Understanding mercury oxidation and air–snow exchange on the East Antarctic Plateau: a modeling study

Distinct diurnal and seasonal variations of mercury (Hg) have been observed in near-surface air at Concordia Station on the East Antarctic Plateau, but the processes controlling these characteristics are not well understood. Here, we use a box model to interpret the Hg0 (gaseous elemental mercury) m...

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Main Authors: Gallée, Hubert, Sprovieri, Francesca, Pirrone, Nicola, Helmig, Detlev, Savarino, Joël, Magand, Olivier, Dommergue, Aurélien, Song, Shaojie, Angot, Helene Paule, Selin, Noelle E
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Article
Published: Copernicus Publications 2019
Online Access:http://hdl.handle.net/1721.1/120548
https://orcid.org/0000-0001-6395-7422
https://orcid.org/0000-0002-6396-5622
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author Gallée, Hubert
Sprovieri, Francesca
Pirrone, Nicola
Helmig, Detlev
Savarino, Joël
Magand, Olivier
Dommergue, Aurélien
Song, Shaojie
Angot, Helene Paule
Selin, Noelle E
author2 Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
author_facet Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Gallée, Hubert
Sprovieri, Francesca
Pirrone, Nicola
Helmig, Detlev
Savarino, Joël
Magand, Olivier
Dommergue, Aurélien
Song, Shaojie
Angot, Helene Paule
Selin, Noelle E
author_sort Gallée, Hubert
collection MIT
description Distinct diurnal and seasonal variations of mercury (Hg) have been observed in near-surface air at Concordia Station on the East Antarctic Plateau, but the processes controlling these characteristics are not well understood. Here, we use a box model to interpret the Hg0 (gaseous elemental mercury) measurements in thes year 2013. The model includes atmospheric Hg0 oxidation (by OH, O3, or bromine), surface snow HgII (oxidized mercury) reduction, and air-snow exchange, and is driven by meteorological fields from a regional climate model. The simulations suggest that a photochemically driven mercury diurnal cycle occurs at the air-snow interface in austral summer. The fast oxidation of Hg0 in summer may be provided by a two-step bromine-initiated scheme, which is favored by low temperature and high nitrogen oxides at Concordia. The summertime diurnal variations of Hg0 (peaking during daytime) may be confined within several tens of meters above the snow surface and affected by changing mixed layer depths. Snow re-emission of Hg0 is mainly driven by photoreduction of snow HgII in summer. Intermittent warming events and a hypothesized reduction of HgII occurring in snow in the dark may be important processes controlling the mercury variations in the non-summer period, although their relative importance is uncertain. The Br-initiated oxidation of Hg0 is expected to be slower at Summit Station in Greenland than at Concordia (due to their difference in temperature and levels of nitrogen oxides and ozone), which may contribute to the observed differences in the summertime diurnal variations of Hg0 between these two polar inland stations.
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spelling mit-1721.1/1205482022-10-01T13:20:57Z Understanding mercury oxidation and air–snow exchange on the East Antarctic Plateau: a modeling study Gallée, Hubert Sprovieri, Francesca Pirrone, Nicola Helmig, Detlev Savarino, Joël Magand, Olivier Dommergue, Aurélien Song, Shaojie Angot, Helene Paule Selin, Noelle E Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Massachusetts Institute of Technology. Institute for Data, Systems, and Society Song, Shaojie Angot, Helene Paule Selin, Noelle E Distinct diurnal and seasonal variations of mercury (Hg) have been observed in near-surface air at Concordia Station on the East Antarctic Plateau, but the processes controlling these characteristics are not well understood. Here, we use a box model to interpret the Hg0 (gaseous elemental mercury) measurements in thes year 2013. The model includes atmospheric Hg0 oxidation (by OH, O3, or bromine), surface snow HgII (oxidized mercury) reduction, and air-snow exchange, and is driven by meteorological fields from a regional climate model. The simulations suggest that a photochemically driven mercury diurnal cycle occurs at the air-snow interface in austral summer. The fast oxidation of Hg0 in summer may be provided by a two-step bromine-initiated scheme, which is favored by low temperature and high nitrogen oxides at Concordia. The summertime diurnal variations of Hg0 (peaking during daytime) may be confined within several tens of meters above the snow surface and affected by changing mixed layer depths. Snow re-emission of Hg0 is mainly driven by photoreduction of snow HgII in summer. Intermittent warming events and a hypothesized reduction of HgII occurring in snow in the dark may be important processes controlling the mercury variations in the non-summer period, although their relative importance is uncertain. The Br-initiated oxidation of Hg0 is expected to be slower at Summit Station in Greenland than at Concordia (due to their difference in temperature and levels of nitrogen oxides and ozone), which may contribute to the observed differences in the summertime diurnal variations of Hg0 between these two polar inland stations. National Science Foundation (U.S.) (Grant ACP-1053648) 2019-02-26T20:16:49Z 2019-02-26T20:16:49Z 2018-11 2018-09 2019-02-25T12:36:32Z Article http://purl.org/eprint/type/JournalArticle 1680-7324 1680-7316 http://hdl.handle.net/1721.1/120548 Song, Shaojie et al. “Understanding Mercury Oxidation and Air–snow Exchange on the East Antarctic Plateau: a Modeling Study.” Atmospheric Chemistry and Physics 18, 21 (November 2018): 15825–15840 © 2018 Author(s) https://orcid.org/0000-0001-6395-7422 https://orcid.org/0000-0002-6396-5622 http://dx.doi.org/10.5194/acp-18-15825-2018 Atmospheric Chemistry and Physics Creative Commons Attribution 4.0 International license https://creativecommons.org/licenses/by/4.0/ application/pdf Copernicus Publications Copernicus
spellingShingle Gallée, Hubert
Sprovieri, Francesca
Pirrone, Nicola
Helmig, Detlev
Savarino, Joël
Magand, Olivier
Dommergue, Aurélien
Song, Shaojie
Angot, Helene Paule
Selin, Noelle E
Understanding mercury oxidation and air–snow exchange on the East Antarctic Plateau: a modeling study
title Understanding mercury oxidation and air–snow exchange on the East Antarctic Plateau: a modeling study
title_full Understanding mercury oxidation and air–snow exchange on the East Antarctic Plateau: a modeling study
title_fullStr Understanding mercury oxidation and air–snow exchange on the East Antarctic Plateau: a modeling study
title_full_unstemmed Understanding mercury oxidation and air–snow exchange on the East Antarctic Plateau: a modeling study
title_short Understanding mercury oxidation and air–snow exchange on the East Antarctic Plateau: a modeling study
title_sort understanding mercury oxidation and air snow exchange on the east antarctic plateau a modeling study
url http://hdl.handle.net/1721.1/120548
https://orcid.org/0000-0001-6395-7422
https://orcid.org/0000-0002-6396-5622
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