Observations of atmospheric chemical deposition to high Arctic snow

Rapidly rising temperatures and loss of snow and ice cover have demonstrated the unique vulnerability of the high Arctic to climate change. There are major uncertainties in modelling the chemical depositional and scavenging processes of Arctic snow. To that end, fresh snow samples collected on avera...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Macdonald, Katrina M., Sharma, Sangeeta, Toom, Desiree, Chivulescu, Alina, Hanna, Sarah, Bertram, Allan K., Platt, Andrew, Elsasser, Mike, Huang, Lin, Tarasick, David, Chellman, Nathan, McConnell, Joseph R., Bozem, Heiko, Kunkel, Daniel, Lei, Ying Duan, Evans, Greg J., Abbatt, Jonathan P. D.
Format: Article in Journal/Newspaper
Language:English
Published: European Geosciences Union 2017
Subjects:
Online Access:http://hdl.handle.net/1807/87374
https://doi.org/10.5194/acp-17-5775-2017
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spelling ftunivtoronto:oai:localhost:1807/87374 2023-05-15T14:27:08+02:00 Observations of atmospheric chemical deposition to high Arctic snow Macdonald, Katrina M. Sharma, Sangeeta Toom, Desiree Chivulescu, Alina Hanna, Sarah Bertram, Allan K. Platt, Andrew Elsasser, Mike Huang, Lin Tarasick, David Chellman, Nathan McConnell, Joseph R. Bozem, Heiko Kunkel, Daniel Lei, Ying Duan Evans, Greg J. Abbatt, Jonathan P. D. 2017-05-10 http://hdl.handle.net/1807/87374 https://doi.org/10.5194/acp-17-5775-2017 en_ca eng European Geosciences Union Macdonald K.M., S. Sharma, D. Toom, A. Chivulescu, S. Hanna, A. Bertram, A. Platt, M. Elsasser, L. Huang, N. Chellman, J. R. McConnell, H. Bozem, D. Kunkel, Y. D. Lei, G. J. Evans, J. P. D. Abbatt “Observations of Atmospheric Chemical Deposition to High Arctic Snow” Atm. Chem. and Phys. 17, 5775-5788, doi:10.5194/acp-2016-944, 2017. 1680-7324 http://hdl.handle.net/1807/87374 doi:10.5194/acp-17-5775-2017 Attribution 4.0 International http://creativecommons.org/licenses/by/4.0/ CC-BY Article 2017 ftunivtoronto https://doi.org/10.5194/acp-17-5775-2017 https://doi.org/10.5194/acp-2016-944 2020-06-17T12:16:41Z Rapidly rising temperatures and loss of snow and ice cover have demonstrated the unique vulnerability of the high Arctic to climate change. There are major uncertainties in modelling the chemical depositional and scavenging processes of Arctic snow. To that end, fresh snow samples collected on average every 4 days at Alert, Nunavut, from September 2014 to June 2015 were analyzed for black carbon, major ions, and metals, and their concentrations and fluxes were reported. Comparison with simultaneous measurements of atmospheric aerosol mass loadings yields effective deposition velocities that encompass all processes by which the atmospheric species are transferred to the snow. It is inferred from these values that dry deposition is the dominant removal mechanism for several compounds over the winter while wet deposition increased in importance in the fall and spring, possibly due to enhanced scavenging by mixed-phase clouds. Black carbon aerosol was the least effi- ciently deposited species to the snow. Funding of this study was provided as part of the Network on Climate and Aerosols Research (NETCARE), Natural Science and Engineering Research Council of Canada (NSERC), the government of Ontario through the Ontario Graduate Scholarship (OGS), and Environment and Climate Change Canada. This project would not have been possible without the collaboration of many skilled individuals: Richard Leaitch at Environment Canada and Catherine Philips-Smith and Cheol-Heon Jeong at the University of Toronto. Article in Journal/Newspaper Arctic Arctic black carbon Climate change Nunavut University of Toronto: Research Repository T-Space Arctic Canada Nunavut Atmospheric Chemistry and Physics 17 9 5775 5788
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language English
description Rapidly rising temperatures and loss of snow and ice cover have demonstrated the unique vulnerability of the high Arctic to climate change. There are major uncertainties in modelling the chemical depositional and scavenging processes of Arctic snow. To that end, fresh snow samples collected on average every 4 days at Alert, Nunavut, from September 2014 to June 2015 were analyzed for black carbon, major ions, and metals, and their concentrations and fluxes were reported. Comparison with simultaneous measurements of atmospheric aerosol mass loadings yields effective deposition velocities that encompass all processes by which the atmospheric species are transferred to the snow. It is inferred from these values that dry deposition is the dominant removal mechanism for several compounds over the winter while wet deposition increased in importance in the fall and spring, possibly due to enhanced scavenging by mixed-phase clouds. Black carbon aerosol was the least effi- ciently deposited species to the snow. Funding of this study was provided as part of the Network on Climate and Aerosols Research (NETCARE), Natural Science and Engineering Research Council of Canada (NSERC), the government of Ontario through the Ontario Graduate Scholarship (OGS), and Environment and Climate Change Canada. This project would not have been possible without the collaboration of many skilled individuals: Richard Leaitch at Environment Canada and Catherine Philips-Smith and Cheol-Heon Jeong at the University of Toronto.
