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...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Journal of the atmospheric sciences 2003-04, Vol.60 (8), p.993-1023
1. Verfasser: ORLANSKI, Isidoro
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 1023
container_issue 8
container_start_page 993
container_title Journal of the atmospheric sciences
container_volume 60
creator ORLANSKI, Isidoro
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
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_743088257</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>21365622</sourcerecordid><originalsourceid>FETCH-LOGICAL-c492t-2d3443c0f0d18b5b7c30115d44279df4fe2b069e7837674bfa291344d9124e363</originalsourceid><addsrcrecordid>eNp90VGL1DAQB_AgCq6n3yEo6vnQdTJJk_ROhLtl1cLCvehzSNMEcmbbNekK--1t2UNB0LzMy29mkvwJqRisGVP1e1YjVCBkc4kA_J2ED03Dr7rok4sfcQ1rN17jI7L67R6TFQBiJRrUT8mzUu5hPqjYirS3MRyzs1McBxoH6vv-RFMMnrqTS75c0XZ_SPEMCg1jpmUa855O2brv9KfN0XYxxen0nDwJNhX_4qFekG-ftl83X6rd3ed2c7Or3Lx-qrDnQnAHAXqmu7pTjgNjdS8EqqYPInjsQDZeaa6kEl2w2LC5pW8YCs8lvyBvz3MPefxx9GUy-1icT8kOfjwWowQHrbFWs3zzX4mMy1oizvDVX_B-POZhfoVBjTB_o6zZrF7-U3EpsNF6QdszcnksJftgDjnubT4ZBmZJzyypmCUVs6RnJJg5PXPbbneb1qABs7kzy5VePyyzxdkUsh1cLH-GCSVAS8V_AU4dmzk</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>236429881</pqid></control><display><type>article</type><title>Bifurcation in eddy life cycles: Implications for storm track variability</title><source>American Meteorological Society</source><source>Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals</source><source>Alma/SFX Local Collection</source><creator>ORLANSKI, Isidoro</creator><creatorcontrib>ORLANSKI, Isidoro</creatorcontrib><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><identifier>ISSN: 0022-4928</identifier><identifier>EISSN: 1520-0469</identifier><identifier>DOI: 10.1175/1520-0469(2003)60&lt;993:bielci&gt;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&amp;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 breaking</subject><subject>Weather</subject><issn>0022-4928</issn><issn>1520-0469</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>BEC</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNp90VGL1DAQB_AgCq6n3yEo6vnQdTJJk_ROhLtl1cLCvehzSNMEcmbbNekK--1t2UNB0LzMy29mkvwJqRisGVP1e1YjVCBkc4kA_J2ED03Dr7rok4sfcQ1rN17jI7L67R6TFQBiJRrUT8mzUu5hPqjYirS3MRyzs1McBxoH6vv-RFMMnrqTS75c0XZ_SPEMCg1jpmUa855O2brv9KfN0XYxxen0nDwJNhX_4qFekG-ftl83X6rd3ed2c7Or3Lx-qrDnQnAHAXqmu7pTjgNjdS8EqqYPInjsQDZeaa6kEl2w2LC5pW8YCs8lvyBvz3MPefxx9GUy-1icT8kOfjwWowQHrbFWs3zzX4mMy1oizvDVX_B-POZhfoVBjTB_o6zZrF7-U3EpsNF6QdszcnksJftgDjnubT4ZBmZJzyypmCUVs6RnJJg5PXPbbneb1qABs7kzy5VePyyzxdkUsh1cLH-GCSVAS8V_AU4dmzk</recordid><startdate>20030415</startdate><enddate>20030415</enddate><creator>ORLANSKI, Isidoro</creator><general>American Meteorological Society</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>7XB</scope><scope>88F</scope><scope>88I</scope><scope>8AF</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>L7M</scope><scope>M1Q</scope><scope>M2O</scope><scope>M2P</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>R05</scope><scope>S0X</scope></search><sort><creationdate>20030415</creationdate><title>Bifurcation 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 &amp; Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Military Database (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>STEM Database</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies &amp; Aerospace Collection</collection><collection>Agricultural &amp; Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>eLibrary</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aerospace Database</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Military Database</collection><collection>Research Library</collection><collection>Science Database</collection><collection>Research Library (Corporate)</collection><collection>Advanced Technologies &amp; Aerospace Database</collection><collection>ProQuest Advanced Technologies &amp; Aerospace Collection</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric &amp; Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>University of Michigan</collection><collection>SIRS Editorial</collection><jtitle>Journal of the atmospheric sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>ORLANSKI, Isidoro</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Bifurcation in eddy life cycles: Implications for storm track 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&lt;993:bielci&gt;2.0.co;2</doi><tpages>31</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0022-4928
ispartof Journal of the atmospheric sciences, 2003-04, Vol.60 (8), p.993-1023
issn 0022-4928
1520-0469
language eng
recordid cdi_proquest_miscellaneous_743088257
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
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-09T21%3A27%3A51IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Bifurcation%20in%20eddy%20life%20cycles:%20Implications%20for%20storm%20track%20variability&rft.jtitle=Journal%20of%20the%20atmospheric%20sciences&rft.au=ORLANSKI,%20Isidoro&rft.date=2003-04-15&rft.volume=60&rft.issue=8&rft.spage=993&rft.epage=1023&rft.pages=993-1023&rft.issn=0022-4928&rft.eissn=1520-0469&rft.coden=JAHSAK&rft_id=info:doi/10.1175/1520-0469(2003)60%3C993:bielci%3E2.0.co;2&rft_dat=%3Cproquest_cross%3E21365622%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=236429881&rft_id=info:pmid/&rfr_iscdi=true