EGU General Assembly 2009 © Author(s) 2008 Titan’s Stratospheric chemistry: Spatial And Temporal Variations Of

Four years into the Cassini-Huygens mission, we present results obtained on Titan’s chemical composition by analyzing CIRS data in the far-and mid-IR region. With respect to previous publications (Flasar et al., 2005; Coustenis et al., 2007, 2008b; Teanby et al., 2006, 2008; Vinatier et al., 2007) w...

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Main Author: Trace Species
Other Authors: The Pennsylvania State University CiteSeerX Archives
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.658.7403
http://meetingorganizer.copernicus.org/egu2009/egu2009-1668.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.658.7403 2023-05-15T17:39:59+02:00 EGU General Assembly 2009 © Author(s) 2008 Titan’s Stratospheric chemistry: Spatial And Temporal Variations Of Trace Species The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.658.7403 http://meetingorganizer.copernicus.org/egu2009/egu2009-1668.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.658.7403 http://meetingorganizer.copernicus.org/egu2009/egu2009-1668.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://meetingorganizer.copernicus.org/egu2009/egu2009-1668.pdf text ftciteseerx 2016-01-08T16:44:17Z Four years into the Cassini-Huygens mission, we present results obtained on Titan’s chemical composition by analyzing CIRS data in the far-and mid-IR region. With respect to previous publications (Flasar et al., 2005; Coustenis et al., 2007, 2008b; Teanby et al., 2006, 2008; Vinatier et al., 2007) we improved our analysis by exploiting a considerably larger number of nadir spectra, in particular at high resolution (0.53 cm−1). The more complete coverage of Titan’s disk, combined with the larger number of spectra at high resolution, allows for the inference of more precise abundances for the trace gases and for a more adequate definition of meridional variations, in particular in the northern regions. The retrievals of the meridional variations of the trace constituents show an enhancement for some of them towards the North pole. Molecules showing a significant enhancement at northern latitudes are the nitriles (HC3N, HCN) and the complex hydrocarbons (C4H2, C3H4). To a lesser degree, acetylene and ethane also exhibit abundance increases by factors of 1.5-2. Isotopic ratios in carbon, nitrogen and oxygen have been determined (Jennings et al., 2008, Nixon et al., 2008a,b). The D/H ratio on Titan was also determined from the CH3D band at 8.6 micron and the C2HD band at 678 cm−1 (Coustenis et al., 2008a). We compare our results with previous inferences from earlier CIRS and Voyager1/IRIS data and from ISO data taken in 1997. The results are tied to predictions by dynamical-photochemical models (Rannou et al., 2005; Lavvas et al., 2008a,b, Crespin et al., 2008 and references therein). Finally, we will present the case for future observations from space (e.g. with the TSSM mission Text North Pole Unknown Jennings ENVELOPE(72.556,72.556,-70.145,-70.145) North Pole
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description Four years into the Cassini-Huygens mission, we present results obtained on Titan’s chemical composition by analyzing CIRS data in the far-and mid-IR region. With respect to previous publications (Flasar et al., 2005; Coustenis et al., 2007, 2008b; Teanby et al., 2006, 2008; Vinatier et al., 2007) we improved our analysis by exploiting a considerably larger number of nadir spectra, in particular at high resolution (0.53 cm−1). The more complete coverage of Titan’s disk, combined with the larger number of spectra at high resolution, allows for the inference of more precise abundances for the trace gases and for a more adequate definition of meridional variations, in particular in the northern regions. The retrievals of the meridional variations of the trace constituents show an enhancement for some of them towards the North pole. Molecules showing a significant enhancement at northern latitudes are the nitriles (HC3N, HCN) and the complex hydrocarbons (C4H2, C3H4). To a lesser degree, acetylene and ethane also exhibit abundance increases by factors of 1.5-2. Isotopic ratios in carbon, nitrogen and oxygen have been determined (Jennings et al., 2008, Nixon et al., 2008a,b). The D/H ratio on Titan was also determined from the CH3D band at 8.6 micron and the C2HD band at 678 cm−1 (Coustenis et al., 2008a). We compare our results with previous inferences from earlier CIRS and Voyager1/IRIS data and from ISO data taken in 1997. The results are tied to predictions by dynamical-photochemical models (Rannou et al., 2005; Lavvas et al., 2008a,b, Crespin et al., 2008 and references therein). Finally, we will present the case for future observations from space (e.g. with the TSSM mission
author2 The Pennsylvania State University CiteSeerX Archives
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author Trace Species
spellingShingle Trace Species
EGU General Assembly 2009 © Author(s) 2008 Titan’s Stratospheric chemistry: Spatial And Temporal Variations Of
author_facet Trace Species
author_sort Trace Species
title EGU General Assembly 2009 © Author(s) 2008 Titan’s Stratospheric chemistry: Spatial And Temporal Variations Of
title_short EGU General Assembly 2009 © Author(s) 2008 Titan’s Stratospheric chemistry: Spatial And Temporal Variations Of
title_full EGU General Assembly 2009 © Author(s) 2008 Titan’s Stratospheric chemistry: Spatial And Temporal Variations Of
title_fullStr EGU General Assembly 2009 © Author(s) 2008 Titan’s Stratospheric chemistry: Spatial And Temporal Variations Of
title_full_unstemmed EGU General Assembly 2009 © Author(s) 2008 Titan’s Stratospheric chemistry: Spatial And Temporal Variations Of
title_sort egu general assembly 2009 © author(s) 2008 titan’s stratospheric chemistry: spatial and temporal variations of
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.658.7403
http://meetingorganizer.copernicus.org/egu2009/egu2009-1668.pdf
long_lat ENVELOPE(72.556,72.556,-70.145,-70.145)
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http://meetingorganizer.copernicus.org/egu2009/egu2009-1668.pdf
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