Secondary gigantic jets as possible inducers of sprites

Three multi‐transient luminous events, which were recorded by ISUAL on FORMOSAT‐2 and shared a similar generating sequence, are reported. Each event began with a positive cloud‐to‐ground lightning discharge (CG)‐induced sprite, and a secondary gigantic jet (GJ) followed within ~30–50 ms. Then, 1 ms...

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Veröffentlicht in:Geophysical research letters 2013-04, Vol.40 (8), p.1462-1467
Hauptverfasser: Lee, Li-Jou, Hsu, Rue-Ron, Su, Han-Tzong, Huang, Sung-Ming, Chou, Jung-Kung, Kuo, Cheng-Ling, Chang, Shu-Chun, Wu, Yen-Jung, Chen, Alfred B., Frey, Harald U., Takahashi, Yukihiro, Lee, Lou-Chuang
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container_end_page 1467
container_issue 8
container_start_page 1462
container_title Geophysical research letters
container_volume 40
creator Lee, Li-Jou
Hsu, Rue-Ron
Su, Han-Tzong
Huang, Sung-Ming
Chou, Jung-Kung
Kuo, Cheng-Ling
Chang, Shu-Chun
Wu, Yen-Jung
Chen, Alfred B.
Frey, Harald U.
Takahashi, Yukihiro
Lee, Lou-Chuang
description Three multi‐transient luminous events, which were recorded by ISUAL on FORMOSAT‐2 and shared a similar generating sequence, are reported. Each event began with a positive cloud‐to‐ground lightning discharge (CG)‐induced sprite, and a secondary gigantic jet (GJ) followed within ~30–50 ms. Then, 1 ms after the GJ, a new sprite occurred near the GJ without associated impulsive lightning signal. The associated electromagnetic signal for one of the events indicates that the GJ is a negative cloud‐to‐ionosphere discharge carrying a high peak current moment. Cross‐analysis of the spectral, image, and electromagnetic data of these three events indicates that the new sprites are likely induced by the secondary GJs, and the high current moment of the secondary GJs appears to be a crucial factor for the induction of the new sprites. Hence, these secondary GJs may have played a role in inducing sprites as much as the negative CGs do for the occurrence of negative sprites. Key Points Three possible GJ‐induced sprites observed by ISUAL are analyzed and reported The high current moment GJs may be the key factor in the induction of sprites The secondary GJ discharge seems to be more impulsive than the typical GJs
doi_str_mv 10.1002/grl.50300
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Each event began with a positive cloud‐to‐ground lightning discharge (CG)‐induced sprite, and a secondary gigantic jet (GJ) followed within ~30–50 ms. Then, 1 ms after the GJ, a new sprite occurred near the GJ without associated impulsive lightning signal. The associated electromagnetic signal for one of the events indicates that the GJ is a negative cloud‐to‐ionosphere discharge carrying a high peak current moment. Cross‐analysis of the spectral, image, and electromagnetic data of these three events indicates that the new sprites are likely induced by the secondary GJs, and the high current moment of the secondary GJs appears to be a crucial factor for the induction of the new sprites. Hence, these secondary GJs may have played a role in inducing sprites as much as the negative CGs do for the occurrence of negative sprites. Key Points Three possible GJ‐induced sprites observed by ISUAL are analyzed and reported The high current moment GJs may be the key factor in the induction of sprites The secondary GJ discharge seems to be more impulsive than the typical GJs</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1002/grl.50300</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Cloud-to-ground lightning ; Discharge ; Electromagnetic induction ; Geophysics ; Giganitc jet ; High current ; Image processing ; Ionosphere ; Jets ; Lightning ; Lightning discharges ; Meteorology ; Sequencing ; Spectra ; Sprite ; Sprites ; TLEs ; Transient luminous events</subject><ispartof>Geophysical research letters, 2013-04, Vol.40 (8), p.1462-1467</ispartof><rights>2013. American Geophysical Union. 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Res. Lett</addtitle><description>Three multi‐transient luminous events, which were recorded by ISUAL on FORMOSAT‐2 and shared a similar generating sequence, are reported. Each event began with a positive cloud‐to‐ground lightning discharge (CG)‐induced sprite, and a secondary gigantic jet (GJ) followed within ~30–50 ms. Then, 1 ms after the GJ, a new sprite occurred near the GJ without associated impulsive lightning signal. The associated electromagnetic signal for one of the events indicates that the GJ is a negative cloud‐to‐ionosphere discharge carrying a high peak current moment. Cross‐analysis of the spectral, image, and electromagnetic data of these three events indicates that the new sprites are likely induced by the secondary GJs, and the high current moment of the secondary GJs appears to be a crucial factor for the induction of the new sprites. Hence, these secondary GJs may have played a role in inducing sprites as much as the negative CGs do for the occurrence of negative sprites. Key Points Three possible GJ‐induced sprites observed by ISUAL are analyzed and reported The high current moment GJs may be the key factor in the induction of sprites The secondary GJ discharge seems to be more impulsive than the typical GJs</description><subject>Cloud-to-ground lightning</subject><subject>Discharge</subject><subject>Electromagnetic induction</subject><subject>Geophysics</subject><subject>Giganitc jet</subject><subject>High current</subject><subject>Image processing</subject><subject>Ionosphere</subject><subject>Jets</subject><subject>Lightning</subject><subject>Lightning discharges</subject><subject>Meteorology</subject><subject>Sequencing</subject><subject>Spectra</subject><subject>Sprite</subject><subject>Sprites</subject><subject>TLEs</subject><subject>Transient luminous events</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><recordid>eNp9kF1LwzAUhoMoOKcX_oOCN3rR7eSjTXspU6tQFL_Qu9A1pyOza2fSovv3xk29EBQCCeF5X855CDmkMKIAbDyz9SgCDrBFBjQVIkwA5DYZAKT-zWS8S_acmwN4htMBkfdYto0u7CqYmVnRdKYM5ti5oHDBsnXOTGsMTKP7Eq0L2ipwS2s6dPtkpypqhwdf95A8Xpw_TC7D_Ca7mpzmYSk4hbAQEed8KiuOEqYakaWxTmVUQYWVKCOAKEVYfxWppgkwf6TGVOsKADkfkuNN79K2rz26Ti2MK7Guiwbb3ikaCSoYkwnz6NEvdN72tvHTKW-Citg383-pWDAQaSIST51sqNJ6CRYr5ddeeEuKgvoUrbxotRbt2fGGfTM1rv4GVXaXfyfCTcK4Dt9_EoV9UbHkMlJP15mK8uxZnslbJfkH_COLew</recordid><startdate>20130428</startdate><enddate>20130428</enddate><creator>Lee, Li-Jou</creator><creator>Hsu, Rue-Ron</creator><creator>Su, Han-Tzong</creator><creator>Huang, Sung-Ming</creator><creator>Chou, Jung-Kung</creator><creator>Kuo, Cheng-Ling</creator><creator>Chang, Shu-Chun</creator><creator>Wu, Yen-Jung</creator><creator>Chen, Alfred B.</creator><creator>Frey, Harald U.</creator><creator>Takahashi, Yukihiro</creator><creator>Lee, Lou-Chuang</creator><general>Blackwell Publishing Ltd</general><general>John Wiley &amp; 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subjects Cloud-to-ground lightning
Discharge
Electromagnetic induction
Geophysics
Giganitc jet
High current
Image processing
Ionosphere
Jets
Lightning
Lightning discharges
Meteorology
Sequencing
Spectra
Sprite
Sprites
TLEs
Transient luminous events
title Secondary gigantic jets as possible inducers of sprites
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