Ice nucleating particles at a coastal marine boundary layer site: correlations with aerosol type and meteorological conditions

Information on what aerosol particle types are the major sources of ice nucleating particles (INPs) in the atmosphere is needed for climate predictions. To determine which aerosol particles are the major sources of immersion-mode INPs at a coastal site in Western Canada, we investigated correlations...

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Main Authors: R. H. Mason, M. Si, J. Li, C. Chou, R. Dickie, D. Toom-Sauntry, C. Pöhlker, J. D. Yakobi-Hancock, L. A. Ladino, K. Jones, W. R. Leaitch, C. L. Schiller, J. P. D. Abbatt, J. A. Huffman, A. K. Bertram
Format: Article
Language:English
Published: Copernicus Publications 2015-11-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/15/12547/2015/acp-15-12547-2015.pdf
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author R. H. Mason
M. Si
J. Li
C. Chou
R. Dickie
D. Toom-Sauntry
C. Pöhlker
J. D. Yakobi-Hancock
L. A. Ladino
K. Jones
W. R. Leaitch
C. L. Schiller
J. P. D. Abbatt
J. A. Huffman
A. K. Bertram
author_facet R. H. Mason
M. Si
J. Li
C. Chou
R. Dickie
D. Toom-Sauntry
C. Pöhlker
J. D. Yakobi-Hancock
L. A. Ladino
K. Jones
W. R. Leaitch
C. L. Schiller
J. P. D. Abbatt
J. A. Huffman
A. K. Bertram
author_sort R. H. Mason
collection DOAJ
description Information on what aerosol particle types are the major sources of ice nucleating particles (INPs) in the atmosphere is needed for climate predictions. To determine which aerosol particles are the major sources of immersion-mode INPs at a coastal site in Western Canada, we investigated correlations between INP number concentrations and both concentrations of different atmospheric particles and meteorological conditions. We show that INP number concentrations are strongly correlated with the number concentrations of fluorescent bioparticles between −15 and −25 °C, and that the size distribution of INPs is most consistent with the size distribution of fluorescent bioparticles. We conclude that biological particles were likely the major source of ice nuclei at freezing temperatures between −15 and −25 °C at this site for the time period studied. At −30 °C, INP number concentrations are also well correlated with number concentrations of the total aerosol particles ≥ 0.5 μm, suggesting that non-biological particles may have an important contribution to the population of INPs active at this temperature. As we found that black carbon particles were unlikely to be a major source of ice nuclei during this study, these non-biological INPs may include mineral dust. Furthermore, correlations involving chemical tracers of marine aerosols and marine biological activity, sodium and methanesulfonic acid, indicate that the majority of INPs measured at the coastal site likely originated from terrestrial rather than marine sources. Finally, six existing empirical parameterizations of ice nucleation were tested to determine if they accurately predict the measured INP number concentrations. We found that none of the parameterizations selected are capable of predicting INP number concentrations with high accuracy over the entire temperature range investigated. This finding illustrates that additional measurements are needed to improve parameterizations of INPs and their subsequent climatic impacts.
