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An empirical profile of VLF triggered emissions
The Siple Transmitter Experiment operated from 1973 to 1988 and generated a wealth of observations of nonlinear wave‐particle interactions including extensive recordings of triggered emissions generated by VLF signals injected into the magnetosphere from the transmitter at Siple Station, Antarctica....
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Published in: | Journal of geophysical research. Space physics 2015-08, Vol.120 (8), p.6581-6595 |
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description | The Siple Transmitter Experiment operated from 1973 to 1988 and generated a wealth of observations of nonlinear wave‐particle interactions including extensive recordings of triggered emissions generated by VLF signals injected into the magnetosphere from the transmitter at Siple Station, Antarctica. Due to their complex appearance and immensely varied behavior, triggered emissions remain poorly described and understood. This work provides a comprehensive statistical description of observed triggered emissions and establishes statistical bounds on triggered emission type (fallers, risers, and positive and negative hooks) and behavior (frequency changes between 1 kHz and 2.5 kHz with initial sweep rates between −2.5 kHz/s and 2.5 kHz/s, with risers undergoing a median frequency change of 556 Hz and fallers a median frequency change of −198 Hz). The statistical study also reveals an apparent dependence of the triggered emission behavior on the transmitted signal itself. Long tones and rising ramps generate more risers and positive hooks, while short tones and falling ramps produce more fallers and negative hooks. Triggered emissions also appear to favorably initiate with sweep rates similar to that of the triggering element, with the 1 kHz/s rising ramps triggering initial risers with a median sweep rate of 1.03 kHz/s and −1 kHz/s triggering initial fallers with a median sweep rate of −0.73 kHz/s. These results improve observations of wave modification resulting from wave‐particle interactions in the radiation belts and can be used to validate numerical simulations of triggered emissions.
Key Points
Risers undergo a larger net frequency change and can endure for a longer duration than fallers
Triggering behavior at initiation depends on the transmitted element but later becomes independent
The number of triggered emissions correlates with the total transmitted signal growth and with Kp |
doi_str_mv | 10.1002/2015JA021444 |
format | article |
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Key Points
Risers undergo a larger net frequency change and can endure for a longer duration than fallers
Triggering behavior at initiation depends on the transmitted element but later becomes independent
The number of triggered emissions correlates with the total transmitted signal growth and with Kp</description><identifier>ISSN: 2169-9380</identifier><identifier>EISSN: 2169-9402</identifier><identifier>DOI: 10.1002/2015JA021444</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Computer simulation ; Durability ; ELF/VLF ; Emission analysis ; Emissions ; Geophysics ; Hooks ; Magnetic fields ; Magnetosphere ; Magnetospheres ; Median (statistics) ; Numerical simulations ; Particle interactions ; Radiation ; Radiation belts ; Ramps ; Risers ; Simulation ; Siple Station ; Transmitters ; triggered emissions ; Very Low Frequencies ; VLF ; Wave-particle interactions</subject><ispartof>Journal of geophysical research. Space physics, 2015-08, Vol.120 (8), p.6581-6595</ispartof><rights>2015. American Geophysical Union. All Rights Reserved.</rights><rights>Copyright Blackwell Publishing Ltd. Aug 2015</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c5478-1360dd6750dc92b5d2507ee0f67ce4de2531a1fa1116a56d3f51e8adaf4dca6c3</citedby><cites>FETCH-LOGICAL-c5478-1360dd6750dc92b5d2507ee0f67ce4de2531a1fa1116a56d3f51e8adaf4dca6c3</cites></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>Li, J. D.</creatorcontrib><creatorcontrib>Spasojevic, M.</creatorcontrib><creatorcontrib>Inan, U. S.</creatorcontrib><title>An empirical profile of VLF triggered emissions</title><title>Journal of geophysical research. Space physics</title><addtitle>J. Geophys. Res. Space Physics</addtitle><description>The Siple Transmitter Experiment operated from 1973 to 1988 and generated a wealth of observations of nonlinear wave‐particle interactions including extensive recordings of triggered emissions generated by VLF signals injected into the magnetosphere from the transmitter at Siple Station, Antarctica. Due to their complex appearance and immensely varied behavior, triggered emissions remain poorly described and understood. This work provides a comprehensive statistical description of observed triggered emissions and establishes statistical bounds on triggered emission type (fallers, risers, and positive and negative hooks) and behavior (frequency changes between 1 kHz and 2.5 kHz with initial sweep rates between −2.5 kHz/s and 2.5 kHz/s, with risers undergoing a median frequency change of 556 Hz and fallers a median frequency change of −198 Hz). The statistical study also reveals an apparent dependence of the triggered emission behavior on the transmitted signal itself. Long tones and rising ramps generate more risers and positive hooks, while short tones and falling ramps produce more fallers and negative hooks. Triggered emissions also appear to favorably initiate with sweep rates similar to that of the triggering element, with the 1 kHz/s rising ramps triggering initial risers with a median sweep rate of 1.03 kHz/s and −1 kHz/s triggering initial fallers with a median sweep rate of −0.73 kHz/s. These results improve observations of wave modification resulting from wave‐particle interactions in the radiation belts and can be used to validate numerical simulations of triggered emissions.
