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Height-dependent ionospheric variations in the vicinity of nightside poleward expanding aurora after substorm onset
High‐latitude ionospheric variations at times near auroral substorms exhibit large temporal variations in both vertical and horizontal extents. Statistical analysis was made of data from the European Incoherent Scatter UHF radar at Tromsø, Norway, and International Monitor for Auroral Geomagnetic Ef...
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Published in: | Journal of geophysical research. Space physics 2014-05, Vol.119 (5), p.4146-4156 |
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container_title | Journal of geophysical research. Space physics |
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creator | Oyama, S. Miyoshi, Y. Shiokawa, K. Kurihara, J. Tsuda, T. T. Watkins, B. J. |
description | High‐latitude ionospheric variations at times near auroral substorms exhibit large temporal variations in both vertical and horizontal extents. Statistical analysis was made of data from the European Incoherent Scatter UHF radar at Tromsø, Norway, and International Monitor for Auroral Geomagnetic Effects magnetometer for finding common features in electron density, ion and electron temperatures and relating these to currents and associated heating. This paper particularly focused on the height dependencies. Results show clear evidences of large electric field with corresponding frictional heating and Pedersen currents located just outside the front of the poleward expanding aurora, which typically appeared at the eastside of westward traveling surge. At the beginning of the substorm recovery phase, the ionospheric density had a large peak in the E region and a smaller peak in the F region. This structure was named as C form in this paper based on its shape in the altitude‐time plot. The lower altitude density maximum is associated with hard auroral electron precipitation probably during pulsating aurora. We attribute the upper F region density maximum to local ionization by lower energy particle precipitation and/or long‐lived plasma that is convected horizontally into the overhead measurement volume from the dayside hemisphere.
Key Points
Ionosphere near poleward moving aurora is studied using EISCAT data
Joule energy is dissipated just outside the poleward expanding aurora
Ionospheric density at early recovery phase has a double peak in height |
doi_str_mv | 10.1002/2013JA019704 |
format | article |
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Key Points
Ionosphere near poleward moving aurora is studied using EISCAT data
Joule energy is dissipated just outside the poleward expanding aurora
Ionospheric density at early recovery phase has a double peak in height</description><identifier>ISSN: 2169-9380</identifier><identifier>EISSN: 2169-9402</identifier><identifier>DOI: 10.1002/2013JA019704</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Altitude ; aurora ; Auroras ; Density ; Electric fields ; F region ; Geophysics ; Heating ; Ionization ; Ionosphere ; Ionospherics ; Recovery ; Statistical analysis ; substorm ; UHF</subject><ispartof>Journal of geophysical research. Space physics, 2014-05, Vol.119 (5), p.4146-4156</ispartof><rights>2014. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c5152-5300ece2b13f238775afab35eb2253098bc0eb9e59db42bcd13c7fc8dbb760553</citedby><cites>FETCH-LOGICAL-c5152-5300ece2b13f238775afab35eb2253098bc0eb9e59db42bcd13c7fc8dbb760553</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Oyama, S.</creatorcontrib><creatorcontrib>Miyoshi, Y.</creatorcontrib><creatorcontrib>Shiokawa, K.</creatorcontrib><creatorcontrib>Kurihara, J.</creatorcontrib><creatorcontrib>Tsuda, T. T.</creatorcontrib><creatorcontrib>Watkins, B. J.</creatorcontrib><title>Height-dependent ionospheric variations in the vicinity of nightside poleward expanding aurora after substorm onset</title><title>Journal of geophysical research. Space physics</title><addtitle>J. Geophys. Res. Space Physics</addtitle><description>High‐latitude ionospheric variations at times near auroral substorms exhibit large temporal variations in both vertical and horizontal extents. Statistical analysis was made of data from the European Incoherent Scatter UHF radar at Tromsø, Norway, and International Monitor for Auroral Geomagnetic Effects magnetometer for finding common features in electron density, ion and electron temperatures and relating these to currents and associated heating. This paper particularly focused on the height dependencies. Results show clear evidences of large electric field with corresponding frictional heating and Pedersen currents located just outside the front of the poleward expanding aurora, which typically appeared at the eastside of westward traveling surge. At the beginning of the substorm recovery phase, the ionospheric density had a large peak in the E region and a smaller peak in the F region. This structure was named as C form in this paper based on its shape in the altitude‐time plot. The lower altitude density maximum is associated with hard auroral electron precipitation probably during pulsating aurora. We attribute the upper F region density maximum to local ionization by lower energy particle precipitation and/or long‐lived plasma that is convected horizontally into the overhead measurement volume from the dayside hemisphere.
