Compressional perturbations of the dayside magnetosphere during high‐speed‐stream‐driven geomagnetic storms
The quasi‐DC compressions of the Earth's dayside magnetic field by ram‐pressure fluctuations in the solar wind are characterized by using multiple GOES spacecraft in geosynchronous orbit, multiple Los Alamos spacecraft in geosynchronous orbit, global MHD simulations, and ACE and Wind solar wind...
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Veröffentlicht in: | Journal of geophysical research. Space physics 2016-05, Vol.121 (5), p.4569-4589 |
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description | The quasi‐DC compressions of the Earth's dayside magnetic field by ram‐pressure fluctuations in the solar wind are characterized by using multiple GOES spacecraft in geosynchronous orbit, multiple Los Alamos spacecraft in geosynchronous orbit, global MHD simulations, and ACE and Wind solar wind measurements. Owing to the inward‐outward advection of plasma as the dayside magnetic field is compressed, magnetic field compressions experienced by the plasma in the dayside magnetosphere are greater than the magnetic field compressions measured by a spacecraft. Theoretical calculations indicate that the plasma compression can be a factor of 2 higher than the observed magnetic field compression. The solar wind ram‐pressure changes causing the quasi‐DC magnetospheric compressions are mostly owed to rapid changes in the solar wind number density associated with the crossing of plasma boundaries; an Earth crossing of a plasma boundary produces a sudden change in the dayside magnetic field strength accompanied by a sudden inward or outward motion of the plasma in the dayside magnetosphere. Superposed epoch analysis of high‐speed‐stream‐driven storms was used to explore solar wind compressions and storm time geosynchronous magnetic field compressions, which are of particular interest for the possible contribution to the energization of the outer electron radiation belt. The occurrence distributions of dayside magnetic field compressions, solar wind ram‐pressure changes, and dayside radial plasma flow velocities were investigated: all three quantities approximately obey power law statistics for large values. The approximate power law indices for the distributions of magnetic compressions and ram‐pressure changes were both −3.
Key Points
Quasi‐DC compressions of the dayside magnetosphere are responses to solar wind ram‐pressure changes
The plasma compression in the dayside is greater than the field compression measured by a satellite
Field compressions, ram‐pressure changes, and flow velocities obey large‐value power law statistics |
doi_str_mv | 10.1002/2015JA022136 |
format | Article |
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Key Points
Quasi‐DC compressions of the dayside magnetosphere are responses to solar wind ram‐pressure changes
The plasma compression in the dayside is greater than the field compression measured by a satellite
Field compressions, ram‐pressure changes, and flow velocities obey large‐value power law statistics</description><identifier>ISSN: 2169-9380</identifier><identifier>EISSN: 2169-9402</identifier><identifier>DOI: 10.1002/2015JA022136</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Activation ; Advection ; Compressing ; compression ; Compression tests ; dayside magnetosphere ; Electron radiation ; Field strength ; Flow velocity ; Geomagnetic storms ; Geomagnetism ; Geosynchronous orbits ; image dipole ; Magnetic fields ; magnetic pumping ; Magnetic storms ; Magnetohydrodynamics ; Magnetosphere ; Magnetospheres ; Plasma ; Plasma compression ; Power law ; Pressure changes ; Pressure fluctuations ; Radiation ; Solar magnetic field ; Solar wind ; solar wind structure ; Spacecraft ; Statistics ; Storms ; Time compression ; Velocity ; Wind measurement</subject><ispartof>Journal of geophysical research. Space physics, 2016-05, Vol.121 (5), p.4569-4589</ispartof><rights>2016. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4823-3bfc53411f013ece29182b9b637042c1c2e82bfc2ea81def4569c422063976593</citedby><cites>FETCH-LOGICAL-c4823-3bfc53411f013ece29182b9b637042c1c2e82bfc2ea81def4569c422063976593</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2F2015JA022136$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2F2015JA022136$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,1427,27903,27904,45553,45554,46387,46811</link.rule.ids></links><search><creatorcontrib>Borovsky, Joseph E.</creatorcontrib><creatorcontrib>Denton, Michael H.