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spelling doaj.art-31d268147635417e945570790c203d572022-12-22T01:38:42ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242015-11-011521125471256610.5194/acp-15-12547-2015Ice nucleating particles at a coastal marine boundary layer site: correlations with aerosol type and meteorological conditionsR. H. Mason0M. Si1J. Li2C. Chou3R. Dickie4D. Toom-Sauntry5C. Pöhlker6J. D. Yakobi-Hancock7L. A. Ladino8K. Jones9W. R. Leaitch10C. L. Schiller11J. P. D. Abbatt12J. A. Huffman13A. K. Bertram14Department of Chemistry, University of British Columbia, Vancouver, BC, V6T1Z1, CanadaDepartment of Chemistry, University of British Columbia, Vancouver, BC, V6T1Z1, CanadaDepartment of Chemistry and Biochemistry, University of Denver, Denver, CO, 80208, USADepartment of Chemistry, University of British Columbia, Vancouver, BC, V6T1Z1, CanadaDepartment of Chemistry, University of British Columbia, Vancouver, BC, V6T1Z1, CanadaClimate Research Division, Environment Canada, Toronto, ON, M3H5T4, CanadaBiogeochemistry Department, Max Planck Institute of Chemistry, Mainz, 55020, GermanyDepartment of Chemistry, University of Toronto, Toronto, ON, M5S3H6, CanadaDepartment of Chemistry, University of Toronto, Toronto, ON, M5S3H6, CanadaAir Quality Science Unit, Environment Canada, Vancouver, BC, V6C3S5, CanadaClimate Research Division, Environment Canada, Toronto, ON, M3H5T4, CanadaAir Quality Science Unit, Environment Canada, Vancouver, BC, V6C3S5, CanadaDepartment of Chemistry, University of Toronto, Toronto, ON, M5S3H6, CanadaDepartment of Chemistry and Biochemistry, University of Denver, Denver, CO, 80208, USADepartment of Chemistry, University of British Columbia, Vancouver, BC, V6T1Z1, CanadaInformation on what aerosol particle types are the major sources of ice nucleating particles (INPs) in the atmosphere is needed for climate predictions. To determine which aerosol particles are the major sources of immersion-mode INPs at a coastal site in Western Canada, we investigated correlations between INP number concentrations and both concentrations of different atmospheric particles and meteorological conditions. We show that INP number concentrations are strongly correlated with the number concentrations of fluorescent bioparticles between −15 and −25 °C, and that the size distribution of INPs is most consistent with the size distribution of fluorescent bioparticles. We conclude that biological particles were likely the major source of ice nuclei at freezing temperatures between −15 and −25 °C at this site for the time period studied. At −30 °C, INP number concentrations are also well correlated with number concentrations of the total aerosol particles ≥ 0.5 μm, suggesting that non-biological particles may have an important contribution to the population of INPs active at this temperature. As we found that black carbon particles were unlikely to be a major source of ice nuclei during this study, these non-biological INPs may include mineral dust. Furthermore, correlations involving chemical tracers of marine aerosols and marine biological activity, sodium and methanesulfonic acid, indicate that the majority of INPs measured at the coastal site likely originated from terrestrial rather than marine sources. Finally, six existing empirical parameterizations of ice nucleation were tested to determine if they accurately predict the measured INP number concentrations. We found that none of the parameterizations selected are capable of predicting INP number concentrations with high accuracy over the entire temperature range investigated. This finding illustrates that additional measurements are needed to improve parameterizations of INPs and their subsequent climatic impacts.http://www.atmos-chem-phys.net/15/12547/2015/acp-15-12547-2015.pdf
spellingShingle R. H. Mason
M. Si
J. Li
C. Chou
R. Dickie
D. Toom-Sauntry
C. Pöhlker
J. D. Yakobi-Hancock
L. A. Ladino
K. Jones
W. R. Leaitch
C. L. Schiller
J. P. D. Abbatt
J. A. Huffman
A. K. Bertram
Ice nucleating particles at a coastal marine boundary layer site: correlations with aerosol type and meteorological conditions
Atmospheric Chemistry and Physics
title Ice nucleating particles at a coastal marine boundary layer site: correlations with aerosol type and meteorological conditions
title_full Ice nucleating particles at a coastal marine boundary layer site: correlations with aerosol type and meteorological conditions
title_fullStr Ice nucleating particles at a coastal marine boundary layer site: correlations with aerosol type and meteorological conditions
title_full_unstemmed Ice nucleating particles at a coastal marine boundary layer site: correlations with aerosol type and meteorological conditions
title_short Ice nucleating particles at a coastal marine boundary layer site: correlations with aerosol type and meteorological conditions
title_sort ice nucleating particles at a coastal marine boundary layer site correlations with aerosol type and meteorological conditions
url http://www.atmos-chem-phys.net/15/12547/2015/acp-15-12547-2015.pdf
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