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Baroclinic Model of Jupiter’s Great Red Spot
This paper proposes a quasi-geostrophic baroclinic model of Jupiter’s Great Red Spot (GRS) as a localized eddy formation in a continuously stratified rotating atmosphere under the action of a horizontal shear flow in the f -plane approximation. On the basis of the theory of ellipsoidal vortices, an...
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Published in: | Izvestiya. Atmospheric and oceanic physics 2023-06, Vol.59 (3), p.243-254 |
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creator | Suetin, B. P. Zhmur, V. V. Chkhetiani, O. G. |
description | This paper proposes a quasi-geostrophic baroclinic model of Jupiter’s Great Red Spot (GRS) as a localized eddy formation in a continuously stratified rotating atmosphere under the action of a horizontal shear flow in the
f
-plane approximation. On the basis of the theory of ellipsoidal vortices, an analytical relationship is obtained between the geometric dimensions of the vortex, the potential vorticity of the vortex core, and the characteristics of the background flow. Measurements of a number of characteristics of both the vortex and the background flow in the Voyager 1 (1979), Galileo (1996), and Cassini (2000) missions were used. Based on the theory, the vertical size of the GRS was calculated, which turned out to be close to the same characteristic measured in the Voyager 1 (1979) mission. |
doi_str_mv | 10.1134/S0001433823030088 |
format | article |
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f
-plane approximation. On the basis of the theory of ellipsoidal vortices, an analytical relationship is obtained between the geometric dimensions of the vortex, the potential vorticity of the vortex core, and the characteristics of the background flow. Measurements of a number of characteristics of both the vortex and the background flow in the Voyager 1 (1979), Galileo (1996), and Cassini (2000) missions were used. Based on the theory, the vertical size of the GRS was calculated, which turned out to be close to the same characteristic measured in the Voyager 1 (1979) mission.</description><identifier>ISSN: 0001-4338</identifier><identifier>EISSN: 1555-628X</identifier><identifier>DOI: 10.1134/S0001433823030088</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Approximation ; Climatology ; Earth and Environmental Science ; Earth Sciences ; Eddy formation ; Fluid flow ; Geophysics/Geodesy ; Jupiter ; Jupiter red spot ; Potential vorticity ; Shear flow ; Space missions ; Vortices ; Vorticity</subject><ispartof>Izvestiya. Atmospheric and oceanic physics, 2023-06, Vol.59 (3), p.243-254</ispartof><rights>Pleiades Publishing, Ltd. 2023. ISSN 0001-4338, Izvestiya, Atmospheric and Oceanic Physics, 2023, Vol. 59, No. 3, pp. 243–254. © Pleiades Publishing, Ltd., 2023. Russian Text © The Author(s), 2023, published in Izvestiya Rossiiskoi Akademii Nauk, Fizika Atmosfery i Okeana, 2023, Vol. 59, No. 3, pp. 286–298.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c268t-8fe1d7786351339b5f86bc505ae79b975a404a958889659f24dfd4da818fdba63</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,777,781,27905,27906</link.rule.ids></links><search><creatorcontrib>Suetin, B. P.</creatorcontrib><creatorcontrib>Zhmur, V. V.</creatorcontrib><creatorcontrib>Chkhetiani, O. G.</creatorcontrib><title>Baroclinic Model of Jupiter’s Great Red Spot</title><title>Izvestiya. Atmospheric and oceanic physics</title><addtitle>Izv. Atmos. Ocean. Phys</addtitle><description>This paper proposes a quasi-geostrophic baroclinic model of Jupiter’s Great Red Spot (GRS) as a localized eddy formation in a continuously stratified rotating atmosphere under the action of a horizontal shear flow in the
f