</creatorcontrib><title>Compressional perturbations of the dayside magnetosphere during high‐speed‐stream‐driven geomagnetic storms</title><title>Journal of geophysical research. Space physics</title><description>The quasi‐DC compressions of the Earth's dayside magnetic field by ram‐pressure fluctuations in the solar wind are characterized by using multiple GOES spacecraft in geosynchronous orbit, multiple Los Alamos spacecraft in geosynchronous orbit, global MHD simulations, and ACE and Wind solar wind measurements. Owing to the inward‐outward advection of plasma as the dayside magnetic field is compressed, magnetic field compressions experienced by the plasma in the dayside magnetosphere are greater than the magnetic field compressions measured by a spacecraft. Theoretical calculations indicate that the plasma compression can be a factor of 2 higher than the observed magnetic field compression. The solar wind ram‐pressure changes causing the quasi‐DC magnetospheric compressions are mostly owed to rapid changes in the solar wind number density associated with the crossing of plasma boundaries; an Earth crossing of a plasma boundary produces a sudden change in the dayside magnetic field strength accompanied by a sudden inward or outward motion of the plasma in the dayside magnetosphere. Superposed epoch analysis of high‐speed‐stream‐driven storms was used to explore solar wind compressions and storm time geosynchronous magnetic field compressions, which are of particular interest for the possible contribution to the energization of the outer electron radiation belt. The occurrence distributions of dayside magnetic field compressions, solar wind ram‐pressure changes, and dayside radial plasma flow velocities were investigated: all three quantities approximately obey power law statistics for large values. The approximate power law indices for the distributions of magnetic compressions and ram‐pressure changes were both −3.
Key Points
Quasi‐DC compressions of the dayside magnetosphere are responses to solar wind ram‐pressure changes
The plasma compression in the dayside is greater than the field compression measured by a satellite
Field compressions, ram‐pressure changes, and flow velocities obey large‐value power law statistics</description><subject>Activation</subject><subject>Advection</subject><subject>Compressing</subject><subject>compression</subject><subject>Compression tests</subject><subject>dayside magnetosphere</subject><subject>Electron radiation</subject><subject>Field strength</subject><subject>Flow velocity</subject><subject>Geomagnetic storms</subject><subject>Geomagnetism</subject><subject>Geosynchronous orbits</subject><subject>image dipole</subject><subject>Magnetic fields</subject><subject>magnetic pumping</subject><subject>Magnetic storms</subject><subject>Magnetohydrodynamics</subject><subject>Magnetosphere</subject><subject>Magnetospheres</subject><subject>Plasma</subject><subject>Plasma compression</subject><subject>Power law</subject><subject>Pressure changes</subject><subject>Pressure fluctuations</subject><subject>Radiation</subject><subject>Solar magnetic field</subject><subject>Solar wind</subject><subject>solar wind structure</subject><subject>Spacecraft</subject><subject>Statistics</subject><subject>Storms</subject><subject>Time compression</subject><subject>Velocity</subject><subject>Wind measurement</subject><issn>2169-9380</issn><issn>2169-9402</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNqNkcFq20AQhkVpoSbJLQ8g6KWHONmdXa20R2PSJMYQCM1ZrFcje42klXekFt_yCHnGPknWuIHSg8lc_pnhm2F2_yS55OyaMwY3wHi2mDEALtSnZAJc6amWDD6_56JgX5MLoi2LUcQWzybJbu7bPiCR851p0h7DMIaVGWJJqa_TYYNpZfbkKkxbs-5w8NRvMMTuGFy3Tjduvfnz8ko9YnXQIaBpY1IF9wu7dI3-OOZsSoMPLZ0nX2rTEF781bPk-cftz_n9dPl49zCfLadWFiCmYlXbTEjOa8YFWgTNC1jplRI5k2C5BYx1HcUUvMJaZkpbCcCU0LnKtDhLvh_39sHvRqShbB1ZbBrToR-pjOsyqTNQ6gMoK5SUQuYR_fYfuvVjiF9HJUQbtMwLXpyieK5zyEDnhwuvjpQNnihgXfbBtSbsS87Kg6flv55GXBzx367B_Um2XNw9zeLThBBvGKukrg</recordid><startdate>201605</startdate><enddate>201605</enddate><creator>Borovsky, Joseph E.</creator><creator>Denton, Michael H.</creator><general>Blackwell Publishing Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>8FD</scope><scope>H8D</scope><scope>KL.</scope><scope>L7M</scope></search><sort><creationdate>201605</creationdate><title>Compressional perturbations of the dayside magnetosphere during high‐speed‐stream‐driven geomagnetic storms</title><author>Borovsky, Joseph E. ; Denton, Michael H.