On the HCN and CO 2 abundance and distribution in Jupiter's stratosphere

International audience Observations of Jupiter by Cassini/CIRS, acquired during the December 2000 flyby, provide the latitudinal distribution of HCN and CO 2 in Jupiter's stratosphere with unprecedented spatial resolution and coverage. Following up on a preliminary study by Kunde et al. [Kunde,...

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Published in:Icarus
Main Authors: Lellouch, Emmanuel, Bézard, Bruno, Strobel, Darell, Bjoraker, Gordon L., Flasar, Michael, Romani, Paul N.
Other Authors: Observatoire de Paris, Université Paris Sciences et Lettres (PSL), Laboratoire d'études spatiales et d'instrumentation en astrophysique (LESIA), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université Paris Diderot - Paris 7 (UPD7)-Centre National de la Recherche Scientifique (CNRS), Pôle Planétologie du LESIA, Laboratoire d'études spatiales et d'instrumentation en astrophysique = Laboratory of Space Studies and Instrumentation in Astrophysics (LESIA), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Johns Hopkins University (JHU), NASA Goddard Space Flight Center (GSFC)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2006
Subjects:
Online Access:https://hal.science/hal-03742224
https://doi.org/10.1016/j.icarus.2006.05.018
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institution Open Polar
collection HAL Sorbonne Université
op_collection_id ftsorbonneuniv
language English
topic [PHYS.ASTR]Physics [physics]/Astrophysics [astro-ph]
spellingShingle [PHYS.ASTR]Physics [physics]/Astrophysics [astro-ph]
Lellouch, Emmanuel
Bézard, Bruno
Strobel, Darell
Bjoraker, Gordon L.
Flasar, Michael
Romani, Paul N.
On the HCN and CO 2 abundance and distribution in Jupiter's stratosphere
topic_facet [PHYS.ASTR]Physics [physics]/Astrophysics [astro-ph]
description International audience Observations of Jupiter by Cassini/CIRS, acquired during the December 2000 flyby, provide the latitudinal distribution of HCN and CO 2 in Jupiter's stratosphere with unprecedented spatial resolution and coverage. Following up on a preliminary study by Kunde et al. [Kunde, V.G., and 41 colleagues, 2004. Science 305, 1582-1587], the analysis of these observations leads to two unexpected results (i) the total HCN mass in Jupiter's stratosphere in 2000 was (6.0±1.5)×10 g, i.e., at least three times larger than measured immediately after the Shoemaker-Levy 9 (SL9) impacts in July 1994 and (ii) the latitudinal distributions of HCN and CO 2 are strikingly different: while HCN exhibits a maximum at 45° S and a sharp decrease towards high Southern latitudes, the CO 2 column densities peak over the South Pole. The total CO 2 mass is (2.9±1.2)×10 g. A possible cause for the HCN mass increase is its production from the photolysis of NH 3 , although a problem remains because, while millimeter-wave observations clearly indicate that HCN is currently restricted to submillibar ( ˜0.3 mbar) levels, immediate post-impact infrared observations have suggested that most of the ammonia was present in the lower stratosphere near 20 mbar. HCN appears to be a good atmospheric tracer, with negligible chemical losses. Based on 1-dimensional (latitude) transport models, the HCN distribution is best interpreted as resulting from the combination of a sharp decrease (over an order of magnitude in K) of wave-induced eddy mixing poleward of 40° and an equatorward transport with ˜7 cms velocity. The CO 2 distribution was investigated by coupling the transport model with an elementary chemical model, in which CO 2 is produced from the conversion of water originating either from SL9 or from auroral input. The auroral source does not appear adequate to reproduce the CO 2 peak over the South Pole, as required fluxes are unrealistically high and the shape of the CO 2 bulge is not properly matched. In contrast, the CO 2 ...
author2 Observatoire de Paris
Université Paris Sciences et Lettres (PSL)
Laboratoire d'études spatiales et d'instrumentation en astrophysique (LESIA)
Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université Paris Diderot - Paris 7 (UPD7)-Centre National de la Recherche Scientifique (CNRS)
Pôle Planétologie du LESIA
Laboratoire d'études spatiales et d'instrumentation en astrophysique = Laboratory of Space Studies and Instrumentation in Astrophysics (LESIA)
Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)
Johns Hopkins University (JHU)
NASA Goddard Space Flight Center (GSFC)
format Article in Journal/Newspaper
author Lellouch, Emmanuel
Bézard, Bruno
Strobel, Darell
Bjoraker, Gordon L.
Flasar, Michael
Romani, Paul N.
author_facet Lellouch, Emmanuel
Bézard, Bruno
Strobel, Darell
Bjoraker, Gordon L.
