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Uranus's northern polar cap in 2014

Abstract:
In October and November 2014, spectra covering the 1.436 – 1.863-μm wavelength range from the SINFONI Integral Field Unit Spectrometer on the Very Large Telescope showed the presence of a vast bright North polar cap on Uranus, extending northward from about 40ºN and at all longitudes observed. The feature, first detected in August 2014 from Keck telescope images, has a morphology very similar to the southern polar cap that was seen to fade before the 2007 equinox. At strong methane-absorbing wavelengths (for which only the high troposphere or stratosphere is sampled) the feature is not visible, indicating that it is not a stratospheric phenomenon. We show that the observed northern bright polar cap results mainly from a decrease in the tropospheric methane mixing ratio, rather than from a possible latitudinal variation of the optical properties or abundance of aerosol, implying an increase in polar downwelling near the tropopause level.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1029/2018GL077654

Authors


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Institution:
University of Oxford
Division:
MPLS
Department:
Physics
Sub department:
Atmos Ocean & Planet Physics
Role:
Author
ORCID:
0000-0002-9424-2929
More by this author
Institution:
University of Oxford
Division:
MPLS Division
Department:
Physics; Atmos Ocean & Planet Physics
Role:
Author


Publisher:
Wiley
Journal:
Geophysical Research Letters More from this journal
Publication date:
2018-06-04
Acceptance date:
2018-05-25
DOI:
EISSN:
1944-8007
ISSN:
0094-8276


Keywords:
Pubs id:
pubs:857847
UUID:
uuid:dec0dfb0-ab72-45d5-b376-1beab99992ae
Local pid:
pubs:857847
Source identifiers:
857847
Deposit date:
2018-06-17

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