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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Main Authors: | , , , , , |
Other Authors: | , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2006
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Online Access: | https://hal.science/hal-03742224 https://doi.org/10.1016/j.icarus.2006.05.018 |
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Université de Paris: Portail HAL |
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ftunivparis |
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 Icarus https://hal.science/hal-03742224 Icarus, 2006, 184, pp.478-497. ⟨10.1016/j.icarus.2006.05.018⟩ |
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op_doi |
https://doi.org/10.1016/j.icarus.2006.05.018 |
container_title |
Icarus |
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184 |
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2 |
container_start_page |
478 |
op_container_end_page |
497 |
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1799466950946979840 |
spelling |
ftunivparis:oai:HAL:hal-03742224v1 2024-05-19T07:48:39+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 ftunivparis https://doi.org/10.1016/j.icarus.2006.05.018 2024-04-23T03:36:00Z 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 Université de Paris: Portail HAL Icarus 184 2 478 497 |