Cross-field transport due to low-frequency oscillations in the auroral region: A three-dimensional simulation
We have simulated the plasma transport processes in the nightside auroral region using our three‐dimensional (3‐D), multimoment, multifluid model. The model solves the continuity and momentum equations from 1500 km to 10 RE and allows self‐consistent treatment of the cross‐field transport. It has be...
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Veröffentlicht in: | Journal of Geophysical Research 1999-03, Vol.104 (A3), p.4297-4304 |
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creator | Ganguli, Supriya B. Guzdar, Parvez N. Gavrishchaka, Valeriy V. Krueger, Warren A. Blanchard, Paul E. |
description | We have simulated the plasma transport processes in the nightside auroral region using our three‐dimensional (3‐D), multimoment, multifluid model. The model solves the continuity and momentum equations from 1500 km to 10 RE and allows self‐consistent treatment of the cross‐field transport. It has been shown that the low‐frequency D'Angelo instability, driven by the transverse inhomogeneity in the magnetic‐field‐aligned ion flow, was excited for the typical parameters in the auroral region. The instability generates cross‐field transport, which significantly modifies the field‐aligned flow. The effects of cross‐field transport are discussed. In the nonlinear stage of the instability, V‐shaped potential structures with magnitudes ∼1 kV are formed. The simulation provides insight into the dynamical evolution of the D'Angelo instability in the ionosphere‐magnetosphere coupling region, its effects on plasma transport processes, and formation of 3‐D potential structures. |
doi_str_mv | 10.1029/1998JA900108 |
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The model solves the continuity and momentum equations from 1500 km to 10 RE and allows self‐consistent treatment of the cross‐field transport. It has been shown that the low‐frequency D'Angelo instability, driven by the transverse inhomogeneity in the magnetic‐field‐aligned ion flow, was excited for the typical parameters in the auroral region. The instability generates cross‐field transport, which significantly modifies the field‐aligned flow. The effects of cross‐field transport are discussed. In the nonlinear stage of the instability, V‐shaped potential structures with magnitudes ∼1 kV are formed. The simulation provides insight into the dynamical evolution of the D'Angelo instability in the ionosphere‐magnetosphere coupling region, its effects on plasma transport processes, and formation of 3‐D potential structures.</description><identifier>ISSN: 0148-0227</identifier><identifier>EISSN: 2156-2202</identifier><identifier>DOI: 10.1029/1998JA900108</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Interaction between ionosphere and magnetosphere ; Physics of the ionosphere</subject><ispartof>Journal of Geophysical Research, 1999-03, Vol.104 (A3), p.4297-4304</ispartof><rights>Copyright 1999 by the American Geophysical Union.</rights><rights>1999 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4447-17fac02e1b2874cd35565336204f8657af3f2927ea57742dc094ea0be577e2a3</citedby><cites>FETCH-LOGICAL-c4447-17fac02e1b2874cd35565336204f8657af3f2927ea57742dc094ea0be577e2a3</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%2F1998JA900108$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F1998JA900108$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,1433,11514,27924,27925,45574,45575,46409,46468,46833,46892</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=1737414$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Ganguli, Supriya B.</creatorcontrib><creatorcontrib>Guzdar, Parvez N.</creatorcontrib><creatorcontrib>Gavrishchaka, Valeriy V.</creatorcontrib><creatorcontrib>Krueger, Warren A.</creatorcontrib><creatorcontrib>Blanchard, Paul E.</creatorcontrib><title>Cross-field transport due to low-frequency oscillations in the auroral region: A three-dimensional simulation</title><title>Journal of Geophysical Research</title><addtitle>J. Geophys. Res</addtitle><description>We have simulated the plasma transport processes in the nightside auroral region using our three‐dimensional (3‐D), multimoment, multifluid model. The model solves the continuity and momentum equations from 1500 km to 10 RE and allows self‐consistent treatment of the cross‐field transport. It has been shown that the low‐frequency D'Angelo instability, driven by the transverse inhomogeneity in the magnetic‐field‐aligned ion flow, was excited for the typical parameters in the auroral region. The instability generates cross‐field transport, which significantly modifies the field‐aligned flow. The effects of cross‐field transport are discussed. In the nonlinear stage of the instability, V‐shaped potential structures with magnitudes ∼1 kV are formed. The simulation provides insight into the dynamical evolution of the D'Angelo instability in the ionosphere‐magnetosphere coupling region, its effects on plasma transport processes, and formation of 3‐D potential structures.