{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1360004233289296128.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2011jd017025"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011JD017025"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2011JD017025"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Mesospheric concentric gravity waves generated by multiple convective storms over the North American Great Plain"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We report on six continuous hours of OH airglow imager observations (at z ∼ 87 km) of convectively generated gravity waves (GWs) near Fort Collins, Colorado, on the evening of 08 September 2005. These GWs appeared as nearly concentric rings, and had epicenters near the locations of deep convection in three thunderstorms in Colorado, Nebraska and South Dakota. Using GOES satellite and weather radar observations, we show that the GWs closely follow the thunderstorms. Using the background wind from a nearby radar, the intrinsic wave parameters and vertical wavelengths are calculated. The temperature perturbations are estimated to be \n<jats:inline-graphic xmlns:xlink=\"http://www.w3.org/1999/xlink\" xlink:href=\"graphic/jgrd17761-math-0001.gif\" xlink:title=\"urn:x-wiley:01480227:media:jgrd17761:jgrd17761-math-0001\"/> ∼ 1–3% for GWs with horizontal wavelengths <jats:italic>λ</jats:italic><jats:sub><jats:italic>h</jats:italic></jats:sub>∼ 20–40 km and horizontal phase speeds ∼40–60 m/s. The horizontal wavelengths of GWs from a convective cluster decreased in time from 30 to 15 km. We employ convective plume and ray‐trace models to simulate the GW‐induced OH intensity perturbations from convective plumes, clusters and complexes. We find that the results using the background model wind (radiosonde/TIME‐GCM) agree well with the late‐time observations, when the images are dominated by southwestward, short‐wavelength, high‐frequency GWs. These late‐time GWs propagate against the background wind, and have<jats:italic>λ</jats:italic><jats:sub><jats:italic>h</jats:italic></jats:sub> ∼ 30–40 km and periods of <jats:italic>τ</jats:italic> ∼ 20–30 min. The OH intensity perturbations are enhanced because the vertical wavelengths <jats:italic>λ</jats:italic><jats:sub><jats:italic>z</jats:italic></jats:sub> increased, \n<jats:inline-graphic xmlns:xlink=\"http://www.w3.org/1999/xlink\" xlink:href=\"graphic/jgrd17761-math-0001.gif\" xlink:title=\"urn:x-wiley:01480227:media:jgrd17761:jgrd17761-math-0001\"/> increased, and the vertical velocity perturbations <jats:italic>w</jats:italic>′ decreased (because the GWs were near their reflection levels). We also find that these short‐wavelength GWs were created ∼5 h earlier by an extremely energetic, deep convective plume in South Dakota, thereby showing that small‐scale, convective GWs directly link the troposphere and mesopause region.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004233289296142","@type":"Researcher","foaf:name":[{"@value":"Sharon Vadas"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233289296009","@type":"Researcher","foaf:name":[{"@value":"Jia Yue"}]},{"@id":"https://cir.nii.ac.jp/crid/1420001326209115648","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"40217857"},{"@type":"NRID","@value":"1000040217857"},{"@type":"NRID","@value":"9000005913553"},{"@type":"NRID","@value":"9000363503794"},{"@type":"NRID","@value":"9000363410747"},{"@type":"NRID","@value":"9000364037435"},{"@type":"NRID","@value":"9000364000889"},{"@type":"NRID","@value":"9000363406682"},{"@type":"NRID","@value":"9000408855540"},{"@type":"NRID","@value":"9000253044013"},{"@type":"NRID","@value":"9000363502827"},{"@type":"NRID","@value":"9000002455223"},{"@type":"NRID","@value":"9000364037418"},{"@type":"NRID","@value":"9000254739605"},{"@type":"NRID","@value":"9000392818984"},{"@type":"NRID","@value":"9000002343622"},{"@type":"NRID","@value":"9000363408544"},{"@type":"NRID","@value":"9000002453208"},{"@type":"NRID","@value":"9000318570462"},{"@type":"NRID","@value":"9000367053856"},{"@type":"NRID","@value":"9000000143748"},{"@type":"NRID","@value":"9000003269958"},{"@type":"NRID","@value":"9000364038137"},{"@type":"NRID","@value":"9000364039453"},{"@type":"NRID","@value":"9000253660759"},{"@type":"NRID","@value":"9000257767530"},{"@type":"NRID","@value":"9000014144280"},{"@type":"NRID","@value":"9000003228967"},{"@type":"NRID","@value":"9000363407055"},{"@type":"NRID","@value":"9000363406401"},{"@type":"NRID","@value":"9000370752007"},{"@type":"NRID","@value":"9000005305907"},{"@type":"NRID","@value":"9000244914713"},{"@type":"NRID","@value":"9000242877349"},{"@type":"NRID","@value":"9000253660448"},{"@type":"NRID","@value":"9000409807535"},{"@type":"NRID","@value":"9000002468324"},{"@type":"NRID","@value":"9000363981782"},{"@type":"NRID","@value":"9000363959280"},{"@type":"NRID","@value":"9000363404949"},{"@type":"NRID","@value":"9000254739705"},{"@type":"NRID","@value":"9000410971377"},{"@type":"NRID","@value":"9000363502809"},{"@type":"NRID","@value":"9000363406166"},{"@type":"NRID","@value":"9000254739658"},{"@type":"NRID","@value":"9000003231747"},{"@type":"NRID","@value":"9000405742344"},{"@type":"NRID","@value":"9000020