format Article in Journal/Newspaper
author Macdonald, Katrina M.
Sharma, Sangeeta
Toom, Desiree
Chivulescu, Alina
Hanna, Sarah
Bertram, Allan K.
Platt, Andrew
Elsasser, Mike
Huang, Lin
Tarasick, David
Chellman, Nathan
McConnell, Joseph R.
Bozem, Heiko
Kunkel, Daniel
Lei, Ying Duan
Evans, Greg J.
Abbatt, Jonathan P. D.
spellingShingle Macdonald, Katrina M.
Sharma, Sangeeta
Toom, Desiree
Chivulescu, Alina
Hanna, Sarah
Bertram, Allan K.
Platt, Andrew
Elsasser, Mike
Huang, Lin
Tarasick, David
Chellman, Nathan
McConnell, Joseph R.
Bozem, Heiko
Kunkel, Daniel
Lei, Ying Duan
Evans, Greg J.
Abbatt, Jonathan P. D.
Observations of atmospheric chemical deposition to high Arctic snow
author_facet Macdonald, Katrina M.
Sharma, Sangeeta
Toom, Desiree
Chivulescu, Alina
Hanna, Sarah
Bertram, Allan K.
Platt, Andrew
Elsasser, Mike
Huang, Lin
Tarasick, David
Chellman, Nathan
McConnell, Joseph R.
Bozem, Heiko
Kunkel, Daniel
Lei, Ying Duan
Evans, Greg J.
Abbatt, Jonathan P. D.
author_sort Macdonald, Katrina M.
title Observations of atmospheric chemical deposition to high Arctic snow
title_short Observations of atmospheric chemical deposition to high Arctic snow
title_full Observations of atmospheric chemical deposition to high Arctic snow
title_fullStr Observations of atmospheric chemical deposition to high Arctic snow
title_full_unstemmed Observations of atmospheric chemical deposition to high Arctic snow
title_sort observations of atmospheric chemical deposition to high arctic snow
publisher European Geosciences Union
publishDate 2017
url http://hdl.handle.net/1807/87374
https://doi.org/10.5194/acp-17-5775-2017
geographic Arctic
Canada
Nunavut
geographic_facet Arctic
Canada
Nunavut
genre Arctic
Arctic
black carbon
Climate change
Nunavut
genre_facet Arctic
Arctic
black carbon
Climate change
Nunavut
op_relation Macdonald K.M., S. Sharma, D. Toom, A. Chivulescu, S. Hanna, A. Bertram, A. Platt, M. Elsasser, L. Huang, N. Chellman, J. R. McConnell, H. Bozem, D. Kunkel, Y. D. Lei, G. J. Evans, J. P. D. Abbatt “Observations of Atmospheric Chemical Deposition to High Arctic Snow” Atm. Chem. and Phys. 17, 5775-5788, doi:10.5194/acp-2016-944, 2017.
1680-7324
http://hdl.handle.net/1807/87374
doi:10.5194/acp-17-5775-2017
op_rights Attribution 4.0 International
http://creativecommons.org/licenses/by/4.0/
op_rightsnorm CC-BY
op_doi https://doi.org/10.5194/acp-17-5775-2017
https://doi.org/10.5194/acp-2016-944
container_title Atmospheric Chemistry and Physics
container_volume 17
container_issue 9
container_start_page 5775
op_container_end_page 5788
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