{"@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/2051714792052822656.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"NDL_BIB_ID","@value":"9976818"}},{"identifier":{"@type":"DOI","@value":"10.1186/s40623-016-0457-6"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/digimeta/9976818"}},{"identifier":{"@type":"URI","@value":"https://dl.ndl.go.jp/pid/9976818"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1186/s40623-016-0457-6.pdf"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/article/10.1186/s40623-016-0457-6/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1186/s40623-016-0457-6"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"AKATSUKI returns to Venus"}],"dcterms:alternative":[{"@value":"AKATSUKI returns to Venus"}],"dc:language":"en","description":[{"notation":[{"@value":"収集根拠 : オンライン資料収集制度"},{"@value":"資料形態 : テキストデータ"},{"@value":"コレクション : 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/2061714792052822658","@type":"Researcher","foaf:name":[{"@value":"Masato Nakamura"}]},{"@id":"https://cir.nii.ac.jp/crid/2061714792052822656","@type":"Researcher","foaf:name":[{"@value":"Takeshi Imamura"}]},{"@id":"https://cir.nii.ac.jp/crid/2061714792052822657","@type":"Researcher","foaf:name":[{"@value":"Nobuaki Ishii"}]}],"publication":{"publicationIdentifier":[{"@type":"ISSN","@value":"18805981"},{"@type":"LISSN","@value":"13438832"},{"@type":"EISSN","@value":"18805981"}],"prism:publicationName":[{"@value":"EPS : Earth, Planets and Space"}],"dc:publisher":[{"@value":"Springer science+business media"}],"prism:publicationDate":"2016-05-06","prism:volume":"68(75)","prism:startingPage":"75"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/digimeta/9976818"},{"@id":"https://dl.ndl.go.jp/pid/9976818"},{"@id":"http://link.springer.com/content/pdf/10.1186/s40623-016-0457-6.pdf"},{"@id":"http://link.springer.com/article/10.1186/s40623-016-0457-6/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1186/s40623-016-0457-6"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781829330816","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15H03734"},{"@type":"JGN","@value":"JP15H03734"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15H03734/"}],"notation":[{"@language":"ja","@value":"極周回成層圏テレスコープ（風神）を用いた金星大気変動現象の研究"},{"@language":"en","@value":"A study on temporal variation of the Venus atmosphere using a circumpolar stratospheric telescope FUJIN"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000781924278272","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16K17816"},{"@type":"JGN","@value":"JP16K17816"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-16K17816/"}],"notation":[{"@language":"ja","@value":"金星の雲層構造と紫外模様起源"},{"@language":"en","@value":"Venus cloud structure and origin of UV contrast"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000782438326784","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"13J09370"},{"@type":"JGN","@value":"JP13J09370"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-13J09370/"}],"notation":[{"@language":"ja","@value":"飛翔体からの観測データにより解き明かす木星・土星雲層構造の時空間変化"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256821660800","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15K05303"},{"@type":"JGN","@value":"JP15K05303"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15K05303/"}],"notation":[{"@language":"ja","@value":"大気プラズマ結合過程の研究 ー日米共同実験ー"},{"@language":"en","@value":"Coupling between neutral atmosphere and plasma"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256878530944","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H05738"},{"@type":"JGN","@value":"JP16H05738"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-16H05738/"}],"notation":[{"@language":"ja","@value":"ハワイ高高度施設と「あかつき」のコラボ：金星の後光から探る大気駆動メカニズム"},{"@language":"en","@value":"Collaboration between Akatsuki and high-altitude observatories: Venus glory and atmospheric dynamics in clouds"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050012570393345792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Planetary-scale streak structure reproduced in high-resolution simulations of the Venus atmosphere with a low-stability layer"},{"@value":"Planetary-scale streak structure reproduced in a Venus atmospheric simulation"}]},{"@id":"https://cir.nii.ac.jp/crid/1050012570393551360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Overview of Akatsuki data products: definition of data levels, method and accuracy of geometric correction"}]},{"@id":"https://cir.nii.ac.jp/crid/1050025031475140096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"How waves and turbulence maintain the super-rotation of Venus' atmosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1050575520346926592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Performance of Akatsuki/IR2 in Venus orbit: the first year"}]},{"@id":"https://cir.nii.ac.jp/crid/1050575520347193216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Absolute calibration of brightness temperature of the Venus disk observed by the Longwave Infrared Camera onboard Akatsuki"}]},{"@id":"https://cir.nii.ac.jp/crid/1050856995322406656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stationary Features at the Cloud Top of Venus Observed by Ultraviolet Imager Onboard Akatsuki"}]},{"@id":"https://cir.nii.ac.jp/crid/1050856995323578240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Initial performance of the radio occultation experiment in the Venus orbiter mission Akatsuki"}]},{"@id":"https://cir.nii.ac.jp/crid/1050856995323890688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Ultraviolet imager on Venus orbiter Akatsuki and its initial results"},{"@value":"Mean winds at the cloud top of Venus obtained from two-wavelength UV imaging by Akatsuki"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214351363072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Topographical and Local Time Dependence of Large Stationary Gravity Waves Observed at the Cloud Top of Venus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232184247424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Characteristic features in Venus’ nightside cloud-top temperature obtained by Akatsuki/LIR"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232184412544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ground-based observation of the cyclic nature and temporal variability of planetary-scale UV features at the Venus cloud top level"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233436824448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Equatorial jet in the lower to middle cloud layer of Venus revealed by Akatsuki"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005518173730176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Planetary‐Scale Variations in Winds and UV Brightness at the Venusian Cloud Top: Periodicity and Temporal Evolution"}]},{"@id":"https://cir.nii.ac.jp/crid/1360008697851467264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Vertical Coupling Between the Cloud‐Level Atmosphere and the Thermosphere of Venus Inferred From the Simultaneous Observations by Hisaki and Akatsuki"}]},{"@id":"https://cir.nii.ac.jp/crid/1360008697851478400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermal Tides