Articles | Volume 16, issue 23
https://doi.org/10.5194/acp-16-15371-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-16-15371-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
12 Dec 2016
Research article |
| 12 Dec 2016
The major stratospheric final warming in 2016: dispersal of vortex air and termination of Arctic chemical ozone loss
Gloria L. Manney
CORRESPONDING AUTHOR
NorthWest Research Associates, Socorro, New Mexico, USA
Department of Physics, New Mexico Institute of Mining
and Technology, Socorro, New Mexico, USA
Zachary D. Lawrence
Department of Physics, New Mexico Institute of Mining
and Technology, Socorro, New Mexico, USA
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74 citations as recorded by crossref.
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Saved (preprint)
Latest update: 27 May 2023
Short summary
The 2015/16 Arctic winter stratosphere was the coldest on record through late February, raising the possibility of extensive chemical ozone loss. However, a major final sudden stratospheric warming in early March curtailed ozone destruction. We used Aura MLS satellite trace gas data and MERRA-2 meteorological data to show the details of transport, mixing, and dispersal of chemically processed air during the major final warming, and how these processes limited Arctic chemical ozone loss.
The 2015/16 Arctic winter stratosphere was the coldest on record through late February, raising...
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