How relevant is the deposition of mercury onto snowpacks? – Part 2: A modeling study
An unknown fraction of mercury that is deposited onto snowpacks is revolatilized to the atmosphere. Determining the revolatilized fraction is important since mercury that enters the snowpack meltwater may be converted to highly toxic bioaccumulating methylmercury. In this study, we present a new dyn...
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Online Access: | https://doi.org/10.5194/acp-12-9251-2012 https://doaj.org/article/7af3436d586f41a4a6c6be5a35d34e46 |
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ftdoajarticles:oai:doaj.org/article:7af3436d586f41a4a6c6be5a35d34e46 2023-05-15T14:53:07+02:00 How relevant is the deposition of mercury onto snowpacks? – Part 2: A modeling study D. Durnford A. Dastoor A. Ryzhkov L. Poissant M. Pilote D. Figueras-Nieto 2012-10-01T00:00:00Z https://doi.org/10.5194/acp-12-9251-2012 https://doaj.org/article/7af3436d586f41a4a6c6be5a35d34e46 EN eng Copernicus Publications http://www.atmos-chem-phys.net/12/9251/2012/acp-12-9251-2012.pdf https://doaj.org/toc/1680-7316 https://doaj.org/toc/1680-7324 doi:10.5194/acp-12-9251-2012 1680-7316 1680-7324 https://doaj.org/article/7af3436d586f41a4a6c6be5a35d34e46 Atmospheric Chemistry and Physics, Vol 12, Iss 19, Pp 9251-9274 (2012) Physics QC1-999 Chemistry QD1-999 article 2012 ftdoajarticles https://doi.org/10.5194/acp-12-9251-2012 2022-12-31T02:11:56Z An unknown fraction of mercury that is deposited onto snowpacks is revolatilized to the atmosphere. Determining the revolatilized fraction is important since mercury that enters the snowpack meltwater may be converted to highly toxic bioaccumulating methylmercury. In this study, we present a new dynamic physically-based snowpack/meltwater model for mercury that is suitable for large-scale atmospheric models for mercury. It represents the primary physical and chemical processes that determine the fate of mercury deposited onto snowpacks. The snowpack/meltwater model was implemented in Environment Canada's atmospheric mercury model GRAHM. For the first time, observed snowpack-related mercury concentrations are used to evaluate and constrain an atmospheric mercury model. We find that simulated concentrations of mercury in both snowpacks and the atmosphere's surface layer agree closely with observations. The simulated concentration of mercury in both in the top 30 cm and the top 150 cm of the snowpack, averaged over 2005–2009, is predominantly below 6 ng L −1 over land south of 66.5° N but exceeds 18 ng L −1 over sea ice in extensive areas of the Arctic Ocean and Hudson Bay. The average simulated concentration of mercury in snowpack meltwater runoff tends to be higher on the Russian/European side (>20 ng L −1 ) of the Arctic Ocean than on the Canadian side (<10 ng L −1 ). The correlation coefficient between observed and simulated monthly mean atmospheric surface-level gaseous elemental mercury (GEM) concentrations increased significantly with the inclusion of the new snowpack/meltwater model at two of the three stations (midlatitude, subarctic) studied and remained constant at the third (arctic). Oceanic emissions are postulated to produce the observed summertime maximum in concentrations of surface-level atmospheric GEM at Alert in the Canadian Arctic and to generate the summertime volatility observed in these concentrations at both Alert and Kuujjuarapik on subarctic Hudson Bay, Canada. We find that the ... Article in Journal/Newspaper Arctic Arctic Ocean Hudson Bay Kuujjuarapik Sea ice Subarctic Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Hudson Bay Canada Hudson Kuujjuarapik ENVELOPE(-77.762,-77.762,55.276,55.276) Atmospheric Chemistry and Physics 12 19 9251 9274 |
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Directory of Open Access Journals: DOAJ Articles |
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English |
topic |
Physics QC1-999 Chemistry QD1-999 |
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Physics QC1-999 Chemistry QD1-999 D. Durnford A. Dastoor A. Ryzhkov L. Poissant M. Pilote D. Figueras-Nieto How relevant is the deposition of mercury onto snowpacks? – Part 2: A modeling study |
topic_facet |
Physics QC1-999 Chemistry QD1-999 |