in the Upper Cloud Layer of Venus as Deduced From the Emission Angle Dependence of the Brightness Temperature by Akatsuki/LIR"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142935145984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Venus's major cloud feature as an equatorially trapped wave distorted by the wind"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142938623488","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Felsic highland crust on Venus suggested by Galileo Near‐Infrared Mapping Spectrometer data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142939454336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On observing the compositional variability of the surface of Venus using nightside near‐infrared thermal radiation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142940167168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Morphology of the cloud tops as observed by the Venus Express Monitoring Camera"}]},{"@id":"https://cir.nii.ac.jp/crid/1360012878116849280","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Characterising atmospheric gravity waves on the nightside lower clouds of Venus: a systematic analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360014249225565952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Gigantic Vortices From Barotropic Instability Observed in the Atmosphere of Venus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021389823062528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Periodic Variation of Mesoscale Ultraviolet Contrast at the Cloud Top of Venus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025429436569856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A GCM study of synoptic-scale vortices in the lower cloud layer on Venus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025430652075648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Probing solar wind velocity from simultaneous superior solar conjunction radio science experiments of BepiColombo and Akatsuki missions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285706915315712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Return to Venus of the Japanese Venus Climate Orbiter AKATSUKI"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707161052160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Cloud top structure of Venus revealed by Subaru/COMICS mid-infrared images"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707161058816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Venus’ clouds as inferred from the phase curves acquired by IR1 and IR2 on board Akatsuki"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708269382656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fine Vertical Structures at the Cloud Heights of Venus Revealed by Radio Holographic Analysis of Venus Express and Akatsuki Radio Occultation Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708413501952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Large stationary gravity wave in the atmosphere of Venus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617864741632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Superrotation in Planetary Atmospheres"}]},{"@id":"https://cir.nii.ac.jp/crid/1360291932833393792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Horizontal structures of bow-shaped mountain wave trains seen in thermal infrared images of venusian clouds taken by Akatsuki LIR"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617907655936","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Venus Express—The first European mission to Venus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617909791360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Images from Galileo of the Venus Cloud Deck"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617912041472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Planet-C: Venus Climate Orbiter mission of Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617912199552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"HDO and SO<sub>2</sub>thermal mapping on Venus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617912708992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Elucidating the Rate of Volcanism on Venus: Detection of Lava Eruptions Using Near-Infrared Observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617915247232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A reanalysis of Venus winds at two cloud levels from Galileo SSI images"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617916810112","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Lightning Detection by LAC Onboard the Japanese Venus Climate Orbiter, Planet-C"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617917737472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Gravity Wave Packets in the Venusian Atmosphere Observed by Radio Occultation Experiments: Comparison With Saturation Theory"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617917750400","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Structure and meteorology of the middle atmosphere of Venus: Infrared remote sensing from the Pioneer Orbiter"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643708714496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"BepiColombo Science Investigations During Cruise and Flybys at the Earth, Venus and Mercury"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643792861440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Kelvin Wave and Its Impact on the Venus Atmosphere Tested by Observing System Simulation Experiment"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298337126749312","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Long‐Term Variation of the Quasi‐Five‐Day Wave in the Top Layer of Venus Clouds"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298337126864640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"In-orbit recalibration of Longwave Infrared Camera onboard Akatsuki"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298757420973312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Modeling a point-spread function originating from multiple reflection of light in the substrate of array sensor: the case of Akatsuki/IR2"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565475682810752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Automated cloud tracking system for the Akatsuki Venus Climate Orbiter data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182137852288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dawn-dusk difference of periodic oxygen EUV dayglow variations at Venus observed by Hisaki"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182137880448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamical relationship between wind speed magnitude and meridional temperature contrast: Application to an interannual oscillation in Venusian middle atmosphere GCM"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183242856960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Long‐term variation in the cloud‐tracked zonal velocities at the cloud top of Venus deduced from Venus Express VMC images"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183246094848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Local