Titan's atmospheric temperatures, winds, and composition.

Temperatures obtained from early Cassini infrared observations of Titan show a stratopause at an altitude of 310 kilometers (and 186 kelvin at 15 degrees S). Stratospheric temperatures are coldest in the winter northern hemisphere, with zonal winds reaching 160 meters per second. The concentrations...

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Main Authors: Flasar, F, Achterberg, R, Conrath, B, Gierasch, P, Kunde, V, Nixon, C, Bjoraker, G, Jennings, D, Romani, P, Simon-Miller, A, Bézard, B, Coustenis, A, Irwin, P, Teanby, N, Brasunas, J, Pearl, J, Segura, M, Carlson, R, Mamoutkine, A, Schinder, P, Barucci, A, Courtin, R, Fouchet, T, Gautier, D, Lellouch, E
Format: Journal article
Language:English
Published: 2005
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author Flasar, F
Achterberg, R
Conrath, B
Gierasch, P
Kunde, V
Nixon, C
Bjoraker, G
Jennings, D
Romani, P
Simon-Miller, A
Bézard, B
Coustenis, A
Irwin, P
Teanby, N
Brasunas, J
Pearl, J
Segura, M
Carlson, R
Mamoutkine, A
Schinder, P
Barucci, A
Courtin, R
Fouchet, T
Gautier, D
Lellouch, E
author_facet Flasar, F
Achterberg, R
Conrath, B
Gierasch, P
Kunde, V
Nixon, C
Bjoraker, G
Jennings, D
Romani, P
Simon-Miller, A
Bézard, B
Coustenis, A
Irwin, P
Teanby, N
Brasunas, J
Pearl, J
Segura, M
Carlson, R
Mamoutkine, A
Schinder, P
Barucci, A
Courtin, R
Fouchet, T
Gautier, D
Lellouch, E
author_sort Flasar, F
collection OXFORD
description Temperatures obtained from early Cassini infrared observations of Titan show a stratopause at an altitude of 310 kilometers (and 186 kelvin at 15 degrees S). Stratospheric temperatures are coldest in the winter northern hemisphere, with zonal winds reaching 160 meters per second. The concentrations of several stratospheric organic compounds are enhanced at mid- and high northern latitudes, and the strong zonal winds may inhibit mixing between these latitudes and the rest of Titan. Above the south pole, temperatures in the stratosphere are 4 to 5 kelvin cooler than at the equator. The stratospheric mole fractions of methane and carbon monoxide are (1.6 +/- 0.5) x 10(-2) and (4.5 +/- 1.5) x 10(-5), respectively.
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spelling oxford-uuid:35faba32-411a-489b-89d0-268874979f542022-03-26T13:35:02ZTitan's atmospheric temperatures, winds, and composition.Journal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:35faba32-411a-489b-89d0-268874979f54EnglishSymplectic Elements at Oxford2005Flasar, FAchterberg, RConrath, BGierasch, PKunde, VNixon, CBjoraker, GJennings, DRomani, PSimon-Miller, ABézard, BCoustenis, AIrwin, PTeanby, NBrasunas, JPearl, JSegura, MCarlson, RMamoutkine, ASchinder, PBarucci, ACourtin, RFouchet, TGautier, DLellouch, ETemperatures obtained from early Cassini infrared observations of Titan show a stratopause at an altitude of 310 kilometers (and 186 kelvin at 15 degrees S). Stratospheric temperatures are coldest in the winter northern hemisphere, with zonal winds reaching 160 meters per second. The concentrations of several stratospheric organic compounds are enhanced at mid- and high northern latitudes, and the strong zonal winds may inhibit mixing between these latitudes and the rest of Titan. Above the south pole, temperatures in the stratosphere are 4 to 5 kelvin cooler than at the equator. The stratospheric mole fractions of methane and carbon monoxide are (1.6 +/- 0.5) x 10(-2) and (4.5 +/- 1.5) x 10(-5), respectively.
spellingShingle Flasar, F
Achterberg, R
Conrath, B
Gierasch, P
Kunde, V
Nixon, C
Bjoraker, G
Jennings, D
Romani, P
Simon-Miller, A
Bézard, B
Coustenis, A
Irwin, P
Teanby, N
Brasunas, J
Pearl, J
Segura, M
Carlson, R
Mamoutkine, A
Schinder, P
Barucci, A
Courtin, R
Fouchet, T
Gautier, D
Lellouch, E
Titan's atmospheric temperatures, winds, and composition.
title Titan's atmospheric temperatures, winds, and composition.
title_full Titan's atmospheric temperatures, winds, and composition.
title_fullStr Titan's atmospheric temperatures, winds, and composition.
title_full_unstemmed Titan's atmospheric temperatures, winds, and composition.
title_short Titan's atmospheric temperatures, winds, and composition.
title_sort titan s atmospheric temperatures winds and composition
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