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Characteristics of Lightning Electromagnetic Fields Produced by Antarctica Storms

Cited 2 time in wos
Cited 3 time in scopus

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dc.contributor.authorSulaiman Ali Mohammad-
dc.contributor.authorMohd Riduan Ahmad-
dc.contributor.authorMardina Abdullah-
dc.contributor.author박상종-
dc.contributor.authorShamsul Ammar Shamsul Baharin-
dc.contributor.authorNorbayah Yusop-
dc.contributor.authorGaopeng Lu-
dc.contributor.authorVernon Cooray-
dc.date.accessioned2022-06-24T16:36:36Z-
dc.date.available2022-06-24T16:36:36Z-
dc.date.issued2022-
dc.identifier.urihttps://repository.kopri.re.kr/handle/201206/13506-
dc.description.abstractThis paper presents the temporal characteristics of electromagnetic fields produced by cloud-to-ground (CG) lightning flashes associated with Antarctica storms. A total of 51 positive CG (+CG) and 103 negative CG (-CG) flashes have been recorded by a magnetic direction finder (MDF) sensor in King Sejong Station, King George Island. In total, 47 positive and 107 negative return strokes were located, ranges from 32 to 569 km. All CG flashes were detected to occur over the ocean. The return strokes characteristics include the observations of slow front, fast rising, rise time, and pulse duration with geometric mean values of 3.2, 0.53, 3.21, 13.12, and 67.09 s for +CG flashes, while 3.9, 0.57, 3.72, 20.75, and 69.86 s for -CG flashes, respectively. Additionally, the average peak currents of +CG and -CG flashes were 4.13 kA and 3.14 kA, respectively. The temporal characteristics of the return strokes of Antarctica storms are comparable to other geographical regions. The smaller peak currents might be due to small magnitude of Antarctica cloud charges when compared to other geographical regions.-
dc.languageEnglish-
dc.subject.classificationKing Sejong Station-
dc.titleCharacteristics of Lightning Electromagnetic Fields Produced by Antarctica Storms-
dc.title.alternative남극 스톰에 의해 발생한 번개의 전자기장 특성-
dc.typeArticle-
dc.identifier.bibliographicCitationSulaiman Ali Mohammad, et al. 2022. "Characteristics of Lightning Electromagnetic Fields Produced by Antarctica Storms". <em>ATMOSPHERE</em>, 13(4): 588-604.-
dc.citation.titleATMOSPHERE-
dc.citation.volume13-
dc.citation.number4-
dc.identifier.doi10.3390/atmos13040588-
dc.citation.startPage588-
dc.citation.endPage604-
dc.description.articleClassificationSCIE-
dc.description.jcrRateJCR 2020:57.447-
dc.subject.keywordantarctica-
dc.subject.keywordcloud-to-ground-
dc.subject.keywordelectromagnetic-
dc.subject.keywordlightning-
dc.subject.keywordreturn stroke-
dc.identifier.localId2022-0090-
Appears in Collections  
2022-2022, Understanding of Antarctic climate and environment and assessments of global influence (22-22) / Kim, Seong-Joong (PE22030)
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