Flasar, Michael
Romani, Paul N.
author_sort Lellouch, Emmanuel
title On the HCN and CO 2 abundance and distribution in Jupiter's stratosphere
title_short On the HCN and CO 2 abundance and distribution in Jupiter's stratosphere
title_full On the HCN and CO 2 abundance and distribution in Jupiter's stratosphere
title_fullStr On the HCN and CO 2 abundance and distribution in Jupiter's stratosphere
title_full_unstemmed On the HCN and CO 2 abundance and distribution in Jupiter's stratosphere
title_sort on the hcn and co 2 abundance and distribution in jupiter's stratosphere
publisher HAL CCSD
publishDate 2006
url https://hal.science/hal-03742224
https://doi.org/10.1016/j.icarus.2006.05.018
genre South pole
genre_facet South pole
op_source ISSN: 0019-1035
EISSN: 1090-2643
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https://hal.science/hal-03742224
Icarus, 2006, 184, pp.478-497. ⟨10.1016/j.icarus.2006.05.018⟩
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container_title Icarus
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spelling ftsorbonneuniv:oai:HAL:hal-03742224v1 2024-09-15T18:36:45+00:00 On the HCN and CO 2 abundance and distribution in Jupiter's stratosphere Lellouch, Emmanuel Bézard, Bruno Strobel, Darell Bjoraker, Gordon L. Flasar, Michael Romani, Paul N. Observatoire de Paris Université Paris Sciences et Lettres (PSL) Laboratoire d'études spatiales et d'instrumentation en astrophysique (LESIA) Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université Paris Diderot - Paris 7 (UPD7)-Centre National de la Recherche Scientifique (CNRS) Pôle Planétologie du LESIA Laboratoire d'études spatiales et d'instrumentation en astrophysique = Laboratory of Space Studies and Instrumentation in Astrophysics (LESIA) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité) Johns Hopkins University (JHU) NASA Goddard Space Flight Center (GSFC) 2006 https://hal.science/hal-03742224 https://doi.org/10.1016/j.icarus.2006.05.018 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.icarus.2006.05.018 hal-03742224 https://hal.science/hal-03742224 BIBCODE: 2006Icar.184.478L doi:10.1016/j.icarus.2006.05.018 ISSN: 0019-1035 EISSN: 1090-2643 Icarus https://hal.science/hal-03742224 Icarus, 2006, 184, pp.478-497. ⟨10.1016/j.icarus.2006.05.018⟩ [PHYS.ASTR]Physics [physics]/Astrophysics [astro-ph] info:eu-repo/semantics/article Journal articles 2006 ftsorbonneuniv https://doi.org/10.1016/j.icarus.2006.05.018 2024-07-25T23:47:49Z International audience Observations of Jupiter by Cassini/CIRS, acquired during the December 2000 flyby, provide the latitudinal distribution of HCN and CO 2 in Jupiter's stratosphere with unprecedented spatial resolution and coverage. Following up on a preliminary study by Kunde et al. [Kunde, V.G., and 41 colleagues, 2004. Science 305, 1582-1587], the analysis of these observations leads to two unexpected results (i) the total HCN mass in Jupiter's stratosphere in 2000 was (6.0±1.5)×10 g, i.e., at least three times larger than measured immediately after the Shoemaker-Levy 9 (SL9) impacts in July 1994 and (ii) the latitudinal distributions of HCN and CO 2 are strikingly different: while HCN exhibits a maximum at 45° S and a sharp decrease towards high Southern latitudes, the CO 2 column densities peak over the South Pole. The total CO 2 mass is (2.9±1.2)×10 g. A possible cause for the HCN mass increase is its production from the photolysis of NH 3 , although a problem remains because, while millimeter-wave observations clearly indicate that HCN is currently restricted to submillibar ( ˜0.3 mbar) levels, immediate post-impact infrared observations have suggested that most of the ammonia was present in the lower stratosphere near 20 mbar. HCN appears to be a good atmospheric tracer, with negligible chemical losses. Based on 1-dimensional (latitude) transport models, the HCN distribution is best interpreted as resulting from the combination of a sharp decrease (over an order of magnitude in K) of wave-induced eddy mixing poleward of 40° and an equatorward transport with ˜7 cms velocity. The CO 2 distribution was investigated by coupling the transport model with an elementary chemical model, in which CO 2 is produced from the conversion of water originating either from SL9 or from auroral input. The auroral source does not appear adequate to reproduce the CO 2 peak over the South Pole, as required fluxes are unrealistically high and the shape of the CO 2 bulge is not properly matched. In contrast, the CO 2 ... Article in Journal/Newspaper South pole HAL Sorbonne Université Icarus 184 2 478 497