VLF observations of ionospheric disturbances in association with TLEs from the EuroSprite-2007 campaign
Two Very Low Frequency (VLF) AWESOME remote sensing systems located at Algiers, Algeria (36.45°N, 3.28°E) and Sebha, Libya (27.02°N, 14.26°E) monitor VLF signal perturbations for evidence of ionospheric disturbances. During the EuroSprite‐2007 campaign a number of Transient Luminous Events (TLEs) we...
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creator | NaitAmor, S. AlAbdoadaim, M. A. Cohen, M. B. Cotts, B. R. T. Soula, S. Chanrion, O. Neubert, T. Abdelatif, T. |
description | Two Very Low Frequency (VLF) AWESOME remote sensing systems located at Algiers, Algeria (36.45°N, 3.28°E) and Sebha, Libya (27.02°N, 14.26°E) monitor VLF signal perturbations for evidence of ionospheric disturbances. During the EuroSprite‐2007 campaign a number of Transient Luminous Events (TLEs) were captured over the Mediterranean Sea by cameras at Pic du Midi (42.94°N, 0.14°E) and at Centre de Recherches Atmosphériques (CRA) in southwestern France (43.13°N, 0.37°E). The cameras observations are compared to collected VLF AWESOME data. We consider early VLF perturbations observed on 12–13, 17–18 October and 17–18 December, 2007. The data from the two VLF receivers confirm the association between TLEs and early VLF signal perturbations with the perturbations amplitudes dependent on the observation configuration i.e. whether the TLE is near the receiver, near the transmitter, or far from both and the scattering process. The results also reveal that the early VLF perturbations can occur in the absence of a TLE. |
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A. ; Cohen, M. B. ; Cotts, B. R. T. ; Soula, S. ; Chanrion, O. ; Neubert, T. ; Abdelatif, T.</creator><creatorcontrib>NaitAmor, S. ; AlAbdoadaim, M. A. ; Cohen, M. B. ; Cotts, B. R. T. ; Soula, S. ; Chanrion, O. ; Neubert, T. ; Abdelatif, T.</creatorcontrib><description>Two Very Low Frequency (VLF) AWESOME remote sensing systems located at Algiers, Algeria (36.45°N, 3.28°E) and Sebha, Libya (27.02°N, 14.26°E) monitor VLF signal perturbations for evidence of ionospheric disturbances. During the EuroSprite‐2007 campaign a number of Transient Luminous Events (TLEs) were captured over the Mediterranean Sea by cameras at Pic du Midi (42.94°N, 0.14°E) and at Centre de Recherches Atmosphériques (CRA) in southwestern France (43.13°N, 0.37°E). The cameras observations are compared to collected VLF AWESOME data. We consider early VLF perturbations observed on 12–13, 17–18 October and 17–18 December, 2007. The data from the two VLF receivers confirm the association between TLEs and early VLF signal perturbations with the perturbations amplitudes dependent on the observation configuration i.e. whether the TLE is near the receiver, near the transmitter, or far from both and the scattering process. The results also reveal that the early VLF perturbations can occur in the absence of a TLE.</description><identifier>ISSN: 0148-0227</identifier><identifier>ISSN: 2169-9380</identifier><identifier>EISSN: 2156-2202</identifier><identifier>EISSN: 2169-9402</identifier><identifier>DOI: 10.1029/2009JA015026</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Algeria ; Atmospheric and Oceanic Physics ; Atmospheric sciences ; Cameras ; Early ; Ionospheric disturbances ; Lightning ; Mediterranean Sea ; Monitors ; Perturbation ; Physics ; Receivers ; Remote sensing ; Remote sensing systems ; Transient luminous events ; Very Low Frequencies ; VLF ; VLF signals perturbations</subject><ispartof>Journal of Geophysical Research: Space Physics, 2010-07, Vol.115 (A7), p.n/a</ispartof><rights>Copyright 2010 by the American Geophysical Union.</rights><rights>Copyright 2010 by American Geophysical Union</rights><rights>Copyright</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4393-4947d5974ba98de4cce3749c659a21c1f151b584720ee2ea5d4d71fa2ac395373</citedby><cites>FETCH-LOGICAL-c4393-4947d5974ba98de4cce3749c659a21c1f151b584720ee2ea5d4d71fa2ac395373</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2009JA015026$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2009JA015026$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>230,314,780,784,885,1417,1433,11514,27924,27925,45574,45575,46409,46468,46833,46892</link.rule.ids><backlink>$$Uhttps://hal.science/hal-00518358$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>NaitAmor, S.</creatorcontrib><creatorcontrib>AlAbdoadaim, M. A.</creatorcontrib><creatorcontrib>Cohen, M. B.</creatorcontrib><creatorcontrib>Cotts, B. R. T.</creatorcontrib><creatorcontrib>Soula, S.</creatorcontrib><creatorcontrib>Chanrion, O.</creatorcontrib><creatorcontrib>Neubert, T.</creatorcontrib><creatorcontrib>Abdelatif, T.