Bifurcation in eddy life cycles: Implications for storm track variability
By analyzing a number of very high resolution, nonhydrostatic experiments of baroclinic lifecycles, it was concluded that the intensity of the near-surface baroclinic development influences the upper-level wave to such an extent that it could produce cyclonic or anticyclonic wave breaking. Since the...
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Veröffentlicht in: | Journal of the atmospheric sciences 2003-04, Vol.60 (8), p.993-1023 |
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description | By analyzing a number of very high resolution, nonhydrostatic experiments of baroclinic lifecycles, it was concluded that the intensity of the near-surface baroclinic development influences the upper-level wave to such an extent that it could produce cyclonic or anticyclonic wave breaking. Since the final jet position is equatorward or poleward, the position depends on whether the waves break cyclonically or anticyclonically, respectively. The low-level baroclinicity plays a very important role in the outcome of the wave and feedback to the mean circulation. Using a shallow water model the hypothesis that the intensity of the eddy forcing from the lower layers of the atmosphere can have a profound effect on the disturbances of the upper layers is tested. From these experiments the following is concluded. |
doi_str_mv | 10.1175/1520-0469(2003)60<993:bielci>2.0.co;2 |
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Since the final jet position is equatorward or poleward, the position depends on whether the waves break cyclonically or anticyclonically, respectively. The low-level baroclinicity plays a very important role in the outcome of the wave and feedback to the mean circulation. Using a shallow water model the hypothesis that the intensity of the eddy forcing from the lower layers of the atmosphere can have a profound effect on the disturbances of the upper layers is tested. From these experiments the following is concluded.</description><identifier>ISSN: 0022-4928</identifier><identifier>EISSN: 1520-0469</identifier><identifier>DOI: 10.1175/1520-0469(2003)60<993:bielci>2.0.co;2</identifier><identifier>CODEN: JAHSAK</identifier><language>eng</language><publisher>Boston, MA: American Meteorological Society</publisher><subject>Anticyclones ; Atmosphere ; Atmospheric pressure ; Baroclinic mode ; Baroclinity ; Barotropic mode ; Bifurcations ; Cyclones ; Cyclonic vortexes ; Earth, ocean, space ; Eddies ; El Nino ; El Nino phenomena ; El Nino-Southern Oscillation event ; Exact sciences and technology ; External geophysics ; Fluid dynamics ; Fluxes ; Fluxing ; Life cycle ; Life cycles ; Meteorology ; Moisture effects ; Moisture flux ; Other topics in atmospheric geophysics ; Physical simulation ; Shallow water ; Southern Oscillation ; Storm tracks ; Storms ; Upper level waves ; Variability ; Vortices ; Vorticity ; Water circulation ; Wave breaking ; Weather</subject><ispartof>Journal of the atmospheric sciences, 2003-04, Vol.60 (8), p.993-1023</ispartof><rights>2003 INIST-CNRS</rights><rights>Copyright American Meteorological Society Apr 15, 2003</rights><rights>Copyright American Meteorological Society 2003</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c492t-2d3443c0f0d18b5b7c30115d44279df4fe2b069e7837674bfa291344d9124e363</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,3668,27901,27902</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=14740867$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>ORLANSKI, Isidoro</creatorcontrib><title>Bifurcation in eddy life cycles: Implications for storm track variability</title><title>Journal of the atmospheric sciences</title><description>By analyzing a number of very high resolution, nonhydrostatic experiments of baroclinic lifecycles, it was concluded that the intensity of the near-surface baroclinic development influences the upper-level wave to such an extent that it could produce cyclonic or anticyclonic wave breaking. Since the final jet position is equatorward or poleward, the position depends on whether the waves break cyclonically or anticyclonically, respectively. The low-level baroclinicity plays a very important role in the outcome of the wave and feedback to the mean circulation. Using a shallow water model the hypothesis that the intensity of the eddy forcing from the lower layers of the atmosphere can have a profound effect on the disturbances of the upper layers is tested. From these experiments the following is concluded.