523627"},{"@type":"NRID","@value":"9000021782997"},{"@type":"NRID","@value":"9000405746829"},{"@type":"NRID","@value":"9000345258212"},{"@type":"NRID","@value":"9000002683903"},{"@type":"NRID","@value":"9000252918184"},{"@type":"NRID","@value":"9000363410780"},{"@type":"NRID","@value":"9000410265199"},{"@type":"NRID","@value":"9000408879959"},{"@type":"NRID","@value":"9000292188140"},{"@type":"NRID","@value":"9000003231591"},{"@type":"NRID","@value":"9000005884990"},{"@type":"NRID","@value":"9000244911955"},{"@type":"NRID","@value":"9000305613991"},{"@type":"NRID","@value":"9000363404660"},{"@type":"NRID","@value":"9000363496819"},{"@type":"NRID","@value":"9000363404599"},{"@type":"NRID","@value":"9000363502785"},{"@type":"NRID","@value":"9000363404814"},{"@type":"NRID","@value":"9000363503390"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0012993"}],"foaf:name":[{"@value":"Takuji Nakamura"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Atmospheres"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2012-04-14","prism:volume":"117","prism:number":"D7"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011JD017025"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2011JD017025"}],"createdAt":"2012-03-12","modifiedAt":"2023-10-30","project":[{"@id":"https://cir.nii.ac.jp/crid/1040282257046933248","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"21340141"},{"@type":"JGN","@value":"JP21340141"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-21340141/"}],"notation":[{"@language":"ja","@value":"ライダーを活用した中層・超高層大気結合の協同観測-乱流圏界面の解明に向けて-"},{"@language":"en","@value":"Cooperative observations of the couplings of the middle and upper atmosphere utilizing lidars-towards the study of turbopause-"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257174455936","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"24340121"},{"@type":"JGN","@value":"JP24340121"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-24340121/"}],"notation":[{"@language":"ja","@value":"新技術ライダー観測を活用した超高層大気下部の化学過程と物質輸送の研究"},{"@language":"en","@value":"Chemistry and transport at the bottom of the upper atmosphere using novel lidar observations"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282810790115968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"First spaceborne observation of the entire concentric airglow structure caused by tropospheric disturbance"},{"@value":"Evidence for global electron transportation into the jovian inner magnetosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142935411328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Turbulence and stress owing to gravity wave and tidal breakdown"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143559941632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Small‐scale gravity waves in the upper mesosphere and lower thermosphere generated by deep tropical convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143957939968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A simulation study of space‐based observations of gravity waves in the airglow using observed ALOHA‐93 wave parameters"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144038972032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effects of eddy viscosity and thermal conduction and Coriolis force in the dynamics of gravity wave driven fluctuations in the OH nightglow"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144737458176","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Thermospheric responses to gravity waves arising from mesoscale convective complexes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145949184896","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A dynamical‐chemical model of wave‐driven fluctuations in the OH nightglow"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704780814208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coordinated airglow observations between IMAP/VISI and a ground‐based all‐sky imager on concentric gravity wave in the mesopause"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292618494924160","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Characteristics and Momentum Flux Spectrum of Convectively Forced Internal Gravity Waves in Ensemble Numerical Simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179759409024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Three years of concentric gravity wave variability in the mesopause as observed by IMAP/VISI"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567180128991232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Links between mesopause temperatures and ground‐based VLF narrowband radio signals"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092436773120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"First Direct Observational Evidence for Secondary Gravity Waves Generated by Mountain Waves Over the Andes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092887971712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Gravity wave dynamics and effects in the middle atmosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574093672781184","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A full‐wave investigation