Seasonal Evolution of Titan’s Stratospheric Tilt and Temperature Field at High Resolution from Cassini/CIRS

The Cassini spacecraft observed Titan from 2004 to 2017, capturing key atmospheric features, including the tilt of the middle atmosphere and the formation and breakup of winter polar vortices. We analyze low spectral resolution infrared observations from Cassini’s Composite Infrared Spectrometer (CI...

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Main Authors: Lucy Wright, Nicholas A. Teanby, Patrick G. J. Irwin, Conor A. Nixon, Nicholas A. Lombardo, Juan M. Lora, Daniel Mitchell
Format: Article
Language:English
Published: IOP Publishing 2025-01-01
Series:The Planetary Science Journal
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Online Access:https://doi.org/10.3847/PSJ/adcab3
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author Lucy Wright
Nicholas A. Teanby
Patrick G. J. Irwin
Conor A. Nixon
Nicholas A. Lombardo
Juan M. Lora
Daniel Mitchell
author_facet Lucy Wright
Nicholas A. Teanby
Patrick G. J. Irwin
Conor A. Nixon
Nicholas A. Lombardo
Juan M. Lora
Daniel Mitchell
author_sort Lucy Wright
collection DOAJ
description The Cassini spacecraft observed Titan from 2004 to 2017, capturing key atmospheric features, including the tilt of the middle atmosphere and the formation and breakup of winter polar vortices. We analyze low spectral resolution infrared observations from Cassini’s Composite Infrared Spectrometer (CIRS), which provide excellent spatial and temporal coverage and the best horizontal spatial resolution of any of the CIRS observations. With approximately 4 times higher meridional resolution than previous studies, we map the stratospheric temperature for almost half a Titan year. We determine the evolution of Titan’s stratospheric tilt, finding that it is most constant in the inertial frame, directed 120° ± 6° west of the Titan–Sun vector at the northern spring equinox, with seasonal oscillations in the tilt magnitude between around 2 $\mathop{.}\limits^{\unicode{x000b0}}$ 5 and 8°. Using the high meridional resolution temperature field, we reveal finer details in the zonal wind and potential vorticity. In addition to the strong winter zonal jet, a weaker zonal jet in Titan’s summer hemisphere is observed, and there is a suggestion that the main winter hemisphere jet briefly splits into two. We also present the strongest evidence yet that Titan’s polar vortex is annular for part of its life cycle.
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publishDate 2025-01-01
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spelling doaj-art-26855e3bc4494ea098b9199cc3c9ed4d2025-08-20T01:54:02ZengIOP PublishingThe Planetary Science Journal2632-33382025-01-016511410.3847/PSJ/adcab3Seasonal Evolution of Titan’s Stratospheric Tilt and Temperature Field at High Resolution from Cassini/CIRSLucy Wright0https://orcid.org/0000-0002-6023-5755Nicholas A. Teanby1https://orcid.org/0000-0003-3108-5775Patrick G. J. Irwin2https://orcid.org/0000-0002-6772-384XConor A. Nixon3https://orcid.org/0000-0001-9540-9121Nicholas A. Lombardo4https://orcid.org/0000-0001-8621-6520Juan M. Lora5https://orcid.org/0000-0001-9925-1050Daniel Mitchell6https://orcid.org/0000-0002-0117-3486School of Earth Sciences, University of Bristol , Bristol, UKSchool of Earth Sciences, University of Bristol , Bristol, UKAtmospheric, Oceanic, and Planetary Physics, Department of Physics, University of Oxford , Oxford, UKPlanetary Systems Laboratory, NASA Goddard Space Flight Center , Greenbelt, MD 20771, USADepartment of Earth and Planetary Sciences, Yale University , New Haven, CT 06511, USADepartment of Earth and Planetary Sciences, Yale University , New Haven, CT 06511, USASchool of Geographical Sciences, University of Bristol , Bristol, UKThe Cassini spacecraft observed Titan from 2004 to 2017, capturing key atmospheric features, including the tilt of the middle atmosphere and the formation and breakup of winter polar vortices. We analyze low spectral resolution infrared observations from Cassini’s Composite Infrared Spectrometer (CIRS), which provide excellent spatial and temporal coverage and the best horizontal spatial resolution of any of the CIRS observations. With approximately 4 times higher meridional resolution than previous studies, we map the stratospheric temperature for almost half a Titan year. We determine the evolution of Titan’s stratospheric tilt, finding that it is most constant in the inertial frame, directed 120° ± 6° west of the Titan–Sun vector at the northern spring equinox, with seasonal oscillations in the tilt magnitude between around 2 $\mathop{.}\limits^{\unicode{x000b0}}$ 5 and 8°. Using the high meridional resolution temperature field, we reveal finer details in the zonal wind and potential vorticity. In addition to the strong winter zonal jet, a weaker zonal jet in Titan’s summer hemisphere is observed, and there is a suggestion that the main winter hemisphere jet briefly splits into two. We also present the strongest evidence yet that Titan’s polar vortex is annular for part of its life cycle.https://doi.org/10.3847/PSJ/adcab3TitanRadiative transferInfrared spectroscopyPlanetary atmospheres
spellingShingle Lucy Wright
Nicholas A. Teanby
Patrick G. J. Irwin
Conor A. Nixon
Nicholas A. Lombardo
Juan M. Lora
Daniel Mitchell
Seasonal Evolution of Titan’s Stratospheric Tilt and Temperature Field at High Resolution from Cassini/CIRS
The Planetary Science Journal
Titan
Radiative transfer
Infrared spectroscopy
Planetary atmospheres
title Seasonal Evolution of Titan’s Stratospheric Tilt and Temperature Field at High Resolution from Cassini/CIRS
title_full Seasonal Evolution of Titan’s Stratospheric Tilt and Temperature Field at High Resolution from Cassini/CIRS
title_fullStr Seasonal Evolution of Titan’s Stratospheric Tilt and Temperature Field at High Resolution from Cassini/CIRS
title_full_unstemmed Seasonal Evolution of Titan’s Stratospheric Tilt and Temperature Field at High Resolution from Cassini/CIRS
title_short Seasonal Evolution of Titan’s Stratospheric Tilt and Temperature Field at High Resolution from Cassini/CIRS
title_sort seasonal evolution of titan s stratospheric tilt and temperature field at high resolution from cassini cirs
topic Titan
Radiative transfer
Infrared spectroscopy
Planetary atmospheres
url https://doi.org/10.3847/PSJ/adcab3
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