Diversity of microenvironments and the complexity of vortex motion
The complexity of major vortex motion in a system where four scales are coexisting (a subtropical high ridge, the major vortex, meso‐ and small‐scale vortices) is examined numerically using a barotropic primitive equation model. The microenvironment of a major vortex consists of a group of small‐sca...
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| Veröffentlicht in: | Geophysical research letters 2006-12, Vol.33 (24), p.np-n/a |
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| creator | Luo, Zhexian Liu, Chongjian |
| description | The complexity of major vortex motion in a system where four scales are coexisting (a subtropical high ridge, the major vortex, meso‐ and small‐scale vortices) is examined numerically using a barotropic primitive equation model. The microenvironment of a major vortex consists of a group of small‐scale vortices in which varying values for the total number N of initial small‐scale vortices (N = 2, 3, 4, and 5, respectively) creates a diverse range of microenvironments. Three kinds of major vortex motion are observed: (i) the initial major vortex decays away with no new major vortex formation; (ii) a weak new major vortex forms while the major vortex decays; and (iii) a new major vortex occurs, via self‐organization, with its intensity and scale similar to those in the initial stages of the original major vortex, and this vortex continues to shift westwards after the old major vortex decays. |
| doi_str_mv | 10.1029/2006GL027765 |
| format | Article |
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The microenvironment of a major vortex consists of a group of small‐scale vortices in which varying values for the total number N of initial small‐scale vortices (N = 2, 3, 4, and 5, respectively) creates a diverse range of microenvironments. Three kinds of major vortex motion are observed: (i) the initial major vortex decays away with no new major vortex formation; (ii) a weak new major vortex forms while the major vortex decays; and (iii) a new major vortex occurs, via self‐organization, with its intensity and scale similar to those in the initial stages of the original major vortex, and this vortex continues to shift westwards after the old major vortex decays.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/2006GL027765</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>chaos ; Complexity ; Decay ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Fluid flow ; Geophysics ; Mathematical models ; Primitive equations ; Ridges ; sensitivity ; vortex ; Vortices</subject><ispartof>Geophysical research letters, 2006-12, Vol.33 (24), p.np-n/a</ispartof><rights>Copyright 2006 by the American Geophysical Union.</rights><rights>2007 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4178-40412bbc46695c392eb6c4ab957faf6d3b9fc2221ec4290d4820f80c9b3805b93</citedby><cites>FETCH-LOGICAL-c4178-40412bbc46695c392eb6c4ab957faf6d3b9fc2221ec4290d4820f80c9b3805b93</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2006GL027765$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2006GL027765$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,1427,11493,27901,27902,45550,45551,46384,46443,46808,46867</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=18517343$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Luo, Zhexian</creatorcontrib><creatorcontrib>Liu, Chongjian</creatorcontrib><title>Diversity of microenvironments and the complexity of vortex motion</title><title>Geophysical research letters</title><addtitle>Geophys. 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Three kinds of major vortex motion are observed: (i) the initial major vortex decays away with no new major vortex formation; (ii) a weak new major vortex forms while the major vortex decays; and (iii) a new major vortex occurs, via self‐organization, with its intensity and scale similar to those in the initial stages of the original major vortex, and this vortex continues to shift westwards after the old major vortex decays.</description><subject>chaos</subject><subject>Complexity</subject><subject>Decay</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Fluid flow</subject><subject>Geophysics</subject><subject>Mathematical models</subject><subject>Primitive equations</subject><subject>Ridges</subject><subject>sensitivity</subject><subject>vortex</subject><subject>Vortices</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNp9kD1PwzAURS0EEqWw8QOyIDEQeP6IHY9QIAVVICEQo-W4jjAkcbHT0v57UrUCJqb3hnOudC9CxxjOMRB5QQB4MQEiBM920ABLxtIcQOyiAYDsfyL4PjqI8R0AKFA8QFfXbmFDdN0q8VXSOBO8bRcu-LaxbRcT3U6T7s0mxjez2i633MKHzi6TxnfOt4dor9J1tEfbO0QvtzfPo3E6eSzuRpeT1DAs8pQBw6QsDeNcZoZKYktumC5lJipd8SktZWUIIdgaRiRMWU6gysHIkuaQlZIO0ekmdxb859zGTjUuGlvXurV-HhXOKEiZAV-jZxu0rxNjsJWaBdfosFIY1Hoq9XeqHj_ZJutodF0F3RoXf508w4Iy2nNkw3252q7-zVTF06QvI_JeSjeSi_1mP5IOH4oLKjL1-lCoexiPCwqgJP0GkZmFfw</recordid><startdate>200612</startdate><enddate>200612</enddate><creator>Luo, Zhexian</creator><creator>Liu, Chongjian</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope></search><sort><creationdate>200612</creationdate><title>Diversity of microenvironments and the complexity of vortex motion</title><author>Luo, Zhexian ; Liu, Chongjian</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4178-40412bbc46695c392eb6c4ab957faf6d3b9fc2221ec4290d4820f80c9b3805b93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>chaos</topic><topic>Complexity</topic><topic>Decay</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Fluid flow</topic><topic>Geophysics</topic><topic>Mathematical models</topic><topic>Primitive equations</topic><topic>Ridges</topic><topic>sensitivity</topic><topic>vortex</topic><topic>Vortices</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Luo, Zhexian</creatorcontrib><creatorcontrib>Liu, Chongjian</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Luo, Zhexian</au><au>Liu, Chongjian</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Diversity of microenvironments and the complexity of vortex motion</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>2006-12</date><risdate>2006</risdate><volume>33</volume><issue>24</issue><spage>np</spage><epage>n/a</epage><pages>np-n/a</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>The complexity of major vortex motion in a system where four scales are coexisting (a subtropical high ridge, the major vortex, meso‐ and small‐scale vortices) is examined numerically using a barotropic primitive equation model. The microenvironment of a major vortex consists of a group of small‐scale vortices in which varying values for the total number N of initial small‐scale vortices (N = 2, 3, 4, and 5, respectively) creates a diverse range of microenvironments. Three kinds of major vortex motion are observed: (i) the initial major vortex decays away with no new major vortex formation; (ii) a weak new major vortex forms while the major vortex decays; and (iii) a new major vortex occurs, via self‐organization, with its intensity and scale similar to those in the initial stages of the original major vortex, and this vortex continues to shift westwards after the old major vortex decays.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2006GL027765</doi><tpages>6</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | chaos Complexity Decay Earth sciences Earth, ocean, space Exact sciences and technology Fluid flow Geophysics Mathematical models Primitive equations Ridges sensitivity vortex Vortices |
| title | Diversity of microenvironments and the complexity of vortex motion |
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