</description><subject>Anticyclones</subject><subject>Atmosphere</subject><subject>Atmospheric pressure</subject><subject>Baroclinic mode</subject><subject>Baroclinity</subject><subject>Barotropic mode</subject><subject>Bifurcations</subject><subject>Cyclones</subject><subject>Cyclonic vortexes</subject><subject>Earth, ocean, space</subject><subject>Eddies</subject><subject>El Nino</subject><subject>El Nino phenomena</subject><subject>El Nino-Southern Oscillation event</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Fluid dynamics</subject><subject>Fluxes</subject><subject>Fluxing</subject><subject>Life cycle</subject><subject>Life cycles</subject><subject>Meteorology</subject><subject>Moisture effects</subject><subject>Moisture flux</subject><subject>Other topics in atmospheric geophysics</subject><subject>Physical simulation</subject><subject>Shallow water</subject><subject>Southern Oscillation</subject><subject>Storm tracks</subject><subject>Storms</subject><subject>Upper level waves</subject><subject>Variability</subject><subject>Vortices</subject><subject>Vorticity</subject><subject>Water circulation</subject><subject>Wave 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in eddy life cycles: Implications for storm track variability</title><author>ORLANSKI, Isidoro</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c492t-2d3443c0f0d18b5b7c30115d44279df4fe2b069e7837674bfa291344d9124e363</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2003</creationdate><topic>Anticyclones</topic><topic>Atmosphere</topic><topic>Atmospheric pressure</topic><topic>Baroclinic mode</topic><topic>Baroclinity</topic><topic>Barotropic mode</topic><topic>Bifurcations</topic><topic>Cyclones</topic><topic>Cyclonic vortexes</topic><topic>Earth, ocean, space</topic><topic>Eddies</topic><topic>El Nino</topic><topic>El Nino phenomena</topic><topic>El Nino-Southern Oscillation event</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Fluid dynamics</topic><topic>Fluxes</topic><topic>Fluxing</topic><topic>Life cycle</topic><topic>Life cycles</topic><topic>Meteorology</topic><topic>Moisture effects</topic><topic>Moisture flux</topic><topic>Other topics in atmospheric geophysics</topic><topic>Physical simulation</topic><topic>Shallow water</topic><topic>Southern Oscillation</topic><topic>Storm tracks</topic><topic>Storms</topic><topic>Upper level waves</topic><topic>Variability</topic><topic>Vortices</topic><topic>Vorticity</topic><topic>Water circulation</topic><topic>Wave breaking</topic><topic>Weather</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>ORLANSKI, Isidoro</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Military Database (Alumni 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variability</atitle><jtitle>Journal of the atmospheric sciences</jtitle><date>2003-04-15</date><risdate>2003</risdate><volume>60</volume><issue>8</issue><spage>993</spage><epage>1023</epage><pages>993-1023</pages><issn>0022-4928</issn><eissn>1520-0469</eissn><coden>JAHSAK</coden><abstract>By analyzing a number of very high resolution, nonhydrostatic experiments of baroclinic lifecycles, it was concluded that the intensity of the near-surface baroclinic development influences the upper-level wave to such an extent that it could produce cyclonic or anticyclonic wave breaking. Since the final jet position is equatorward or poleward, the position depends on whether the waves break cyclonically or anticyclonically, respectively. The low-level baroclinicity plays a very important role in the outcome of the wave and feedback to the mean circulation. Using a shallow water model the hypothesis that the intensity of the eddy forcing from the lower layers of the atmosphere can have a profound effect on the disturbances of the upper layers is tested. From these experiments the following is concluded.</abstract><cop>Boston, MA</cop><pub>American Meteorological Society</pub><doi>10.1175/1520-0469(2003)60<993:bielci>2.0.co;2</doi><tpages>31</tpages><oa>free_for_read</oa></addata></record> |
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source | American Meteorological Society; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Alma/SFX Local Collection |
subjects | Anticyclones Atmosphere Atmospheric pressure Baroclinic mode Baroclinity Barotropic mode Bifurcations Cyclones Cyclonic vortexes Earth, ocean, space Eddies El Nino El Nino phenomena El Nino-Southern Oscillation event Exact sciences and technology External geophysics Fluid dynamics Fluxes Fluxing Life cycle Life cycles Meteorology Moisture effects Moisture flux Other topics in atmospheric geophysics Physical simulation Shallow water Southern Oscillation Storm tracks Storms Upper level waves Variability Vortices Vorticity Water circulation Wave breaking Weather |
title | Bifurcation in eddy life cycles: Implications for storm track variability |
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