Low-latitude 10eV electrons: Nighttime plasma line as a new research capability
The incoherent scatter radar (ISR) plasma line (PL) in daylight is excited by photoelectrons. Measurement of its intensity ( Kappa T sub(p) ) has long been used for their study. At night, despite the absence of any other excitation mechanism, the PL intensity should have a thermal amplitude level Ka...
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Veröffentlicht in: | Geophysical research letters 2015-09, Vol.42 (18), p.7255-7263 |
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description | The incoherent scatter radar (ISR) plasma line (PL) in daylight is excited by photoelectrons. Measurement of its intensity ( Kappa T sub(p) ) has long been used for their study. At night, despite the absence of any other excitation mechanism, the PL intensity should have a thermal amplitude level Kappa T sub(e), determined by the electron gas temperature T sub(e). To the contrary Carlson et al. (1982) found nighttime PLs over Arecibo enhanced >3 times above thermal intensities despite the absence of any known causative mechanism. Here we present discovery that nighttime PLs frequently recur, with quite variable enhancement. In the absence of direct solar EUV, these enhanced PLs must be produced by particle precipitation, manifested by the presence of variable recurring F region ~10eV electron fluxes. We see this as offering a new tool for space environment studies, opening a new era of particle precipitation research and ISR calibration. Key Points * 10eV electron flux often weakly present at low latitude in total darkness * Nighttime plasma-line detection opens a new area of particle precipitation study * Nighttime plasma lines a new diagnostic for space/geophysical environment |
doi_str_mv | 10.1002/2015GL065172 |
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Measurement of its intensity ( Kappa T sub(p) ) has long been used for their study. At night, despite the absence of any other excitation mechanism, the PL intensity should have a thermal amplitude level Kappa T sub(e), determined by the electron gas temperature T sub(e). To the contrary Carlson et al. (1982) found nighttime PLs over Arecibo enhanced >3 times above thermal intensities despite the absence of any known causative mechanism. Here we present discovery that nighttime PLs frequently recur, with quite variable enhancement. In the absence of direct solar EUV, these enhanced PLs must be produced by particle precipitation, manifested by the presence of variable recurring F region ~10eV electron fluxes. We see this as offering a new tool for space environment studies, opening a new era of particle precipitation research and ISR calibration. Key Points * 10eV electron flux often weakly present at low latitude in total darkness * Nighttime plasma-line detection opens a new area of particle precipitation study * Nighttime plasma lines a new diagnostic for space/geophysical environment</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1002/2015GL065172</identifier><language>eng</language><publisher>Washington: John Wiley & Sons, Inc</publisher><subject>Aerospace environments ; Amplitude ; Atmospheric precipitations ; Calibration ; Daylight ; Electron density ; Electron flux ; Electron gas ; Excitation ; F region ; Gas temperature ; Geophysics ; Incoherent scatter radar ; Latitude ; Measurement ; Night ; Night-time ; Nighttime ; Particle precipitation ; Photoelectrons ; Plasma ; Radar ; Solar EUV ; Temperature ; Temperature effects</subject><ispartof>Geophysical research letters, 2015-09, Vol.42 (18), p.7255-7263</ispartof><rights>2015. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Carlson, Herbert C</creatorcontrib><creatorcontrib>Djuth, Frank T</creatorcontrib><creatorcontrib>Perillat, Phil</creatorcontrib><creatorcontrib>Sulzer, Mike</creatorcontrib><title>Low-latitude 10eV electrons: Nighttime plasma line as a new research capability</title><title>Geophysical research letters</title><description>The incoherent scatter radar (ISR) plasma line (PL) in daylight is excited by photoelectrons. Measurement of its intensity ( Kappa T sub(p) ) has long been used for their study. At night, despite the absence of any other excitation mechanism, the PL intensity should have a thermal amplitude level Kappa T sub(e), determined by the electron gas temperature T sub(e). To the contrary Carlson et al. (1982) found nighttime PLs over Arecibo enhanced >3 times above thermal intensities despite the absence of any known causative mechanism. Here we present discovery that nighttime PLs frequently recur, with quite variable enhancement. In the absence of direct solar EUV, these enhanced PLs must be produced by particle precipitation, manifested by the presence of variable recurring F region ~10eV electron fluxes. We see this as offering a new tool for space environment studies, opening a new era of particle precipitation research and ISR calibration. Key Points * 10eV electron flux often weakly present at low latitude in total darkness * Nighttime plasma-line detection opens a new area of particle precipitation study * Nighttime plasma lines a new diagnostic for space/geophysical environment</description><subject>Aerospace environments</subject><subject>Amplitude</subject><subject>Atmospheric precipitations</subject><subject>Calibration</subject><subject>Daylight</subject><subject>Electron