Riverine source of Arctic Ocean mercury inferred from atmospheric observations
Methylmercury is a potent neurotoxin that accumulates in aquatic food webs. Human activities, including industry and mining, have increased inorganic mercury inputs to terrestrial and aquatic ecosystems. Methylation of this mercury generates methylmercury, and is thus a public health concern. Marine...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.353.4544 2023-05-15T14:35:06+02:00 Riverine source of Arctic Ocean mercury inferred from atmospheric observations Jenny A. Fisher Daniel J. Jacob Anne L. Soerensen Helen M. Amos Ra Steffen Elsie M. Sunderl The Pennsylvania State University CiteSeerX Archives 2012 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.353.4544 http://www.nature.com/ngeo/journal/v5/n7/pdf/ngeo1478.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.353.4544 http://www.nature.com/ngeo/journal/v5/n7/pdf/ngeo1478.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.nature.com/ngeo/journal/v5/n7/pdf/ngeo1478.pdf text 2012 ftciteseerx 2016-01-08T00:27:24Z Methylmercury is a potent neurotoxin that accumulates in aquatic food webs. Human activities, including industry and mining, have increased inorganic mercury inputs to terrestrial and aquatic ecosystems. Methylation of this mercury generates methylmercury, and is thus a public health concern. Marine methylmercury is a particular concern in the Arctic, where indigenous peoples rely heavily on marine-based diets. In the summer, atmospheric inorganic mercury concentrations peak in the Arctic, whereas they reach a minimum in the northern mid-latitudes. Here, we use a global three-dimensional ocean–atmosphere model to examine the cause of this Arctic summertime maximum. According to our simulations, circumpolar rivers deliver large quantities of mercury to the Arctic Ocean during summer; the subsequent evasion of this riverine mercury to the atmosphere can explain the summertime peak in atmospheric mercury levels. We infer that rivers are the dominant source of mercury to the Arctic Ocean on an annual basis. Our simulations suggest that Arctic Ocean mercury concentrations could be highly sensitive to climate-induced changes in river flow, and to increases in the mobility of mercury in soils, for example as a result of permafrost thaw and forest fires. Mercury is emitted from anthropogenic and natural sources primarily as elemental mercury (Hg0). The Hg0 atmospheric lifetime of 6–12 months allows transport of this emitted mercury on a hemispheric scale. Eventual oxidation to highly soluble HgII drives deposition in remote regions. Hg0 has Text Arctic Arctic Ocean permafrost Unknown Arctic Arctic Ocean |
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English |
description |
Methylmercury is a potent neurotoxin that accumulates in aquatic food webs. Human activities, including industry and mining, have increased inorganic mercury inputs to terrestrial and aquatic ecosystems. Methylation of this mercury generates methylmercury, and is thus a public health concern. Marine methylmercury is a particular concern in the Arctic, where indigenous peoples rely heavily on marine-based diets. In the summer, atmospheric inorganic mercury concentrations peak in the Arctic, whereas they reach a minimum in the northern mid-latitudes. Here, we use a global three-dimensional ocean–atmosphere model to examine the cause of this Arctic summertime maximum. According to our simulations, circumpolar rivers deliver large quantities of mercury to the Arctic Ocean during summer; the subsequent evasion of this riverine mercury to the atmosphere can explain the summertime peak in atmospheric mercury levels. We infer that rivers are the dominant source of mercury to the Arctic Ocean on an annual basis. Our simulations suggest that Arctic Ocean mercury concentrations could be highly sensitive to climate-induced changes in river flow, and to increases in the mobility of mercury in soils, for example as a result of permafrost thaw and forest fires. Mercury is emitted from anthropogenic and natural sources primarily as elemental mercury (Hg0). The Hg0 atmospheric lifetime of 6–12 months allows transport of this emitted mercury on a hemispheric scale. Eventual oxidation to highly soluble HgII drives deposition in remote regions. Hg0 has |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Jenny A. Fisher Daniel J. Jacob Anne L. Soerensen Helen M. Amos Ra Steffen Elsie M. Sunderl |
spellingShingle |
Jenny A. Fisher Daniel J. Jacob Anne L. Soerensen Helen M. Amos Ra Steffen Elsie M. Sunderl Riverine source of Arctic Ocean mercury inferred from atmospheric observations |
author_facet |
Jenny A. Fisher Daniel J. Jacob Anne L. Soerensen Helen M. Amos Ra Steffen Elsie M. Sunderl |
author_sort |
Jenny A. Fisher |
title |
Riverine source of Arctic Ocean mercury inferred from atmospheric observations |
title_short |
Riverine source of Arctic Ocean mercury inferred from atmospheric observations |
title_full |
Riverine source of Arctic Ocean mercury inferred from atmospheric observations |
title_fullStr |
Riverine source of Arctic Ocean mercury inferred from atmospheric observations |
title_full_unstemmed |
Riverine source of Arctic Ocean mercury inferred from atmospheric observations |
title_sort |
riverine source of arctic ocean mercury inferred from atmospheric observations |
publishDate |
2012 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.353.4544 http://www.nature.com/ngeo/journal/v5/n7/pdf/ngeo1478.pdf |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean permafrost |
genre_facet |
Arctic Arctic Ocean permafrost |
op_source |
http://www.nature.com/ngeo/journal/v5/n7/pdf/ngeo1478.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.353.4544 http://www.nature.com/ngeo/journal/v5/n7/pdf/ngeo1478.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766307994639794176 |