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Journal article

The formation and evolution of Titan’s winter polar vortex

Abstract:
Saturn’s largest moon Titan has a substantial nitrogen-methane atmosphere, with strong seasonal effects, including formation of winter polar vortices. Following Titan’s 2009 northern spring equinox, peak solar heating moved to the northern hemisphere, initiating south-polar subsidence and winter polar vortex formation. Throughout 2010–2011, strengthening subsidence produced a mesospheric hot-spot and caused extreme enrichment of photochemically produced trace gases. However, in 2012 unexpected and rapid mesospheric cooling was observed. Here we show extreme trace gas enrichment within the polar vortex dramatically increases mesospheric long-wave radiative cooling efficiency, causing unusually cold temperatures 2–6 years post-equinox. The long time-frame to reach a stable vortex configuration results from the high infrared opacity of Titan’s trace gases and the relatively long atmospheric radiative time constant. Winter polar hot-spots have been observed on other planets, but detection of post-equinox cooling is so far unique to Titan.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1038/s41467-017-01839-z

Authors


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Role:
Author
ORCID:
0000-0003-3108-5775
More by this author
Role:
Author
ORCID:
0000-0001-7086-8882


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Funder identifier:
https://ror.org/051sgbe98
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Funder identifier:
https://ror.org/057g20z61


Publisher:
Nature Publishing Group
Journal:
Nature Communications More from this journal
Volume:
8
Issue:
1
Article number:
1586
Publication date:
2017-11-21
Acceptance date:
2017-10-18
DOI:
EISSN:
2041-1723
ISSN:
2041-1723
Pmid:
29162820


Language:
English
Pubs id:
pubs:803118
UUID:
uuid:675cd85a-03fb-48e6-afff-cb35982be03a
Local pid:
pubs:803118
Source identifiers:
803118
Deposit date:
2018-01-09

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