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The Dawn‐Dusk Asymmetry of the Interaction Between Dipolarizing Flux Bundles and the Ambient Plasma: Implications for Asymmetric Wedgelets

The substorm current wedge (SCW), the characteristic current system of Earth's substorms, has been suggested to be a collective effect of many “wedgelets,” mesoscale currents carried by magnetotail flux tubes of strong magnetic fields called dipolarizing flux bundles (DFBs). Each wedgelet conta...

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Published in:Geophysical research letters 2023-08, Vol.50 (15), p.n/a
Main Author: Liu, Jiang
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description The substorm current wedge (SCW), the characteristic current system of Earth's substorms, has been suggested to be a collective effect of many “wedgelets,” mesoscale currents carried by magnetotail flux tubes of strong magnetic fields called dipolarizing flux bundles (DFBs). Each wedgelet contains an asymmetric pair of field‐aligned currents (FACs) so the net FAC of many wedgelets can equal an SCW's FAC content. It is unclear, however, why a wedgelet's FAC is asymmetric. To explore the reason, we investigate how earthward‐traveling DFBs interact with ambient plasma because this interaction leads to their FACs. The interaction is manifested as the pressure and magnetic field distributions around DFBs, which we examine statistically using THEMIS data. The statistical distributions are consistent with an interplay between the DFB‐caused mesoscale perturbations and the global magnetotail configuration and favor the rise of wedgelets' asymmetric FACs. This result reveals the importance of cross‐scale coupling in SCW formation. Plain Language Summary The electric current system of one of the most important energy release events in Earth's near‐space provides valuable information on how such events proceed. Previous studies showed that the current system consists of small elements with unexpected but necessary asymmetries. To understand how such asymmetries are formed, we examine the space plasma environment related to them using spacecraft data. The plasma environment suggests that the asymmetries arise from an interaction between small and global‐scale phenomena, indicating the importance of cross‐scale coupling in understanding the geospace. Key Points We examine the statistical distribution of pressure and magnetic field strength around dipolarizing flux bundles (DFBs) using THEMIS data Around a DFB in the dusk (dawn) sector of the magnetotail, the quantities are larger on its morning (evening) side This asymmetric distribution suggests an interplay between meso and global scales and favors asymmetric wedgelets as previously found
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Each wedgelet contains an asymmetric pair of field‐aligned currents (FACs) so the net FAC of many wedgelets can equal an SCW's FAC content. It is unclear, however, why a wedgelet's FAC is asymmetric. To explore the reason, we investigate how earthward‐traveling DFBs interact with ambient plasma because this interaction leads to their FACs. The interaction is manifested as the pressure and magnetic field distributions around DFBs, which we examine statistically using THEMIS data. The statistical distributions are consistent with an interplay between the DFB‐caused mesoscale perturbations and the global magnetotail configuration and favor the rise of wedgelets' asymmetric FACs. This result reveals the importance of cross‐scale coupling in SCW formation. Plain Language Summary The electric current system of one of the most important energy release events in Earth's near‐space provides valuable information on how such events proceed. Previous studies showed that the current system consists of small elements with unexpected but necessary asymmetries. To understand how such asymmetries are formed, we examine the space plasma environment related to them using spacecraft data. The plasma environment suggests that the asymmetries arise from an interaction between small and global‐scale phenomena, indicating the importance of cross‐scale coupling in understanding the geospace. Key Points We examine the statistical distribution of pressure and magnetic field strength around dipolarizing flux bundles (DFBs) using THEMIS data Around a DFB in the dusk (dawn) sector of the magnetotail, the quantities are larger on its morning (evening) side This asymmetric distribution suggests an interplay between meso and global scales and favors asymmetric wedgelets as previously found</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/2023GL103957</identifier><language>eng</language><publisher>Washington: John Wiley &amp; Sons, Inc</publisher><subject>Asymmetry ; Coupling ; current generation ; dawn‐dusk asymmetry ; dipolarizaing flux bundle ; dipolarization front ; Earth ; Electric currents ; Fluctuations ; Magnetic field ; Magnetic fields ; Magnetotails ; Mesoscale phenomena ; Perturbation ; Plasma ; Space plasmas ; Spacecraft ; Statistical distributions ; substorm current wedge ; Tubes ; wedgelet</subject><ispartof>Geophysical research letters, 2023-08, Vol.50 (15), p.n/a</ispartof><rights>2023. 