-plane approximation. On the basis of the theory of ellipsoidal vortices, an analytical relationship is obtained between the geometric dimensions of the vortex, the potential vorticity of the vortex core, and the characteristics of the background flow. Measurements of a number of characteristics of both the vortex and the background flow in the Voyager 1 (1979), Galileo (1996), and Cassini (2000) missions were used. Based on the theory, the vertical size of the GRS was calculated, which turned out to be close to the same characteristic measured in the Voyager 1 (1979) mission.</description><subject>Approximation</subject><subject>Climatology</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Eddy formation</subject><subject>Fluid flow</subject><subject>Geophysics/Geodesy</subject><subject>Jupiter</subject><subject>Jupiter red spot</subject><subject>Potential vorticity</subject><subject>Shear flow</subject><subject>Space missions</subject><subject>Vortices</subject><subject>Vorticity</subject><issn>0001-4338</issn><issn>1555-628X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNp1kM1Kw0AUhQdRsFYfwF3Adeqd39xZatGqVASr4C5MMjOSUjtxJl2462v4ej6JDRFciKu7ON93LhxCTilMKOXifAEAVHCOjAMHQNwjIyqlzBXDl30y6uO8zw_JUUpLAMUEFCMyuTQx1Ktm3dTZfbBulQWf3W3apnPxa_uZsll0pssenc0WbeiOyYE3q-ROfu6YPF9fPU1v8vnD7HZ6Mc9rprDL0TtqiwIVl5RzXUmPqqolSOMKXelCGgHCaImIWkntmbDeCmuQoreVUXxMzobeNob3jUtduQybuN69LBkKJoXguqfoQNUxpBSdL9vYvJn4UVIo-1nKP7PsHDY4aceuX138bf5f-gafOWI9</recordid><startdate>20230601</startdate><enddate>20230601</enddate><creator>Suetin, B. P.</creator><creator>Zhmur, V. V.</creator><creator>Chkhetiani, O. G.</creator><general>Pleiades Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>20230601</creationdate><title>Baroclinic Model of Jupiter’s Great Red Spot</title><author>Suetin, B. P. ; Zhmur, V. V. ; Chkhetiani, O. G.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c268t-8fe1d7786351339b5f86bc505ae79b975a404a958889659f24dfd4da818fdba63</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Approximation</topic><topic>Climatology</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Eddy formation</topic><topic>Fluid flow</topic><topic>Geophysics/Geodesy</topic><topic>Jupiter</topic><topic>Jupiter red spot</topic><topic>Potential vorticity</topic><topic>Shear flow</topic><topic>Space missions</topic><topic>Vortices</topic><topic>Vorticity</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Suetin, B. P.</creatorcontrib><creatorcontrib>Zhmur, V. V.</creatorcontrib><creatorcontrib>Chkhetiani, O. G.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Izvestiya. Atmospheric and oceanic physics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Suetin, B. P.</au><au>Zhmur, V. V.</au><au>Chkhetiani, O. G.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Baroclinic Model of Jupiter’s Great Red Spot</atitle><jtitle>Izvestiya. Atmospheric and oceanic physics</jtitle><stitle>Izv. Atmos. Ocean. Phys</stitle><date>2023-06-01</date><risdate>2023</risdate><volume>59</volume><issue>3</issue><spage>243</spage><epage>254</epage><pages>243-254</pages><issn>0001-4338</issn><eissn>1555-628X</eissn><abstract>This paper proposes a quasi-geostrophic baroclinic model of Jupiter’s Great Red Spot (GRS) as a localized eddy formation in a continuously stratified rotating atmosphere under the action of a horizontal shear flow in the
f
-plane approximation. On the basis of the theory of ellipsoidal vortices, an analytical relationship is obtained between the geometric dimensions of the vortex, the potential vorticity of the vortex core, and the characteristics of the background flow. Measurements of a number of characteristics of both the vortex and the background flow in the Voyager 1 (1979), Galileo (1996), and Cassini (2000) missions were used. Based on the theory, the vertical size of the GRS was calculated, which turned out to be close to the same characteristic measured in the Voyager 1 (1979) mission.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S0001433823030088</doi><tpages>12</tpages></addata></record> |
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subjects | Approximation Climatology Earth and Environmental Science Earth Sciences Eddy formation Fluid flow Geophysics/Geodesy Jupiter Jupiter red spot Potential vorticity Shear flow Space missions Vortices Vorticity |
title | Baroclinic Model of Jupiter’s Great Red Spot |
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