{"title":"A full-atmosphere model of Jupiter","authors":"Antonín Knížek , Paul B. Rimmer , Martin Ferus","doi":"10.1016/j.icarus.2025.116806","DOIUrl":null,"url":null,"abstract":"<div><div>This paper presents a combined 1D photochemical–thermochemical kinetics model of Jupiter’s deeper atmosphere, troposphere and stratosphere. The model covers atmospheric pressure range from <span><math><mrow><mn>1</mn><mo>.</mo><mn>1</mn><mo>×</mo><mn>1</mn><msup><mrow><mn>0</mn></mrow><mrow><mn>3</mn></mrow></msup></mrow></math></span> bar to <span><math><mrow><mn>7</mn><mo>.</mo><mn>4</mn><mo>×</mo><mn>1</mn><msup><mrow><mn>0</mn></mrow><mrow><mo>−</mo><mn>11</mn></mrow></msup></mrow></math></span> bar and is the first model that incorporates sulfur chemistry when spanning an atmospheric region of this extent. This model incorporates a new version of the STAND reaction network with updated NH<sub>4</sub>SH chemistry, and updated Antoine equation parameters for NH<sub>4</sub>SH and H<sub>2</sub>S. Validation against current models of Jupiter’s atmosphere as well as recent observational data shows that our model successfully describes Jupiter’s main observed chemical features. Since one of the focuses of the model is the chemistry on nitrogen, it correctly predicts the formation of a mixed NH<sub>3</sub>-NH<sub>4</sub>SH cloud layer between 0.1 and 1 bar. It also describes the chemistry of HCN throughout the atmosphere and discovers a region in the stratosphere between <span><math><mrow><mn>1</mn><mo>×</mo><mn>1</mn><msup><mrow><mn>0</mn></mrow><mrow><mo>−</mo><mn>6</mn></mrow></msup></mrow></math></span> and <span><math><mrow><mn>6</mn><mo>.</mo><mn>76</mn><mo>×</mo><mn>1</mn><msup><mrow><mn>0</mn></mrow><mrow><mo>−</mo><mn>8</mn></mrow></msup></mrow></math></span> bar, where HCN forms through radical chemistry with maximum mixing ratio 33 ppb at <span><math><mrow><mn>2</mn><mo>.</mo><mn>94</mn><mo>×</mo><mn>1</mn><msup><mrow><mn>0</mn></mrow><mrow><mo>−</mo><mn>7</mn></mrow></msup></mrow></math></span> bar – a prediction testable by observations. At the same time, our model predicts a quenched N<sub>2</sub> mixing ratio 490 ppm up to 10<sup>−6</sup> bar. The model therefore successfully bridges the gap between existing models of separate regions of Jupiter’s atmosphere and makes new testable predictions of several chemical species.</div></div>","PeriodicalId":13199,"journal":{"name":"Icarus","volume":"444 ","pages":"Article 116806"},"PeriodicalIF":3.0000,"publicationDate":"2025-09-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Icarus","FirstCategoryId":"101","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0019103525003549","RegionNum":2,"RegionCategory":"物理与天体物理","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ASTRONOMY & ASTROPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
This paper presents a combined 1D photochemical–thermochemical kinetics model of Jupiter’s deeper atmosphere, troposphere and stratosphere. The model covers atmospheric pressure range from bar to bar and is the first model that incorporates sulfur chemistry when spanning an atmospheric region of this extent. This model incorporates a new version of the STAND reaction network with updated NH4SH chemistry, and updated Antoine equation parameters for NH4SH and H2S. Validation against current models of Jupiter’s atmosphere as well as recent observational data shows that our model successfully describes Jupiter’s main observed chemical features. Since one of the focuses of the model is the chemistry on nitrogen, it correctly predicts the formation of a mixed NH3-NH4SH cloud layer between 0.1 and 1 bar. It also describes the chemistry of HCN throughout the atmosphere and discovers a region in the stratosphere between and bar, where HCN forms through radical chemistry with maximum mixing ratio 33 ppb at bar – a prediction testable by observations. At the same time, our model predicts a quenched N2 mixing ratio 490 ppm up to 10−6 bar. The model therefore successfully bridges the gap between existing models of separate regions of Jupiter’s atmosphere and makes new testable predictions of several chemical species.
期刊介绍:
Icarus is devoted to the publication of original contributions in the field of Solar System studies. Manuscripts reporting the results of new research - observational, experimental, or theoretical - concerning the astronomy, geology, meteorology, physics, chemistry, biology, and other scientific aspects of our Solar System or extrasolar systems are welcome. The journal generally does not publish papers devoted exclusively to the Sun, the Earth, celestial mechanics, meteoritics, or astrophysics. Icarus does not publish papers that provide "improved" versions of Bode''s law, or other numerical relations, without a sound physical basis. Icarus does not publish meeting announcements or general notices. Reviews, historical papers, and manuscripts describing spacecraft instrumentation may be considered, but only with prior approval of the editor. An entire issue of the journal is occasionally devoted to a single subject, usually arising from a conference on the same topic. The language of publication is English. American or British usage is accepted, but not a mixture of these.