density</subject><subject>Electron flux</subject><subject>Electron gas</subject><subject>Excitation</subject><subject>F region</subject><subject>Gas temperature</subject><subject>Geophysics</subject><subject>Incoherent scatter radar</subject><subject>Latitude</subject><subject>Measurement</subject><subject>Night</subject><subject>Night-time</subject><subject>Nighttime</subject><subject>Particle precipitation</subject><subject>Photoelectrons</subject><subject>Plasma</subject><subject>Radar</subject><subject>Solar EUV</subject><subject>Temperature</subject><subject>Temperature effects</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2015</creationdate><recordtype>article</recordtype><recordid>eNqFz7FOwzAQBmALgUQpbDyAJRaWwJ2d2DEbqqAgRXQB1ursODSVm4TYFeLtiQQTA0z3D5_u_mPsHOEKAcS1ACyWFagCtThgMzR5npUA-pDNAMyUhVbH7CTGLQBIkDhjq6r_yAKlNu1rzxH8K_fBuzT2XbzhT-3bJqV25_kQKO6Ih7bznCIn3vkPPvroaXQb7mgg24Y2fZ6yo4ZC9Gc_c85e7u-eFw9ZtVo-Lm6rbBCgU6aEbUhjI3JNta1lI5wn4xRYVdSqpFqTayQW1lr00ogcyJJ2BkooFRoh5-zye-8w9u97H9N610bnQ6DO9_u4xglKZYoc_6daCQSNUEz04hfd9vuxmx5Zo0EotZyu_6m0EArLYmr4BZ_0dwY</recordid><startdate>20150901</startdate><enddate>20150901</enddate><creator>Carlson, Herbert C</creator><creator>Djuth, Frank T</creator><creator>Perillat, Phil</creator><creator>Sulzer, Mike</creator><general>John Wiley & Sons, Inc</general><scope>7TG</scope><scope>7TN</scope><scope>8FD</scope><scope>F1W</scope><scope>FR3</scope><scope>H8D</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope><scope>7UA</scope><scope>C1K</scope></search><sort><creationdate>20150901</creationdate><title>Low-latitude 10eV electrons: Nighttime plasma line as a new research capability</title><author>Carlson, Herbert C ; Djuth, Frank T ; Perillat, Phil ; Sulzer, Mike</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-p207t-62bfa71f247adbd3f2cea9c60b65d68ad7acf315bbb1e39240aba7c9080861923</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2015</creationdate><topic>Aerospace environments</topic><topic>Amplitude</topic><topic>Atmospheric precipitations</topic><topic>Calibration</topic><topic>Daylight</topic><topic>Electron density</topic><topic>Electron flux</topic><topic>Electron gas</topic><topic>Excitation</topic><topic>F region</topic><topic>Gas temperature</topic><topic>Geophysics</topic><topic>Incoherent scatter radar</topic><topic>Latitude</topic><topic>Measurement</topic><topic>Night</topic><topic>Night-time</topic><topic>Nighttime</topic><topic>Particle precipitation</topic><topic>Photoelectrons</topic><topic>Plasma</topic><topic>Radar</topic><topic>Solar EUV</topic><topic>Temperature</topic><topic>Temperature effects</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Carlson, Herbert C</creatorcontrib><creatorcontrib>Djuth, Frank T</creatorcontrib><creatorcontrib>Perillat, Phil</creatorcontrib><creatorcontrib>Sulzer, Mike</creatorcontrib><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Technology Research Database</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Carlson, Herbert C</au><au>Djuth, Frank T</au><au>Perillat, Phil</au><au>Sulzer, Mike</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Low-latitude 10eV electrons: Nighttime plasma line as a new research capability</atitle><jtitle>Geophysical research letters</jtitle><date>2015-09-01</date><risdate>2015</risdate><volume>42</volume><issue>18</issue><spage>7255</spage><epage>7263</epage><pages>7255-7263</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><abstract>The incoherent scatter radar (ISR) plasma line (PL) in daylight is excited by photoelectrons. Measurement of its intensity ( Kappa T sub(p) ) has long been used for their study. At night, despite the absence of any other excitation mechanism, the PL intensity should have a thermal amplitude level Kappa T sub(e), determined by the electron gas temperature T sub(e). To the contrary Carlson et al. (1982) found nighttime PLs over Arecibo enhanced >3 times above thermal intensities despite the absence of any known causative mechanism. Here we present discovery that nighttime PLs frequently recur, with quite variable enhancement. In the absence of direct solar EUV, these enhanced PLs must be produced by particle precipitation, manifested by the presence of variable recurring F region ~10eV electron fluxes. We see this as offering a new tool for space environment studies, opening a new era of particle precipitation research and ISR calibration. Key Points * 10eV electron flux often weakly present at low latitude in total darkness * Nighttime plasma-line detection opens a new area of particle precipitation study * Nighttime plasma lines a new diagnostic for space/geophysical environment</abstract><cop>Washington</cop><pub>John Wiley & Sons, Inc</pub><doi>10.1002/2015GL065172</doi><tpages>9</tpages></addata></record> |
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subjects | Aerospace environments Amplitude Atmospheric precipitations Calibration Daylight Electron density Electron flux Electron gas Excitation F region Gas temperature Geophysics Incoherent scatter radar Latitude Measurement Night Night-time Nighttime Particle precipitation Photoelectrons Plasma Radar Solar EUV Temperature Temperature effects |
title | Low-latitude 10eV electrons: Nighttime plasma line as a new research capability |
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