Key Points
Risers undergo a larger net frequency change and can endure for a longer duration than fallers
Triggering behavior at initiation depends on the transmitted element but later becomes independent
The number of triggered emissions correlates with the total transmitted signal growth and with Kp</description><subject>Computer simulation</subject><subject>Durability</subject><subject>ELF/VLF</subject><subject>Emission analysis</subject><subject>Emissions</subject><subject>Geophysics</subject><subject>Hooks</subject><subject>Magnetic fields</subject><subject>Magnetosphere</subject><subject>Magnetospheres</subject><subject>Median (statistics)</subject><subject>Numerical simulations</subject><subject>Particle interactions</subject><subject>Radiation</subject><subject>Radiation belts</subject><subject>Ramps</subject><subject>Risers</subject><subject>Simulation</subject><subject>Siple Station</subject><subject>Transmitters</subject><subject>triggered emissions</subject><subject>Very Low Frequencies</subject><subject>VLF</subject><subject>Wave-particle interactions</subject><issn>2169-9380</issn><issn>2169-9402</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2015</creationdate><recordtype>article</recordtype><recordid>eNqNkU9LAzEQxRdRsNTe_AALXjy4NpO_u8elaGsptYjWY4ibpGzd7takRfvtTVkV8VCcS4bh94b3MlF0DugaEMJ9jICNc4SBUnoUdTDwLMkowsffPUnRadTzfolCpWEErBP18zo2q3XpykJV8do1tqxM3Nh4PrmNN65cLIwzOiCl92VT-7PoxKrKm97X242ebm8eB6Nkcj-8G-STpGBUpAkQjrTmgiFdZPiFacyQMAZZLgpDtcGMgAKrAIArxjWxDEyqtLJUF4oXpBtdtnuDpbet8RsZHBSmqlRtmq2XIBhhDIfg_0AxhhQQ7NGLP-iy2bo6BJE4bKIpCn4OUSBAEIwZZIG6aqnCNd47Y-XalSvldhKQ3F9E_r5IwEmLv4cP3h1k5Xj4kIdsOA2qpFWVfmM-flTKvUouiGDyeTqU8wGF2TSdyRH5BA9Jlxc</recordid><startdate>201508</startdate><enddate>201508</enddate><creator>Li, J. D.</creator><creator>Spasojevic, M.</creator><creator>Inan, U. S.</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>201508</creationdate><title>An empirical profile of VLF triggered emissions</title><author>Li, J. D. ; Spasojevic, M. ; Inan, U. S.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c5478-1360dd6750dc92b5d2507ee0f67ce4de2531a1fa1116a56d3f51e8adaf4dca6c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2015</creationdate><topic>Computer simulation</topic><topic>Durability</topic><topic>ELF/VLF</topic><topic>Emission analysis</topic><topic>Emissions</topic><topic>Geophysics</topic><topic>Hooks</topic><topic>Magnetic fields</topic><topic>Magnetosphere</topic><topic>Magnetospheres</topic><topic>Median (statistics)</topic><topic>Numerical simulations</topic><topic>Particle interactions</topic><topic>Radiation</topic><topic>Radiation belts</topic><topic>Ramps</topic><topic>Risers</topic><topic>Simulation</topic><topic>Siple Station</topic><topic>Transmitters</topic><topic>triggered emissions</topic><topic>Very Low Frequencies</topic><topic>VLF</topic><topic>Wave-particle interactions</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Li, J. D.</creatorcontrib><creatorcontrib>Spasojevic, M.</creatorcontrib><creatorcontrib>Inan, U. S.</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>Li, J. D.</au><au>Spasojevic, M.</au><au>Inan, U. S.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>An empirical profile of VLF triggered emissions</atitle><jtitle>Journal of geophysical research. Space physics</jtitle><addtitle>J. Geophys. Res. Space Physics</addtitle><date>2015-08</date><risdate>2015</risdate><volume>120</volume><issue>8</issue><spage>6581</spage><epage>6595</epage><pages>6581-6595</pages><issn>2169-9380</issn><eissn>2169-9402</eissn><abstract>The Siple Transmitter Experiment operated from 1973 to 1988 and generated a wealth of observations of nonlinear wave‐particle interactions including extensive recordings of triggered emissions generated by VLF signals injected into the magnetosphere from the transmitter at Siple Station, Antarctica. Due to their complex appearance and immensely varied behavior, triggered emissions remain poorly described and understood. This work provides a comprehensive statistical description of observed triggered emissions and establishes statistical bounds on triggered emission type (fallers, risers, and positive and negative hooks) and behavior (frequency changes between 1 kHz and 2.5 kHz with initial sweep rates between −2.5 kHz/s and 2.5 kHz/s, with risers undergoing a median frequency change of 556 Hz and fallers a median frequency change of −198 Hz). The statistical study also reveals an apparent dependence of the triggered emission behavior on the transmitted signal itself. Long tones and rising ramps generate more risers and positive hooks, while short tones and falling ramps produce more fallers and negative hooks. Triggered emissions also appear to favorably initiate with sweep rates similar to that of the triggering element, with the 1 kHz/s rising ramps triggering initial risers with a median sweep rate of 1.03 kHz/s and −1 kHz/s triggering initial fallers with a median sweep rate of −0.73 kHz/s. These results improve observations of wave modification resulting from wave‐particle interactions in the radiation belts and can be used to validate numerical simulations of triggered emissions.
Key Points
Risers undergo a larger net frequency change and can endure for a longer duration than fallers
Triggering behavior at initiation depends on the transmitted element but later becomes independent
The number of triggered emissions correlates with the total transmitted signal growth and with Kp</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1002/2015JA021444</doi><tpages>15</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Computer simulation Durability ELF/VLF Emission analysis Emissions Geophysics Hooks Magnetic fields Magnetosphere Magnetospheres Median (statistics) Numerical simulations Particle interactions Radiation Radiation belts Ramps Risers Simulation Siple Station Transmitters triggered emissions Very Low Frequencies VLF Wave-particle interactions |
title | An empirical profile of VLF triggered emissions |
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