description |
An unknown fraction of mercury that is deposited onto snowpacks is revolatilized to the atmosphere. Determining the revolatilized fraction is important since mercury that enters the snowpack meltwater may be converted to highly toxic bioaccumulating methylmercury. In this study, we present a new dynamic physically-based snowpack/meltwater model for mercury that is suitable for large-scale atmospheric models for mercury. It represents the primary physical and chemical processes that determine the fate of mercury deposited onto snowpacks. The snowpack/meltwater model was implemented in Environment Canada's atmospheric mercury model GRAHM. For the first time, observed snowpack-related mercury concentrations are used to evaluate and constrain an atmospheric mercury model. We find that simulated concentrations of mercury in both snowpacks and the atmosphere's surface layer agree closely with observations. The simulated concentration of mercury in both in the top 30 cm and the top 150 cm of the snowpack, averaged over 2005–2009, is predominantly below 6 ng L −1 over land south of 66.5° N but exceeds 18 ng L −1 over sea ice in extensive areas of the Arctic Ocean and Hudson Bay. The average simulated concentration of mercury in snowpack meltwater runoff tends to be higher on the Russian/European side (>20 ng L −1 ) of the Arctic Ocean than on the Canadian side (<10 ng L −1 ). The correlation coefficient between observed and simulated monthly mean atmospheric surface-level gaseous elemental mercury (GEM) concentrations increased significantly with the inclusion of the new snowpack/meltwater model at two of the three stations (midlatitude, subarctic) studied and remained constant at the third (arctic). Oceanic emissions are postulated to produce the observed summertime maximum in concentrations of surface-level atmospheric GEM at Alert in the Canadian Arctic and to generate the summertime volatility observed in these concentrations at both Alert and Kuujjuarapik on subarctic Hudson Bay, Canada. We find that the ... |
format |
Article in Journal/Newspaper |
author |
D. Durnford A. Dastoor A. Ryzhkov L. Poissant M. Pilote D. Figueras-Nieto |
author_facet |
D. Durnford A. Dastoor A. Ryzhkov L. Poissant M. Pilote D. Figueras-Nieto |
author_sort |
D. Durnford |
title |
How relevant is the deposition of mercury onto snowpacks? – Part 2: A modeling study |
title_short |
How relevant is the deposition of mercury onto snowpacks? – Part 2: A modeling study |
title_full |
How relevant is the deposition of mercury onto snowpacks? – Part 2: A modeling study |
title_fullStr |
How relevant is the deposition of mercury onto snowpacks? – Part 2: A modeling study |
title_full_unstemmed |
How relevant is the deposition of mercury onto snowpacks? – Part 2: A modeling study |
title_sort |
how relevant is the deposition of mercury onto snowpacks? – part 2: a modeling study |
publisher |
Copernicus Publications |
publishDate |
2012 |
url |
https://doi.org/10.5194/acp-12-9251-2012 https://doaj.org/article/7af3436d586f41a4a6c6be5a35d34e46 |
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ENVELOPE(-77.762,-77.762,55.276,55.276) |
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Arctic Arctic Ocean Hudson Bay Canada Hudson Kuujjuarapik |
geographic_facet |
Arctic Arctic Ocean Hudson Bay Canada Hudson Kuujjuarapik |
genre |
Arctic Arctic Ocean Hudson Bay Kuujjuarapik Sea ice Subarctic |
genre_facet |
Arctic Arctic Ocean Hudson Bay Kuujjuarapik Sea ice Subarctic |
op_source |
Atmospheric Chemistry and Physics, Vol 12, Iss 19, Pp 9251-9274 (2012) |
op_relation |
http://www.atmos-chem-phys.net/12/9251/2012/acp-12-9251-2012.pdf https://doaj.org/toc/1680-7316 https://doaj.org/toc/1680-7324 doi:10.5194/acp-12-9251-2012 1680-7316 1680-7324 https://doaj.org/article/7af3436d586f41a4a6c6be5a35d34e46 |
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https://doi.org/10.5194/acp-12-9251-2012 |
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Atmospheric Chemistry and Physics |
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12 |
container_issue |
19 |
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9251 |
op_container_end_page |
9274 |
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1766324537817825280 |