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4823-3bfc53411f013ece29182b9b637042c1c2e82bfc2ea81def4569c422063976593</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Activation</topic><topic>Advection</topic><topic>Compressing</topic><topic>compression</topic><topic>Compression tests</topic><topic>dayside magnetosphere</topic><topic>Electron radiation</topic><topic>Field strength</topic><topic>Flow velocity</topic><topic>Geomagnetic storms</topic><topic>Geomagnetism</topic><topic>Geosynchronous orbits</topic><topic>image dipole</topic><topic>Magnetic fields</topic><topic>magnetic pumping</topic><topic>Magnetic storms</topic><topic>Magnetohydrodynamics</topic><topic>Magnetosphere</topic><topic>Magnetospheres</topic><topic>Plasma</topic><topic>Plasma compression</topic><topic>Power law</topic><topic>Pressure changes</topic><topic>Pressure fluctuations</topic><topic>Radiation</topic><topic>Solar magnetic field</topic><topic>Solar wind</topic><topic>solar wind structure</topic><topic>Spacecraft</topic><topic>Statistics</topic><topic>Storms</topic><topic>Time compression</topic><topic>Velocity</topic><topic>Wind measurement</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Borovsky, Joseph E.</creatorcontrib><creatorcontrib>Denton, Michael H.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Journal of geophysical research. Space physics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Borovsky, Joseph E.</au><au>Denton, Michael H.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Compressional perturbations of the dayside magnetosphere during high‐speed‐stream‐driven geomagnetic storms</atitle><jtitle>Journal of geophysical research. Space physics</jtitle><date>2016-05</date><risdate>2016</risdate><volume>121</volume><issue>5</issue><spage>4569</spage><epage>4589</epage><pages>4569-4589</pages><issn>2169-9380</issn><eissn>2169-9402</eissn><abstract>The quasi‐DC compressions of the Earth's dayside magnetic field by ram‐pressure fluctuations in the solar wind are characterized by using multiple GOES spacecraft in geosynchronous orbit, multiple Los Alamos spacecraft in geosynchronous orbit, global MHD simulations, and ACE and Wind solar wind measurements. Owing to the inward‐outward advection of plasma as the dayside magnetic field is compressed, magnetic field compressions experienced by the plasma in the dayside magnetosphere are greater than the magnetic field compressions measured by a spacecraft. Theoretical calculations indicate that the plasma compression can be a factor of 2 higher than the observed magnetic field compression. The solar wind ram‐pressure changes causing the quasi‐DC magnetospheric compressions are mostly owed to rapid changes in the solar wind number density associated with the crossing of plasma boundaries; an Earth crossing of a plasma boundary produces a sudden change in the dayside magnetic field strength accompanied by a sudden inward or outward motion of the plasma in the dayside magnetosphere. Superposed epoch analysis of high‐speed‐stream‐driven storms was used to explore solar wind compressions and storm time geosynchronous magnetic field compressions, which are of particular interest for the possible contribution to the energization of the outer electron radiation belt. The occurrence distributions of dayside magnetic field compressions, solar wind ram‐pressure changes, and dayside radial plasma flow velocities were investigated: all three quantities approximately obey power law statistics for large values. The approximate power law indices for the distributions of magnetic compressions and ram‐pressure changes were both −3.
Key Points
Quasi‐DC compressions of the dayside magnetosphere are responses to solar wind ram‐pressure changes
The plasma compression in the dayside is greater than the field compression measured by a satellite
Field compressions, ram‐pressure changes, and flow velocities obey large‐value power law statistics</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1002/2015JA022136</doi><tpages>21</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Activation Advection Compressing compression Compression tests dayside magnetosphere Electron radiation Field strength Flow velocity Geomagnetic storms Geomagnetism Geosynchronous orbits image dipole Magnetic fields magnetic pumping Magnetic storms Magnetohydrodynamics Magnetosphere Magnetospheres Plasma Plasma compression Power law Pressure changes Pressure fluctuations Radiation Solar magnetic field Solar wind solar wind structure Spacecraft Statistics Storms Time compression Velocity Wind measurement |
title | Compressional perturbations of the dayside magnetosphere during high‐speed‐stream‐driven geomagnetic storms |
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