</description><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Interaction between ionosphere and magnetosphere</subject><subject>Physics of the ionosphere</subject><issn>0148-0227</issn><issn>2156-2202</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1999</creationdate><recordtype>article</recordtype><recordid>eNqFkEFv1DAQhS1EJVbb3vgBPiBOmNoTO064rVaw0C6tVFXiaLnOGAxJvNiJyv77ukoFnGAu1jx_72n0CHkp-FvBoT0XbdtcbFrOBW-ekRUIVTMADs_JigvZMA6gX5CznL_zMlLVkosVGbYp5sx8wL6jU7JjPsQ00W5GOkXax3vmE_6ccXRHGrMLfW-nEMdMw0inb0jtnGKyPU34tcjv6KaoCZF1YcAxF6n85TDMi-2UnHjbZzx7etfk9sP72-1Htr_efdpu9sxJKTUT2lvHAcUdNFq6rlKqVlVVA5e-qZW2vvLQgkartJbQOd5KtPwOy4pgqzV5vcQeUiy358kMITsst48Y52ygboVuoPkvKBrBlRRtAd8soHusK6E3hxQGm45GcPNYv_m7_oK_esq12dnel15dyH88utJSyIJVC3Yfejz-M9Jc7G42QspiXRO2uEKe8Ndvl00_TF2ClflytTOfLy8Bdvsrw6sHmkCidQ</recordid><startdate>19990301</startdate><enddate>19990301</enddate><creator>Ganguli, Supriya B.</creator><creator>Guzdar, Parvez N.</creator><creator>Gavrishchaka, Valeriy V.</creator><creator>Krueger, Warren A.</creator><creator>Blanchard, Paul E.</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>KL.</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>19990301</creationdate><title>Cross-field transport due to low-frequency oscillations in the auroral region: A three-dimensional simulation</title><author>Ganguli, Supriya B. ; Guzdar, Parvez N. ; Gavrishchaka, Valeriy V. ; Krueger, Warren A. ; Blanchard, Paul E.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4447-17fac02e1b2874cd35565336204f8657af3f2927ea57742dc094ea0be577e2a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1999</creationdate><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Interaction between ionosphere and magnetosphere</topic><topic>Physics of the ionosphere</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ganguli, Supriya B.</creatorcontrib><creatorcontrib>Guzdar, Parvez N.</creatorcontrib><creatorcontrib>Gavrishchaka, Valeriy V.</creatorcontrib><creatorcontrib>Krueger, Warren A.</creatorcontrib><creatorcontrib>Blanchard, Paul E.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Journal of Geophysical Research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ganguli, Supriya B.</au><au>Guzdar, Parvez N.</au><au>Gavrishchaka, Valeriy V.</au><au>Krueger, Warren A.</au><au>Blanchard, Paul E.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Cross-field transport due to low-frequency oscillations in the auroral region: A three-dimensional simulation</atitle><jtitle>Journal of Geophysical Research</jtitle><addtitle>J. Geophys. Res</addtitle><date>1999-03-01</date><risdate>1999</risdate><volume>104</volume><issue>A3</issue><spage>4297</spage><epage>4304</epage><pages>4297-4304</pages><issn>0148-0227</issn><eissn>2156-2202</eissn><abstract>We have simulated the plasma transport processes in the nightside auroral region using our three‐dimensional (3‐D), multimoment, multifluid model. The model solves the continuity and momentum equations from 1500 km to 10 RE and allows self‐consistent treatment of the cross‐field transport. It has been shown that the low‐frequency D'Angelo instability, driven by the transverse inhomogeneity in the magnetic‐field‐aligned ion flow, was excited for the typical parameters in the auroral region. The instability generates cross‐field transport, which significantly modifies the field‐aligned flow. The effects of cross‐field transport are discussed. In the nonlinear stage of the instability, V‐shaped potential structures with magnitudes ∼1 kV are formed. The simulation provides insight into the dynamical evolution of the D'Angelo instability in the ionosphere‐magnetosphere coupling region, its effects on plasma transport processes, and formation of 3‐D potential structures.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/1998JA900108</doi><tpages>8</tpages><oa>free_for_read</oa></addata></record> |
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source | Wiley Free Content; Wiley-Blackwell AGU Digital Library; Wiley Online Library All Journals; Alma/SFX Local Collection |
subjects | Earth, ocean, space Exact sciences and technology External geophysics Interaction between ionosphere and magnetosphere Physics of the ionosphere |
title | Cross-field transport due to low-frequency oscillations in the auroral region: A three-dimensional simulation |
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