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dc.contributor.authorChen, Alfred B.en_US
dc.contributor.authorKuo, Cheng-Lingen_US
dc.contributor.authorLee, Yi-Jenen_US
dc.contributor.authorSu, Han-Tzongen_US
dc.contributor.authorHsu, Rue-Ronen_US
dc.contributor.authorChern, Jyh-Longen_US
dc.contributor.authorFrey, Harald U.en_US
dc.contributor.authorMende, Stephen B.en_US
dc.contributor.authorTakahashi, Yukihiroen_US
dc.contributor.authorFukunishi, Hiroshien_US
dc.contributor.authorChang, Yeou-Shinen_US
dc.contributor.authorLiu, Tie-Yueen_US
dc.contributor.authorLee, Lou-Chuangen_US
dc.date.accessioned2014-12-08T15:11:03Z-
dc.date.available2014-12-08T15:11:03Z-
dc.date.issued2008-08-15en_US
dc.identifier.issn0148-0227en_US
dc.identifier.urihttp://dx.doi.org/10.1029/2008JA013101en_US
dc.identifier.urihttp://hdl.handle.net/11536/8465-
dc.description.abstractWe report the global transient luminous event (TLE) distributions and rates based on the Imager of Sprites and Upper Atmospheric Lightning (ISUAL) experiment onboard the FORMOSAT-2 satellite. ISUAL observations cover 45 degrees S to 25 degrees N latitude during the northern summer and 25 degrees S to 45 degrees N latitude during the northern winter. From July 2004 to June 2007, ISUAL recorded 5,434 elves, 633 sprites, 657 halos, and 13 gigantic jets. Surprisingly, elve is the dominant type of TLEs, while sprites/halos are a distant second. Elve occurrence rate jumps as the sea surface temperature exceeds 26 degrees Celsius, manifesting an ocean-atmosphere-ionosphere coupling. In the ISUAL survey, elves concentrate over the Caribbean Sea, South China Sea, east Indian Ocean, central Pacific Ocean, west Atlantic Ocean, and southwest Pacific Ocean; while sprites congregate over central Africa, Japan Sea, and west Atlantic Ocean. The ISUAL experiment observed global rates of 3.23, 0.50, 0.39, and 0.01 events per minute for elves, sprites, halos, and gigantic jets, respectively. Taking the instrumental detection sensitivity and the restricted survey area into account, the corrected global occurrence rates for sprites and elves likely are a factor of two and an order of magnitude higher, respectively. ISUAL observations also indicate that the relative frequency of high peak current lightning (> 80 kA) is 10 times higher over the oceans than over the land. On the basis of the corrected ISUAL elve global occurrence rate, the total electron content at the lower ionosphere above elve hot zones was computed to be elevated by more than 5%.en_US
dc.language.isoen_USen_US
dc.titleGlobal distributions and occurrence rates of transient luminous eventsen_US
dc.typeArticleen_US
dc.identifier.doi10.1029/2008JA013101en_US
dc.identifier.journalJOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICSen_US
dc.citation.volume113en_US
dc.citation.issueA8en_US
dc.citation.epageen_US
dc.contributor.department光電工程學系zh_TW
dc.contributor.departmentDepartment of Photonicsen_US
dc.identifier.wosnumberWOS:000258515200004-
dc.citation.woscount76-
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