Time Dependence of the Thermal Structure in the Venusian Equatorial Upper Atmosphere: Comparison of Akatsuki Radio Occultation Measurements and GCM Results"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183424826368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stationary waves and slowly moving features in the night upper clouds of Venus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360571647804880640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"New cloud morphologies discovered on the Venus's night during Akatsuki"}]},{"@id":"https://cir.nii.ac.jp/crid/1360571647804888832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A Long‐Lived Sharp Disruption on the Lower Clouds of Venus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360571647804901120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Brightness modulations of our nearest terrestrial planet Venus reveal atmospheric super-rotation rather than surface features"}]},{"@id":"https://cir.nii.ac.jp/crid/1360571968061637504","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Improved automatic estimation of winds at the cloud top of Venus using superposition of cross-correlation surfaces"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092883395968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Long-term variations of the UV contrast on Venus observed by the Venus Monitoring Camera on board Venus Express"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092890300160","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The abundance and vertical distribution of the unknown ultraviolet absorber in the venusian atmosphere from analysis of Venus Monitoring Camera images"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092893590144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"UV contrasts and microphysical properties of the upper clouds of Venus from the UV and NIR VMC/VEx images"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118685528960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Instrumental requirements for the study of Venus’ cloud top using the UV imaging spectrometer VeSUV"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846639281846912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Three‐Dimensional Structures of Thermal Tides Simulated by a Venus GCM"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846950521110784","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Longwave Infrared Camera onboard the Venus Climate Orbiter"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848664602243456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Scattering Properties of the Venusian Clouds Observed by the UV Imager on board Akatsuki"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853122781591552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Venus night-side photometry with “cleaned” Akatsuki/IR2 data: Aerosol properties and variations of carbon monoxide"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853122781603456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Investigation of UV Absorbers on Venus Using the 283 and 365 nm Phase Curves Obtained From Akatsuki"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853122781614336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The nightside cloud-top circulation of the atmosphere of Venus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567861077888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Horizontal structure of planetary-scale waves at the cloud top of Venus deduced from Galileo SSI images with an improved cloud-tracking technique"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567867140864","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Variable winds on Venus mapped in three dimensions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567867854848","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Venus Monitoring Camera for Venus Express"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567871152000","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Structure of the Venus neutral atmosphere as observed by the Radio Science experiment VeRa on Venus Express"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861286472294016","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Correlation of Venusian Mesoscale Cloud Morphology Between Images Acquired at Various Wavelengths"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861286474898560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Amateur Observers Witness the Return of Venus’ Cloud Discontinuity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861286474909824","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Twelve-Year Cycle in the Cloud Top Winds Derived from VMC/Venus Express and UVI/Akatsuki Imaging"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861286475019904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reflectivity of Venus’s Dayside Disk During the 2020 Observation Campaign: Outcomes and Future Perspectives"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861286530600320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Venus cloud discontinuity in 2022"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861289677184768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The first assimilation of Akatsuki single-layer winds and its validation with Venusian atmospheric waves excited by solar heating"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412893055899392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Formation of the Y Feature at the Venusian Cloud Top by Planetary‐Scale Waves and the Mean Circulation: Analysis of Venus Express VMC Images"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412893056531456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Constraints on Venus Lightning From Akatsuki's First 3 Years in Orbit"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412893477716736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Principal components of short-term variability in the ultraviolet albedo of Venus"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520966378496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The atmosphere of Venus"}]},{"@id":"https://cir.nii.ac.jp/crid/1361694366761317760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Solar-locked and geographical atmospheric structures inferred from a Venus general circulation model with radiative transfer"}]},{"@id":"https://cir.nii.ac.jp/crid/1361975843215420800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermal structure of the Venusian atmosphere from the sub-cloud region to the mesosphere as observed by radio occultation"}]},{"@id":"https://cir.nii.ac.jp/crid/1362539019285093888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Long-term Variations of Venus’s 365 nm Albedo Observed by Venus Express, Akatsuki, MESSENGER, and the Hubble Space Telescope"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368447522560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Detection of Sub-Micron Radiation from the Surface of Venus by Cassini/VIMS"}]},{"@id":"https://cir.nii.ac.jp/crid/1390024953937830016","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"小型月着陸実証機（SLIM）推進系の開発と運用"},{"@language":"en","@value":"The