{"@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/1360004233288208256.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2011gl048717"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011GL048717"}},{"identifier":{"@type":"URI","@value":"http://www.agu.org/journals/gl/gl1118/2011GL048717/2011GL048717.pdf"}},{"identifier":{"@type":"NAID","@value":"20000705690"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Responses of marine ecosystem to typhoon passages in the western subtropical North Pacific"}],"dcterms:alternative":[{"@value":"MARINE ECOSYSTEM TO TYPHOON"}],"description":[{"notation":[{"@value":"[1] Strong phytoplankton blooms are occasionally observed around a recurvature point of typhoon tracks in the western subtropical Pacific. These are noteworthy events in subtropical regions where both nutrient concentrations and biological production are persistently low. We investigated the response of phytoplankton to typhoon passage using a numerical model with/without biogeochemical processes. The model reproduced the observed patch-like phytoplankton bloom around a recurvature point of Typhoon Keith in 1997. The strong bloom is caused by the typhoon-centered upwelling of nutrient-rich water from below the euphotic layer, which supplies the nutrients required for phytoplankton growth, resulting in higher chlorophyll-a concentrations. Biogeochemical processes then play essential roles in determining the response after the passage of typhoons in subtropical regions."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004233288208388","@type":"Researcher","foaf:name":[{"@value":"Ryota Shibano"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Environmental Science; Hokkaido University; Sapporo; Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233288208396","@type":"Researcher","foaf:name":[{"@value":"Yasuhiro Yamanaka"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Environmental Science; Hokkaido University; Sapporo; Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233288208256","@type":"Researcher","foaf:name":[{"@value":"Naosuke Okada"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Environmental Science; Hokkaido University; Sapporo; Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233288208264","@type":"Researcher","foaf:name":[{"@value":"Takashi Chuda"}],"jpcoar:affiliationName":[{"@value":"Atmosphere and Ocean Research Institute; University of Tokyo; Kashiwa; Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233288208257","@type":"Researcher","foaf:name":[{"@value":"Shin-ichi Suzuki"}],"jpcoar:affiliationName":[{"@value":"National Research Institute for Earth Science and Disaster Prevention; Tsukuba; Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801202554496","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"90272525"},{"@type":"NRID","@value":"1000090272525"},{"@type":"NRID","@value":"9000363494293"},{"@type":"NRID","@value":"9000397426027"},{"@type":"NRID","@value":"9000257828064"},{"@type":"NRID","@value":"9000363496154"},{"@type":"NRID","@value":"9000415410383"},{"@type":"NRID","@value":"9000415415109"},{"@type":"NRID","@value":"9000362199953"},{"@type":"NRID","@value":"9000283593782"},{"@type":"NRID","@value":"9000283593388"},{"@type":"NRID","@value":"9000363489600"},{"@type":"NRID","@value":"9000363490119"},{"@type":"NRID","@value":"9000363493976"},{"@type":"NRID","@value":"9000363492671"},{"@type":"NRID","@value":"9000363493869"},{"@type":"NRID","@value":"9000363490831"}],"foaf:name":[{"@value":"Hiroshi Niino"}],"jpcoar:affiliationName":[{"@value":"Atmosphere and Ocean Research Institute; University of Tokyo; Kashiwa; Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233288208387","@type":"Researcher","foaf:name":[{"@value":"Mitsuhiro Toratani"}],"jpcoar:affiliationName":[{"@value":"School of High-Technology for Human Welfare; Tokai University; Numazu; Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2011-09-28","prism:volume":"38","prism:number":"18","prism:startingPage":"n/a","prism:endingPage":"n/a"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://doi.wiley.com/10.1002/tdm_license_1.1"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011GL048717"},{"@id":"http://www.agu.org/journals/gl/gl1118/2011GL048717/2011GL048717.pdf"}],"createdAt":"2011-08-19","modifiedAt":"2021-07-21","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782070200448","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"21340134"},{"@type":"JGN","@value":"JP21340134"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-21340134/"}],"notation":[{"@language":"ja","@value":"大気境界層の激しい渦の発生機構・構造・力学及び乱流輸送に果たす役割の解明"},{"@language":"en","@value":"Generation Mechanism, Structure and Dynamics of Violent Vortices in the Atmospheric Boundary layer and their Roles in Turbulent Transport"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001338209104384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Impact of cyclonic eddies and typhoons on biogeochemistry in the oligotrophic ocean based on biogeochemical/physical/meteorological time-series at station KEO"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144834709632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Satellite observation of chlorophyll and nutrients increase induced by Typhoon Megi in the Japan/East Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283692410411776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The mechanism of upper-oceanic vertical motions forced by a moving typhoon"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617915184384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An Improved Mellor–Yamada Level-3 Model: Its Numerical Stability and Application to a Regional Prediction of Advection Fog"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620317353472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Short-term changes in chlorophyll distribution in response to a moving storm: a modelling study"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179760547200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Contributions of physical and biogeochemical processes to phytoplankton biomass enhancement in the surface and subsurface layers during the passage of Typhoon Damrey"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181335533568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Comparison of carbon cycle between the western Pacific subarctic and subtropical time-series stations: highlights of the K2S1 project"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094108169856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"New evidence for enhanced ocean primary production triggered by tropical cyclone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570696150272","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"NEMURO—a lower trophic level model for the North Pacific marine ecosystem"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045070938624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sea surface cooling caused by typhoons in the Tohoku area in August 1989"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419981282304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Satellite observations of sea surface cooling by hurricanes"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420963446016","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Upper Ocean Response to a Hurricane"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544421275627392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Upper-Ocean Thermal Structure and the Western North Pacific Category 5 Typhoons. 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Interactions between Boundary Layers and the Free Atmosphere(Vertical Interaction in Various Interface Regions of the Atmosphere (A Report on the Symposium of the 2010 Fall Assembly of the Meteorological Society of Japan))"}]},{"@id":"https://cir.nii.ac.jp/crid/1521417755658780544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fifty years of the 137°E repeat hydrographic section in the western North Pacific Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892096588672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Scalability of future climate changes across Japan examined with large-ensemble simulations at +1.5K, +2K, and +4K global warming levels"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2011gl048717"},{"@type":"CIA","@value":"20000705690"},{"@type":"KAKEN","@value":"PRODUCT-12656180"},{"@type":"OPENAIRE","@value":"doi_dedup___::b888333969781669c6fdbb0a63dc12e4"},{"@type":"CROSSREF","@value":"10.1007/s10872-017-0461-x_references_DOI_8hAmCchrKnNVChxvNMl3MfH98ij"},{"@type":"CROSSREF","@value":"10.1002/2016jg003331_references_DOI_8hAmCchrKnNVChxvNMl3MfH98ij"},{"@type":"CROSSREF","@value":"10.1007/s10872-017-0423-3_references_DOI_8hAmCchrKnNVChxvNMl3MfH98ij"},{"@type":"CROSSREF","@value":"10.5928/kaiyou.25.2_17_references_DOI_8hAmCchrKnNVChxvNMl3MfH98ij"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0196-3_references_DOI_8hAmCchrKnNVChxvNMl3MfH98ij"}]}