Convective forcing of mercury and ozone in the Arctic boundary layer induced by leads in sea ice-Reference-Cited by-同舟云学术

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Convective forcing of mercury and ozone in the Arctic boundary layer induced by leads in sea ice

Published:2014-01-15 Issue:7486 Volume:506 Page:81-84
ISSN:0028-0836
Container-title:Nature
language:en
Short-container-title:Nature

Author:

Moore Christopher W.,Obrist Daniel,Steffen Alexandra,Staebler Ralf M.,Douglas Thomas A.,Richter Andreas,Nghiem Son V.

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/nature12924.pdf

Reference32 articles.

1. Nghiem, S. V. et al. Rapid reduction of Arctic perennial sea ice. Geophys. Res. Lett. 34, L19504 (2007)

2. Hutchings, J. K. & Rigor, I. G. Role of ice dynamics in anomalous ice conditions in the Beaufort Sea during 2006 and 2007. J. Geophys. Res. 117, C00E04 (2012)

3. Stroeve, J. et al. The Arctic’s rapidly shrinking sea ice cover: a research synthesis. Clim. Change 110, 1005–1027 (2012)

4. Nghiem, S. V. et al. Field and satellite observations of the formation and distribution of Arctic atmospheric bromine above a rejuvenated sea ice cover. J. Geophys. Res. 117, D00S05 (2012)

5. Steffen, A. et al. A synthesis of atmospheric mercury depletion event chemistry in the atmosphere and snow. Atmos. Chem. Phys. 8, 1445–1482 (2008)

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