Development and Operation of Propulsion System for SLIM (Smart Lander for Investigating Moon)"}]},{"@id":"https://cir.nii.ac.jp/crid/1523388080069817344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Overview of Venus orbiter, Akatsuki"},{"@language":"ja-Kana","@value":"Overview of Venus orbiter Akatsuki"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942124908032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Initial products of Akatsuki 1-μm camera"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942192558592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Development and in-flight calibration of IR2 : 2-μm camera onboard Japan's Venus orbiter, Akatsuki"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417101622400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Venus looks different from day to night across wavelengths : morphology from Akatsuki multispectral images"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417161599360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Contrast sources for the infrared images taken by the Venus mission Akatsuki"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892138311424","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Radio occultation experiment of the Venus atmosphere and ionosphere with the Venus orbiter Akatsuki"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842031753600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ultraviolet imager on Venus orbiter Akatsuki and its initial results"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842042436864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Special issue “Akatsuki at Venus : the first year of scientific operation”"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996267021864320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Science requirements and description of the 1 μm camera onboard the Akatsuki Venus Orbiter"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996267021883392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"LIR : Longwave Infrared Camera onboard the Venus orbiter Akatsuki"}]},{"@id":"https://cir.nii.ac.jp/crid/2120307889360528000","@type":"OtherWorks","resourceType":"学術雑誌論文(journal article)","relationType":["isIdenticalTo"],"jpcoar:relatedTitle":[{"@language":"en","@value":"AKATSUKI returns to Venus"}]}],"dataSourceIdentifier":[{"@type":"NDL_SEARCH","@value":"oai:ndlsearch.ndl.go.jp:R100000039-I9976818"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0457-6"},{"@type":"KAKEN","@value":"PRODUCT-20822656"},{"@type":"KAKEN","@value":"PRODUCT-21307199"},{"@type":"KAKEN","@value":"PRODUCT-20486052"},{"@type":"KAKEN","@value":"PRODUCT-21165478"},{"@type":"KAKEN","@value":"PRODUCT-20860060"},{"@type":"OPENAIRE","@value":"doi_dedup___::ca8a208411e321a04cc9607359dc486c"},{"@type":"IRDB","@value":"oai:irdb.nii.ac.jp:01332:0004476905_isIdenticalTo_DOI_OJ66U6w6YoUTeJMPILz4g3VaJUI"},{"@type":"CROSSREF","@value":"10.1002/2017gl075792_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0727-y_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1029/2018je005842_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1038/ngeo3016_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1186/s40623-018-0916-3_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1029/2019je006065_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1126/science.aaz4439_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2016.06.011_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1029/2019je006192_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1029/2020je006808_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1051/0004-6361/202040193_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1029/2021je006912_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1029/2023je007852_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2025.116523_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1093/mnras/stae1929_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0772-6_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1186/s40623-018-0789-5_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0451-z_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0736-x_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0749-5_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0773-5_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1029/2018je005627_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1038/ngeo2873_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1007/s11214-020-00703-9_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2022.114936_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1007/s11214-021-00797-9_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.3390/atmos13020182_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1029/2022je007596_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1186/s40623-023-01803-w_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1117/12.2638444_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1029/2018je005640_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1038/s41467-018-07919-y_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1038/s41550-017-0187_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0775-3_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2017.10.012_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2019.05.026_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1029/2020gl087221_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1038/s41467-020-19385-6_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1016/j.asr.2021.03.012_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1002/2017je005449_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0722-3_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.3847/1538-3881/aa78a5_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2020.114134_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1029/2020gl090577_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1038/s41586-021-03636-7_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1029/2022je007228_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.3390/atmos13020348_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.3390/atmos13122023_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.3847/psj/ac84d1_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1029/2022gl101633_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1051/0004-6361/202244822_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1038/s41598-022-18634-6_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.2322/astj.24.s80_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1029/2018je005779_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1029/2019gl083311_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1051/0004-6361/201935388_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2016.12.027_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2018.11.015_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.1038/s41598-020-59278-8_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"},{"@type":"CROSSREF","@value":"10.3847/1538-3881/ab3120_references_DOI_1NeJSIXta9d5uImYVcpRXyj4aHu"}]}