Key Points
Ionosphere near poleward moving aurora is studied using EISCAT data
Joule energy is dissipated just outside the poleward expanding aurora
Ionospheric density at early recovery phase has a double peak in height</description><subject>Altitude</subject><subject>aurora</subject><subject>Auroras</subject><subject>Density</subject><subject>Electric fields</subject><subject>F region</subject><subject>Geophysics</subject><subject>Heating</subject><subject>Ionization</subject><subject>Ionosphere</subject><subject>Ionospherics</subject><subject>Recovery</subject><subject>Statistical analysis</subject><subject>substorm</subject><subject>UHF</subject><issn>2169-9380</issn><issn>2169-9402</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><recordid>eNqFkU9PGzEQxVeoSEWUGx_AEpceuq3_xOvdY4hKUoRAikBws2zvLDHd2FvbC-Tb11GgqjjAXDx6_r2nsacojgn-TjCmPygm7HyKSSPwZK84oKRqymaC6afXntX4c3EU4wPOVWeJ8IMiLsDer1LZwgCuBZeQ9c7HYQXBGvSoglUpKxFZh9IK0KM11tm0Qb5DbuuMtgU0-B6eVGgRPA_KtdbdIzUGHxRSXYKA4qhj8mGNchKkL8V-p_oIRy_nYXFz9vN6tigvrua_ZtOL0nDCackZxmCAasI6ymohuOqUZhw0pfmuqbXBoBvgTasnVJuWMCM6U7daiwpzzg6Lr7vcIfg_I8Qk1zYa6HvlwI9RkkqQClMq6o9RzptKiPzPGT15gz74Mbj8kBzIaoYrSlmmvu0oE3yMATo5BLtWYSMJltt9yf_3lXG2w59sD5t3WXk-X045wZPtKOXOZWOC538uFX7LSjDB5e3lXC5PF9czdncql-wvhe-mnA</recordid><startdate>201405</startdate><enddate>201405</enddate><creator>Oyama, S.</creator><creator>Miyoshi, Y.</creator><creator>Shiokawa, K.</creator><creator>Kurihara, J.</creator><creator>Tsuda, T. T.</creator><creator>Watkins, B. J.</creator><general>Blackwell Publishing Ltd</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>8FD</scope><scope>H8D</scope><scope>KL.</scope><scope>L7M</scope></search><sort><creationdate>201405</creationdate><title>Height-dependent ionospheric variations in the vicinity of nightside poleward expanding aurora after substorm onset</title><author>Oyama, S. ; Miyoshi, Y. ; Shiokawa, K. ; Kurihara, J. ; Tsuda, T. T. ; Watkins, B. J.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c5152-5300ece2b13f238775afab35eb2253098bc0eb9e59db42bcd13c7fc8dbb760553</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Altitude</topic><topic>aurora</topic><topic>Auroras</topic><topic>Density</topic><topic>Electric fields</topic><topic>F region</topic><topic>Geophysics</topic><topic>Heating</topic><topic>Ionization</topic><topic>Ionosphere</topic><topic>Ionospherics</topic><topic>Recovery</topic><topic>Statistical analysis</topic><topic>substorm</topic><topic>UHF</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Oyama, S.</creatorcontrib><creatorcontrib>Miyoshi, Y.</creatorcontrib><creatorcontrib>Shiokawa, K.</creatorcontrib><creatorcontrib>Kurihara, J.</creatorcontrib><creatorcontrib>Tsuda, T. T.</creatorcontrib><creatorcontrib>Watkins, B. J.</creatorcontrib><collection>Istex</collection><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>Oyama, S.</au><au>Miyoshi, Y.</au><au>Shiokawa, K.</au><au>Kurihara, J.</au><au>Tsuda, T. T.</au><au>Watkins, B. J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Height-dependent ionospheric variations in the vicinity of nightside poleward expanding aurora after substorm onset</atitle><jtitle>Journal of geophysical research. Space physics</jtitle><addtitle>J. Geophys. Res. Space Physics</addtitle><date>2014-05</date><risdate>2014</risdate><volume>119</volume><issue>5</issue><spage>4146</spage><epage>4156</epage><pages>4146-4156</pages><issn>2169-9380</issn><eissn>2169-9402</eissn><abstract>High‐latitude ionospheric variations at times near auroral substorms exhibit large temporal variations in both vertical and horizontal extents. Statistical analysis was made of data from the European Incoherent Scatter UHF radar at Tromsø, Norway, and International Monitor for Auroral Geomagnetic Effects magnetometer for finding common features in electron density, ion and electron temperatures and relating these to currents and associated heating. This paper particularly focused on the height dependencies. Results show clear evidences of large electric field with corresponding frictional heating and Pedersen currents located just outside the front of the poleward expanding aurora, which typically appeared at the eastside of westward traveling surge. At the beginning of the substorm recovery phase, the ionospheric density had a large peak in the E region and a smaller peak in the F region. This structure was named as C form in this paper based on its shape in the altitude‐time plot. The lower altitude density maximum is associated with hard auroral electron precipitation probably during pulsating aurora. We attribute the upper F region density maximum to local ionization by lower energy particle precipitation and/or long‐lived plasma that is convected horizontally into the overhead measurement volume from the dayside hemisphere.
Key Points
Ionosphere near poleward moving aurora is studied using EISCAT data
Joule energy is dissipated just outside the poleward expanding aurora
Ionospheric density at early recovery phase has a double peak in height</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1002/2013JA019704</doi><tpages>11</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Altitude aurora Auroras Density Electric fields F region Geophysics Heating Ionization Ionosphere Ionospherics Recovery Statistical analysis substorm UHF |
title | Height-dependent ionospheric variations in the vicinity of nightside poleward expanding aurora after substorm onset |
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