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Mesospheric short-period gravity waves in the Antarctic Peninsula observed in all-sky airglow images and their possible source locations

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dc.contributor.authorKam, Hosik-
dc.contributor.authorSong, In-Sun-
dc.contributor.authorKim, Jeong-Han-
dc.contributor.authorKim, Yong Ha-
dc.contributor.authorSong, Byeong-Gwon-
dc.contributor.authorNakamura, Takuji-
dc.contributor.authorTomikawa, Yoshihiro-
dc.contributor.authorKogure, Masaru-
dc.contributor.authorEjiri, Mitsumu K.-
dc.contributor.authorPerwitasari, Septi-
dc.contributor.authorTsutsumi, Masaki-
dc.contributor.authorKwak, Young-Sil-
dc.date.accessioned2022-03-14T07:05:15Z-
dc.date.available2022-03-14T07:05:15Z-
dc.date.issued2021-12-27-
dc.identifier.urihttps://repository.kopri.re.kr/handle/201206/13265-
dc.description.abstractThis study presents an analysis of OH airglow images observed from an all-sky camera (ASC) at King Sejong Station (KSS), Antarctic for the 2012?2016 period. The two- dimensional power spectra of short-period gravity waves (< 1 h) as a function of phase velocities are obtained using the M-transform method that employs the time sequence of ASC images. The amplitudes of the power spectral densities show that the mesospheric wave activity is the largest during winter (May, June, and July) and is the smallest in fall (February, March, and April). Wind-blocking diagrams are constructed on the same two-dimensional domain as in the two-dimensional spectra using horizontal winds obtained from MERRA-2 reanalysis at z = 0?80 km and from KSS meteor radar data at z = 80?90 km. Climatologically, the spectral regions of slowly propagating gravity waves (< 30 m s-1) are overlaid by the wind-blocking areas, which suggests the filtering of gravity waves with small phase speeds by winds below the upper stratosphere. Eastward propagating gravity waves in winter and intense south- eastward waves in spring (October) are found to be unfiltered by the stratospheric winds. It is also found from the spectral analysis that these unfiltered gravity waves can originate from the upper stratosphere or the lower mesosphere, and not from the troposphere, which suggests the possibility of ASC observation of the secondary gravity waves generated near the stratopause.en_US
dc.languageEnglishen_US
dc.language.isoenen_US
dc.subjectMeteorology & Atmospheric Sciencesen_US
dc.subject.classificationKing Sejong Stationen_US
dc.titleMesospheric short-period gravity waves in the Antarctic Peninsula observed in all-sky airglow images and their possible source locationsen_US
dc.title.alternative대기광 관측 자료를 활용한 남극반도 상공 중간권에서의 단주기 대기중량파 특성과 이들 파동의 잠재적 원천 고도 연구en_US
dc.typeArticleen_US
dc.identifier.bibliographicCitationKam, Hosik, et al. 2021. "Mesospheric short-period gravity waves in the Antarctic Peninsula observed in all-sky airglow images and their possible source locations". <em>JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES</em>, 126(24): 1-12.-
dc.citation.titleJOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERESen_US
dc.citation.volume126en_US
dc.citation.number24en_US
dc.identifier.doi10.1029/2021JD035842-
dc.citation.startPage1en_US
dc.citation.endPage12en_US
dc.description.articleClassificationSCIE-
dc.description.jcrRateJCR 2019:27.957en_US
dc.subject.keywordmesospheric short-period gravity waveen_US
dc.subject.keywordAntarctic Peninsulaen_US
dc.subject.keywordwind filtering effecten_US
dc.identifier.localId2021-0356-
dc.identifier.scopusid2-s2.0-85121751323-
dc.identifier.wosid000735878700027-
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