated the ratio of mineral dustsurface area to sea spray surface area ranged from 0.03 to 0.09. Based on these ratiosand the ice active surface site densities of mineral dust and sea spray aerosoldetermined in previous laboratory studies, our results suggest that mineral dust is amore important contributor to the INP population than sea spray aerosol for the samplesanalysed. Based on particle dispersion modelling, the highest concentrations of INPs wereoften associated with lower-latitude source regions such as the Hudson Bay area, easternGreenland, or north-western continental Canada. On the other hand, the lowestconcentrations were often associated with regions further north of the sampling sites andover Baffin Bay. A weak correlation was observed between INP concentrations and the timethe air mass spent over bare land, and a weak negative correlation was observed betweenINP concentrations and the time the air mass spent over ice and open water. Thesecombined results suggest that mineral dust from local sources is an important contributorto the INP population in the Canadian Arctic marine boundary layer during summer 2014. Other/Unknown Material Arctic Baffin Bay Baffin Bay Baffin Hudson Bay SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Arctic Hudson Bay Baffin Bay Canada Hudson Atmospheric Chemistry and Physics 19 2 1027 1039
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 54 ENVIRONMENTAL SCIENCES
spellingShingle 54 ENVIRONMENTAL SCIENCES
Irish, Victoria E.
Hanna, Sarah J.
Willis, Megan D.
China, Swarup
Thomas, Jennie L.
Wentzell, Jeremy J. B.
Cirisan, Ana
Si, Meng
Leaitch, W. Richard
Murphy, Jennifer G.
Abbatt, Jonathan P. D.
Laskin, Alexander
Girard, Eric
Bertram, Allan K.
Ice nucleating particles in the marine boundary layer in the Canadian Arctic during summer 2014
topic_facet 54 ENVIRONMENTAL SCIENCES
description Ice nucleating particles (INPs) in the Arctic can influence climateand precipitation in the region; yet our understanding of the concentrations and sourcesof INPs in this region remain uncertain. In the following, we (1) measured concentrationsof INPs in the immersion mode in the Canadian Arctic marine boundary layer duringsummer 2014 on board the CCGS Amundsen , (2) determined ratios of surface areasof mineral dust aerosol to sea spray aerosol, and (3) investigated the source region ofthe INPs using particle dispersion modelling. Average concentrations of INPs at -15 , -20 , and -25 - C were 0.005, 0.044, and 0.154 L -1 ,respectively. These concentrations fall within the range of INP concentrations measuredin other marine environments. For the samples investigated the ratio of mineral dustsurface area to sea spray surface area ranged from 0.03 to 0.09. Based on these ratiosand the ice active surface site densities of mineral dust and sea spray aerosoldetermined in previous laboratory studies, our results suggest that mineral dust is amore important contributor to the INP population than sea spray aerosol for the samplesanalysed. Based on particle dispersion modelling, the highest concentrations of INPs wereoften associated with lower-latitude source regions such as the Hudson Bay area, easternGreenland, or north-western continental Canada. On the other hand, the lowestconcentrations were often associated with regions further north of the sampling sites andover Baffin Bay. A weak correlation was observed between INP concentrations and the timethe air mass spent over bare land, and a weak negative correlation was observed betweenINP concentrations and the time the air mass spent over ice and open water. Thesecombined results suggest that mineral dust from local sources is an important contributorto the INP population in the Canadian Arctic marine boundary layer during summer 2014.
author Irish, Victoria E.
Hanna, Sarah J.
Willis, Megan D.
China, Swarup
Thomas, Jennie L.
Wentzell, Jeremy J. B.
Cirisan, Ana
Si, Meng
Leaitch, W. Richard
Murphy, Jennifer G.
Abbatt, Jonathan P. D.
Laskin, Alexander
Girard, Eric
Bertram, Allan K.
author_facet Irish, Victoria E.
Hanna, Sarah J.
Willis, Megan D.
China, Swarup
Thomas, Jennie L.
Wentzell, Jeremy J. B.
Cirisan, Ana
Si, Meng
Leaitch, W. Richard
Murphy, Jennifer G.
Abbatt, Jonathan P. D.
Laskin, Alexander
Girard, Eric
Bertram, Allan K.
author_sort Irish, Victoria E.
title Ice nucleating particles in the marine boundary layer in the Canadian Arctic during summer 2014
title_short Ice nucleating particles in the marine boundary layer in the Canadian Arctic during summer 2014
title_full Ice nucleating particles in the marine boundary layer in the Canadian Arctic during summer 2014
title_fullStr Ice nucleating particles in the marine boundary layer in the Canadian Arctic during summer 2014
title_full_unstemmed Ice nucleating particles in the marine boundary layer in the Canadian Arctic during summer 2014
title_sort ice nucleating particles in the marine boundary layer in the canadian arctic during summer 2014
publishDate 2023
url http://www.osti.gov/servlets/purl/1501757
https://www.osti.gov/biblio/1501757
https://doi.org/10.5194/acp-19-1027-2019
geographic Arctic
Hudson Bay
Baffin Bay
Canada
Hudson
geographic_facet Arctic
Hudson Bay
Baffin Bay
Canada
Hudson
genre Arctic
Baffin Bay
Baffin Bay
Baffin
Hudson Bay
genre_facet Arctic
Baffin Bay
Baffin Bay
Baffin
Hudson Bay
op_relation http://www.osti.gov/servlets/purl/1501757
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https://doi.org/10.5194/acp-19-1027-2019
doi:10.5194/acp-19-1027-2019
op_doi https://doi.org/10.5194/acp-19-1027-2019
container_title Atmospheric Chemistry and Physics
container_volume 19
container_issue 2
container_start_page 1027
op_container_end_page 1039
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