of the use of a “cancellation factor” in gravity wave–OH airglow interaction studies"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095333933568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the nature of traveling ionospheric disturbances launched by low-altitude nuclear explosions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095568587392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Mechanism for the Generation of Acoustic-Gravity Waves During Thunderstorm Formation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096188835072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Occurrence frequency of convective gravity waves during the North American thunderstorm season"}]},{"@id":"https://cir.nii.ac.jp/crid/1360579819685605504","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Gravity waves in the mesosphere generated by tropospheric convention"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846639278563584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Typhoon-induced concentric airglow structures in the mesopause region"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855568785957888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mesospheric gravity wave imaging at a subauroral site: First results from Millstone Hill"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569175586560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A thermosphere‐ionosphere‐mesosphere‐electrodynamics general circulation model (time‐GCM): Equinox solar cycle minimum simulations (30–500 km)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869855143657344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Gravity waves generated by the Hunga Tonga–Hunga Ha′apai volcanic eruption and their global propagation in the mesosphere/lower thermosphere observed by meteor radars and modeled with the High-Altitude general Mechanistic Circulation Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043750182144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Analytical models for the responses of the mesospheric OH* and Na layers to atmospheric gravity waves"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044209407616","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effects of Nonlinearity on Convectively Forced Internal Gravity Waves: Application to a Gravity Wave Drag Parameterization"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519308122496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Wave‐driven fluctuations in OH nightglow from an extended source region"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993832788864","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Two-dimensional spectral analysis of mesospheric airglow image data"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995903741696","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Convectively generated mesoscale gravity waves simulated throughout the middle atmosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468378352768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Numerical Modeling of Gravity Wave Generation by Deep Tropical Convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943468228480","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The effect of breaking gravity waves on the dynamics and chemical composition of the mesosphere and lower thermosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945074926592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"ALOHA‐93 measurements of intrinsic AGW characteristics using airborne airglow imager and groundbased Na wind/temperature lidar"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262946361441280","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Concentric gravity waves in the mesosphere generated by deep convective plumes in the lower atmosphere near Fort Collins, Colorado"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544418814148480","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"All‐sky measurements of short period waves imaged in the OI(557.7 nm), Na(589.2 nm) and near infrared OH and O<sub>2</sub>(0,1) nightglow emissions during the ALOHA‐93 Campaign"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544421030080000","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Simultaneous observation of dual-site airglow imagers and a sodium temperature-wind lidar, and effect of atmospheric stability on the airglow structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544421278711680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Wavelength dependence of eddy dissipation and coriolis force in the dynamics of gravity wave driven fluctuations in the OH nightglow"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544421378238592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A modeling study of O<sub>2</sub> and OH airglow perturbations induced by atmospheric gravity waves"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893855696000","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A model study of the effects of winds on concentric rings of gravity waves from a convective plume near Fort Collins on 11 May 