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Toyota, K., Dastoor, A. P., Ryzhkov, A. (2014) Air–snowpack exchange of bromine, ozone and mercury in the springtime Arctic simulated by the 1-D model PHANTAS – Part 2: Mercury and its speciation. Atmospheric Chemistry and Physics, 14 (8). 4135-4167 doi:10.5194/acp-14-4135-2014

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Reference TypeJournal (article/letter/editorial)
TitleAir–snowpack exchange of bromine, ozone and mercury in the springtime Arctic simulated by the 1-D model PHANTAS – Part 2: Mercury and its speciation
JournalAtmospheric Chemistry and Physics
AuthorsToyota, K.Author
Dastoor, A. P.Author
Ryzhkov, A.Author
Year2014 (April 25)Volume14
Issue8
PublisherCopernicus GmbH
DOIdoi:10.5194/acp-14-4135-2014Search in ResearchGate
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Mindat Ref. ID8932147Long-form Identifiermindat:1:5:8932147:0
GUID0
Full ReferenceToyota, K., Dastoor, A. P., Ryzhkov, A. (2014) Air–snowpack exchange of bromine, ozone and mercury in the springtime Arctic simulated by the 1-D model PHANTAS – Part 2: Mercury and its speciation. Atmospheric Chemistry and Physics, 14 (8). 4135-4167 doi:10.5194/acp-14-4135-2014
Plain TextToyota, K., Dastoor, A. P., Ryzhkov, A. (2014) Air–snowpack exchange of bromine, ozone and mercury in the springtime Arctic simulated by the 1-D model PHANTAS – Part 2: Mercury and its speciation. Atmospheric Chemistry and Physics, 14 (8). 4135-4167 doi:10.5194/acp-14-4135-2014
In(2014, April) Atmospheric Chemistry and Physics Vol. 14 (8) Copernicus GmbH

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Toyota, K., McConnell, J. C., Staebler, R. M., Dastoor, A. P. (2014) Air–snowpack exchange of bromine, ozone and mercury in the springtime Arctic simulated by the 1-D model PHANTAS – Part 1: In-snow bromine activation and its impact on ozone. Atmospheric Chemistry and Physics, 14 (8). 4101-4133 doi:10.5194/acp-14-4101-2014
Toyota, K., Dastoor, A. P., Ryzhkov, A. (2013) Air-snowpack exchange of bromine, ozone and mercury in the springtime Arctic simulated by the 1-D model PHANTAS – Part 2: Mercury and its speciation. Atmospheric Chemistry and Physics Discussions, 13 (8). 22151-22220 doi:10.5194/acpd-13-22151-2013
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