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Cited by 534

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Dynamic Oxidation of Gaseous Mercury in the Arctic Troposphere at Polar Sunrise

Lindberg, Steve E., Brooks, Steve, Lin, C.-J., Scott, Karen J., Landis, Matthew S., Stevens, Robert K., Goodsite, Mike, Richter, Andreas·2002·Environmental Science & Technology

Abstract

Gaseous elemental mercury (Hg0) is a globally distributed air toxin with a long atmospheric residence time. Any process that reduces its atmospheric lifetime increases its potential accumulation in the biosphere. Our data from Barrow, AK, at 71 degrees N show that rapid, photochemically driven oxidation of boundary-layer Hg0 after polar sunrise, probably by reactive halogens, creates a rapidly depositing species of oxidized gaseous mercury in the remote Arctic troposphere at concentrations in excess of 900 pg m(-3). This mercury accumulates in the snowpack during polar spring at an accelerated rate in a form that is bioavailable to bacteria and is released with snowmelt during the summer emergence of the Arctic ecosystem. Evidence suggests that this is a recent phenomenon that may be occurring throughout the earth's polar regions.

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Metadata

Authors
Lindberg, S. E., Brooks, S., Lin, C.-J., Scott, K. J., Landis, M. S., Stevens, R. K., Goodsite, M., & Richter, A.
Venue
Environmental Science & Technology
Published
2002-02-13
Volume
36
Issue
6
Pages
1245-1256
ISSN
  • 0013-936X (ISSN-L)
  • 1520-5851
OpenAlex
W1987969549
Cited by
534
References
0
FWCI
29.71
Type
journal article
Language
en
Open access
closed

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.