2004"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895347172992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Convection: the likely source of the medium-scale gravity waves observed in the OH airglow  layer near Brasilia, Brazil, during the SpreadFEx campaign"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368614573696","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Generation of large‐scale gravity waves and neutral winds in the thermosphere from the dissipation of convectively generated gravity waves"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319837742720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Gravity wave breaking, secondary wave generation, and mixing above deep convection in a three‐dimensional cloud model"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320383276800","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"MSX satellite observations of thunderstorm‐generated gravity waves in mid‐wave infrared images of the upper stratosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320397437696","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sources of the traveling ionospheric disturbances observed by the ionospheric TIDDBIT sounder near Wallops Island on 30 October 2007"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794166531712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An idealized ray model of gravity wave‐tidal interactions"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795210167936","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Gravity waves generated by convection in the Darwin area during the Darwin Area Wave Experiment"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795219376000","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A concentric gravity wave structure in the mesospheric airglow images"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795706147328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Earth observations during space shuttle mission STS‐55:<i>Columbia's</i>mission to planet earth (April 26 ‐ May 6, 1993)"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269227904128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Model Study of Waves Generated by Convection with Direct Validation via Satellite"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269974168064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Ionospheric and dynamical characteristics of the mesosphere‐lower thermosphere region over Platteville (40°N, 105°W) and comparisons with the region over Saskatoon (52°N, 107°W)"}]},{"@id":"https://cir.nii.ac.jp/crid/1370004233289296013","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Forecasting hailfall in Alberta"}]},{"@id":"https://cir.nii.ac.jp/crid/1370016861870307458","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016862801250691","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016864271634048","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016864271634049","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016864271634051","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016864271634053","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016864271634054","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016864271634055","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016864271634056","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016864271634057","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016864271634058","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016864271634059","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016864271634060","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016864271634062","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016864271634063","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016864271634064","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016864271634065","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016864271634066","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370016864271634067","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1571698599922781952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Infrasonic variation of OH emission in the upper atmosphere"},{"@value":"Infrasonic variations of OH emissions in the upper atmosphere"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2011jd017025"},{"@type":"KAKEN","@value":"PRODUCT-12656660"},{"@type":"KAKEN","@value":"PRODUCT-12656722"},{"@type":"KAKEN","@value":"PRODUCT-14543369"},{"@type":"OPENAIRE","@value":"doi_dedup___::e9cd834964f4dd64b2a80b57d23cc8ce"},{"@type":"CROSSREF","@value":"10.1002/2014gl061403_references_DOI_Uo68EQmPZ7lTta28LhyeXNfL2kZ"},{"@type":"CROSSREF","@value":"10.1002/2015ja021424_references_DOI_Uo68EQmPZ7lTta28LhyeXNfL2kZ"},{"@type":"CROSSREF","@value":"10.1002/2016gl071511_references_DOI_Uo68EQmPZ7lTta28LhyeXNfL2kZ"},{"@type":"CROSSREF","@value":"10.1002/jgrd.50379_references_DOI_Uo68EQmPZ7lTta28LhyeXNfL2kZ"},{"@type":"CROSSREF","@value":"10.1029/2020gl088845_references_DOI_Uo68EQmPZ7lTta28LhyeXNfL2kZ"},{"@type":"CROSSREF","@value":"10.1002/2013gl058087_references_DOI_Uo68EQmPZ7lTta28LhyeXNfL2kZ"},{"@type":"CROSSREF","@value":"10.5194/acp-24-4851-2024_references_DOI_Uo68EQmPZ7lTta28LhyeXNfL2kZ"}]}