Mercury isotope evidence for Arctic summertime re-emission of mercury from the cryosphere

During Arctic springtime, halogen radicals oxidize atmospheric elemental mercury (Hg(0)), which deposits to the cryosphere. This is followed by a summertime atmospheric Hg(0) peak that is thought to result mostly from terrestrial Hg inputs to the Arctic Ocean, followed by photoreduction and emission...

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Detalles Bibliográficos
Autores principales: Araujo, Beatriz Ferreira, Osterwalder, Stefan, Szponar, Natalie, Lee, Domenica, Petrova, Mariia V., Pernov, Jakob Boyd, Ahmed, Shaddy, Heimbürger-Boavida, Lars-Eric, Laffont, Laure, Teisserenc, Roman, Tananaev, Nikita, Nordstrom, Claus, Magand, Olivier, Stupple, Geoff, Skov, Henrik, Steffen, Alexandra, Bergquist, Bridget, Pfaffhuber, Katrine Aspmo, Thomas, Jennie L., Scheper, Simon, Petäjä, Tuukka, Dommergue, Aurélien, Sonke, Jeroen E.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9402541/
https://www.ncbi.nlm.nih.gov/pubmed/36002442
http://dx.doi.org/10.1038/s41467-022-32440-8

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9402541/
https://www.ncbi.nlm.nih.gov/pubmed/36002442
http://dx.doi.org/10.1038/s41467-022-32440-8

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