{"refrec":{"BRefID":338157,"RR":"<b>Carone, L.; Keppens, R.; Decin, L.; Henning, T.</b> (2018). Stratosphere circulation on tidally locked ExoEarths. <i>Monthly Notices of the Royal Astronomical Society 473(4)</i>: 4672-4685. <a href=\"https://hdl.handle.net/10.1093/mnras/stx2732\" target=\"_blank\">https://hdl.handle.net/10.1093/mnras/stx2732</a>","BEntID":334782,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Monthly Notices of the Royal Astronomical Society 473(4)</i>: 4672-4685. <a href=\"https://hdl.handle.net/10.1093/mnras/stx2732\" target=\"_blank\">https://hdl.handle.net/10.1093/mnras/stx2732</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Carone, L.; Keppens, R.; Decin, L.; Henning, T.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Carone, L. <i>et al.</i>","Englishabstract":"<p class=\"chapter-para\">Stratosphere circulation is important to interpret abundances of photochemically produced compounds like ozone which we aim to observe to assess habitability of exoplanets. We thus investigate a tidally locked ExoEarth scenario for TRAPPIST-1b, TRAPPIST-1d, Proxima Centauri b and GJ 667 C f with a simplified 3D atmosphere model and for different stratospheric wind breaking assumptions.</p><p class=\"chapter-para\">These planets are representatives for different circulation regimes for orbital periods: <em>P</em><sub>orb</sub> = 1–100  d. The circulation of exoplanets with <em>P</em><sub>orb</sub> ≤ 25 d can be dominated by the standing tropical Rossby wave in the troposphere and also in the stratosphere: It leads to a strong equatorial eastward wind jet and to an ‘Anti-Brewer-Dobson’-circulation that confines airmasses to the stratospheric equatorial region. Thus, the distribution of photochemically produced species and aerosols may be limited to an ‘equatorial transport belt’. In contrast, planets with <em>P</em><sub>orb</sub> > 25  d, like GJ 667 C f, exhibit efficient thermally driven circulation in the stratosphere which allows for a day side-wide distribution of airmasses.</p><p class=\"chapter-para\">The influence of the standing tropical Rossby waves on tidally locked ExoEarths with <em>P</em><sub>orb</sub> ≤ 25  d can, however, be circumvented with deep stratospheric wind breaking alone – allowing for equator-to-pole transport like on Earth. For planets with 3 ≤ <em>P</em><sub>orb</sub> ≤ 6  d, the extratropical Rossby wave acts as an additional safeguard against the tropical Rossby wave in case of shallow wind breaking. Therefore, TRAPPIST-1d is less prone to have an equatorial transport belt in the stratosphere than Proxima Centauri b.</p><p class=\"chapter-para\">Even our Earth model shows an equatorial wind jet, if stratosphere wind breaking is inefficient.</p>","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Stratosphere circulation on tidally locked ExoEarths","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"methods: numerical; planets and satellites: atmospheres","OtherDescriptors":null,"Notes":null,"AnaPub":2018,"MonPub":null,"DateUpdate":"2021-09-08","DateCreate":"2021-05-17","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000424117300029","VABBcode":null,"OpenAcc":0,"Handle":"10.1093/mnras/stx2732"},"refs":null,"anarec":{"AnaID":338157,"PubliDate":2018,"Pagination":"4672-4685","XtraPublOfAnaID":null,"ISBN":null,"Volume":"473","Issue":"4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":274984,"SerRR":"Monthly Notices of the Royal Astronomical Society. 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