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Each wedgelet contains an asymmetric pair of field‐aligned currents (FACs) so the net FAC of many wedgelets can equal an SCW's FAC content. It is unclear, however, why a wedgelet's FAC is asymmetric. To explore the reason, we investigate how earthward‐traveling DFBs interact with ambient plasma because this interaction leads to their FACs. The interaction is manifested as the pressure and magnetic field distributions around DFBs, which we examine statistically using THEMIS data. The statistical distributions are consistent with an interplay between the DFB‐caused mesoscale perturbations and the global magnetotail configuration and favor the rise of wedgelets' asymmetric FACs. This result reveals the importance of cross‐scale coupling in SCW formation. Plain Language Summary The electric current system of one of the most important energy release events in Earth's near‐space provides valuable information on how such events proceed. Previous studies showed that the current system consists of small elements with unexpected but necessary asymmetries. To understand how such asymmetries are formed, we examine the space plasma environment related to them using spacecraft data. The plasma environment suggests that the asymmetries arise from an interaction between small and global‐scale phenomena, indicating the importance of cross‐scale coupling in understanding the geospace. Key Points We examine the statistical distribution of pressure and magnetic field strength around dipolarizing flux bundles (DFBs) using THEMIS data Around a DFB in the dusk (dawn) sector of the magnetotail, the quantities are larger on its morning (evening) side This asymmetric distribution suggests an interplay between meso and global scales and favors asymmetric wedgelets as previously found</description><subject>Asymmetry</subject><subject>Coupling</subject><subject>current generation</subject><subject>dawn‐dusk asymmetry</subject><subject>dipolarizaing flux bundle</subject><subject>dipolarization front</subject><subject>Earth</subject><subject>Electric currents</subject><subject>Fluctuations</subject><subject>Magnetic field</subject><subject>Magnetic fields</subject><subject>Magnetotails</subject><subject>Mesoscale phenomena</subject><subject>Perturbation</subject><subject>Plasma</subject><subject>Space plasmas</subject><subject>Spacecraft</subject><subject>Statistical distributions</subject><subject>substorm current wedge</subject><subject>Tubes</subject><subject>wedgelet</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>24P</sourceid><sourceid>DOA</sourceid><recordid>eNp9kc9uEzEQxlcIJELhxgNY4kro-M_u2tzSpg2RIoFQEUfLa88Gh911sL0K4cQD9MAz8iRsG1Rx4jSjmd9830hfUbyk8IYCU-cMGF9tKHBV1o-KGVVCzCVA_biYAaipZ3X1tHiW0g4AOHA6K25vviBZmsPw--ev5Zi-kkU69j3meCShJXlaroeM0djsw0AuMB8QB7L0-9CZ6H_4YUuuu_E7uRgH12EiZnD3V4u-8Thk8qEzqTdvybrfd96aO5VE2hAffLwln9FtscOcnhdPWtMlfPG3nhWfrq9uLt_NN-9X68vFZm55Vas5LxllbWOZtACsrCXHhpaNk6hAlQ1Y66xl3HLhjDWsBlG1ICXFViCTyvGzYn3SdcHs9D763sSjDsbr-0GIW21i9rZDDY1qXcMqyRwXCGCkLB2VIFFADSVMWq9OWvsYvo2Yst6FMQ7T-5rJkglZCaUm6vWJsjGkFLF9cKWg77LT_2Y34eyEH3yHx_-yevVxU1UgFP8DEaGbsw</recordid><startdate>20230816</startdate><enddate>20230816</enddate><creator>Liu, Jiang</creator><general>John Wiley &amp; 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Each wedgelet contains an asymmetric pair of field‐aligned currents (FACs) so the net FAC of many wedgelets can equal an SCW's FAC content. It is unclear, however, why a wedgelet's FAC is asymmetric. To explore the reason, we investigate how earthward‐traveling DFBs interact with ambient plasma because this interaction leads to their FACs. The interaction is manifested as the pressure and magnetic field distributions around DFBs, which we examine statistically using THEMIS data. The statistical distributions are consistent with an interplay between the DFB‐caused mesoscale perturbations and the global magnetotail configuration and favor the rise of wedgelets' asymmetric FACs. This result reveals the importance of cross‐scale coupling in SCW formation. Plain Language Summary The electric current system of one of the most important energy release events in Earth's near‐space provides valuable information on how such events proceed. Previous studies showed that the current system consists of small elements with unexpected but necessary asymmetries. To understand how such asymmetries are formed, we examine the space plasma environment related to them using spacecraft data. The plasma environment suggests that the asymmetries arise from an interaction between small and global‐scale phenomena, indicating the importance of cross‐scale coupling in understanding the geospace. Key Points We examine the statistical distribution of pressure and magnetic field strength around dipolarizing flux bundles (DFBs) using THEMIS data Around a DFB in the dusk (dawn) sector of the magnetotail, the quantities are larger on its morning (evening) side This asymmetric distribution suggests an interplay between meso and global scales and favors asymmetric wedgelets as previously found</abstract><cop>Washington</cop><pub>John Wiley &amp; Sons, Inc</pub><doi>10.1029/2023GL103957</doi><tpages>10</tpages><orcidid>https://orcid.org/0000-0002-7489-9384</orcidid><oa>free_for_read</oa></addata></record>
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subjects Asymmetry
Coupling
current generation
dawn‐dusk asymmetry
dipolarizaing flux bundle
dipolarization front
Earth
Electric currents
Fluctuations
Magnetic field
Magnetic fields
Magnetotails
Mesoscale phenomena
Perturbation
Plasma
Space plasmas
Spacecraft
Statistical distributions
substorm current wedge
Tubes
wedgelet
title The Dawn‐Dusk Asymmetry of the Interaction Between Dipolarizing Flux Bundles and the Ambient Plasma: Implications for Asymmetric Wedgelets
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