</creatorcontrib><title>VLF observations of ionospheric disturbances in association with TLEs from the EuroSprite-2007 campaign</title><title>Journal of Geophysical Research: Space Physics</title><addtitle>J. Geophys. Res</addtitle><description>Two Very Low Frequency (VLF) AWESOME remote sensing systems located at Algiers, Algeria (36.45°N, 3.28°E) and Sebha, Libya (27.02°N, 14.26°E) monitor VLF signal perturbations for evidence of ionospheric disturbances. During the EuroSprite‐2007 campaign a number of Transient Luminous Events (TLEs) were captured over the Mediterranean Sea by cameras at Pic du Midi (42.94°N, 0.14°E) and at Centre de Recherches Atmosphériques (CRA) in southwestern France (43.13°N, 0.37°E). The cameras observations are compared to collected VLF AWESOME data. We consider early VLF perturbations observed on 12–13, 17–18 October and 17–18 December, 2007. The data from the two VLF receivers confirm the association between TLEs and early VLF signal perturbations with the perturbations amplitudes dependent on the observation configuration i.e. whether the TLE is near the receiver, near the transmitter, or far from both and the scattering process. The results also reveal that the early VLF perturbations can occur in the absence of a TLE.</description><subject>Algeria</subject><subject>Atmospheric and Oceanic Physics</subject><subject>Atmospheric sciences</subject><subject>Cameras</subject><subject>Early</subject><subject>Ionospheric disturbances</subject><subject>Lightning</subject><subject>Mediterranean Sea</subject><subject>Monitors</subject><subject>Perturbation</subject><subject>Physics</subject><subject>Receivers</subject><subject>Remote sensing</subject><subject>Remote sensing systems</subject><subject>Transient luminous events</subject><subject>Very Low Frequencies</subject><subject>VLF</subject><subject>VLF signals perturbations</subject><issn>0148-0227</issn><issn>2169-9380</issn><issn>2156-2202</issn><issn>2169-9402</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp90V1rFDEUBuBBFFxq7_wBQS9UcPTke3K51u2uZVC09QNvQjab6aadnazJTGv_vRlHigg2NwfCc5L3cIriMYZXGIh6TQDUyRwwByLuFTOCuSgJAXK_mAFmVQmEyIfFYUoXkA_jggGeFedf6mMU1snFK9P70CUUGpRrSPuti96ijU_9ENemsy4h3yGTUrD-t0XXvt-is3qRUBPDDvVbhxZDDKf76HtX5kASWbPbG3_ePSoeNKZN7vBPPSg-Hy_OjlZl_WH57mhel5ZRRUummNxwJdnaqGrjmLWOSqas4MoQbHGDOV7zikkCzhFn-IZtJG4MMZYqTiU9KF5M725Nq3OOnYk3OhivV_Naj3cAHFeUV1c422eT3cfwY3Cp1zufrGtb07kwJK2AMVFxgCyf3ymxlEAkEYxm-uQfehGG2OWZdSVAYqXo-PPT_yGshMCUQTWql5OyMaQUXXM7EAY97lz_vfPM6cSvfetu7rT6ZPlpToDBmLecuvKe3c_bLhMvtZBUcv31_VJz8fH7m2-rU_2W_gLi17hY</recordid><startdate>201007</startdate><enddate>201007</enddate><creator>NaitAmor, S.</creator><creator>AlAbdoadaim, M. 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A.</au><au>Cohen, M. B.</au><au>Cotts, B. R. T.</au><au>Soula, S.</au><au>Chanrion, O.</au><au>Neubert, T.</au><au>Abdelatif, T.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>VLF observations of ionospheric disturbances in association with TLEs from the EuroSprite-2007 campaign</atitle><jtitle>Journal of Geophysical Research: Space Physics</jtitle><addtitle>J. Geophys. Res</addtitle><date>2010-07</date><risdate>2010</risdate><volume>115</volume><issue>A7</issue><epage>n/a</epage><issn>0148-0227</issn><issn>2169-9380</issn><eissn>2156-2202</eissn><eissn>2169-9402</eissn><abstract>Two Very Low Frequency (VLF) AWESOME remote sensing systems located at Algiers, Algeria (36.45°N, 3.28°E) and Sebha, Libya (27.02°N, 14.26°E) monitor VLF signal perturbations for evidence of ionospheric disturbances. During the EuroSprite‐2007 campaign a number of Transient Luminous Events (TLEs) were captured over the Mediterranean Sea by cameras at Pic du Midi (42.94°N, 0.14°E) and at Centre de Recherches Atmosphériques (CRA) in southwestern France (43.13°N, 0.37°E). The cameras observations are compared to collected VLF AWESOME data. We consider early VLF perturbations observed on 12–13, 17–18 October and 17–18 December, 2007. The data from the two VLF receivers confirm the association between TLEs and early VLF signal perturbations with the perturbations amplitudes dependent on the observation configuration i.e. whether the TLE is near the receiver, near the transmitter, or far from both and the scattering process. The results also reveal that the early VLF perturbations can occur in the absence of a TLE.</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2009JA015026</doi><tpages>9</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Algeria Atmospheric and Oceanic Physics Atmospheric sciences Cameras Early Ionospheric disturbances Lightning Mediterranean Sea Monitors Perturbation Physics Receivers Remote sensing Remote sensing systems Transient luminous events Very Low Frequencies VLF VLF signals perturbations |
title | VLF observations of ionospheric disturbances in association with TLEs from the EuroSprite-2007 campaign |
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