{"@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/1390001205222346112.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2151/sola.6a-004"}},{"identifier":{"@type":"URI","@value":"http://www.jstage.jst.go.jp/article/sola/6A/SpecialEdition/6A_SpecialEdition_13/_pdf"}},{"identifier":{"@type":"NAID","@value":"130004448528"}}],"dc:title":[{"@language":"en","@value":"Impact of Wave-Ocean Interaction on Typhoon Hai-Tang in 2005"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"We investigated the impact of wave-ocean interaction on numerical predictions for Typhoon Hai-Tang in 2005 using a nonhydrostatic atmosphere model coupled with a third-generation ocean wave model and a mixed-layer ocean model. Here we address the effect of breaking surface waves on entrainment induced at the mixed-layer base, assuming that the turbulent transport due to breaking surface waves is expressed as a function of both wave-induced and surface wind stresses. The introduction of breaking surface waves into the coupled model enables us to reproduce the evolution of Hai-Tang's central pressure and sea-surface temperature (SST) distribution more realistically. SST decreases significantly (rarely) along Hai-Tang's track where the mixed-layer depth is relatively shallow (deep). Hai-Tang tends to intensify where the initial mixed layer is relatively deep along Hai-Tang's track. Introducing the wave-ocean interaction may lead to more precise tropical cyclone intensity prediction through more realistic reproduction of the SST distribution."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420564276160601216","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"20354475"},{"@type":"NRID","@value":"1000020354475"},{"@type":"CINII_AUTHOR_ID","@value":"DA18490340"},{"@type":"URI","@value":"https://ci.nii.ac.jp/author/DA18490340#entity"},{"@type":"URI","@value":"https://viaf.org/viaf/NII%7CDA18490340"},{"@type":"NRID","@value":"9000001423497"},{"@type":"NRID","@value":"9000363486421"},{"@type":"NRID","@value":"9000402818771"},{"@type":"NRID","@value":"9000001026251"},{"@type":"NRID","@value":"9000253191152"},{"@type":"NRID","@value":"9000409504836"},{"@type":"NRID","@value":"9000301746333"},{"@type":"NRID","@value":"9000399261804"},{"@type":"NRID","@value":"9000415409155"},{"@type":"NRID","@value":"9000391637149"},{"@type":"NRID","@value":"9000356661487"},{"@type":"NRID","@value":"9000409895918"},{"@type":"NRID","@value":"9000241203935"},{"@type":"NRID","@value":"9000257827841"},{"@type":"NRID","@value":"9000410889306"},{"@type":"NRID","@value":"9000379602814"},{"@type":"NRID","@value":"9000324997413"},{"@type":"NRID","@value":"9000315141630"},{"@type":"NRID","@value":"9000414745635"},{"@type":"NRID","@value":"9000398988828"},{"@type":"NRID","@value":"9000257979045"},{"@type":"NRID","@value":"9000257978984"},{"@type":"NRID","@value":"9000404156868"},{"@type":"NRID","@value":"9000411827868"},{"@type":"NRID","@value":"9000008080117"},{"@type":"NRID","@value":"9000414742080"},{"@type":"NRID","@value":"9000404149326"},{"@type":"NRID","@value":"9000356661375"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/Typhoon"}],"foaf:name":[{"@language":"en","@value":"Wada Akiyoshi"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research Institute"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001205222346112","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000257827842"}],"foaf:name":[{"@language":"en","@value":"Kohno Nadao"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Japan Meteorological Agency"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001205222346113","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000257827843"}],"foaf:name":[{"@language":"en","@value":"Kawai Yoshimi"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Japan Agency for Marine-Earth Science and Technology"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"13496476"}],"prism:publicationName":[{"@language":"en","@value":"SOLA"},{"@language":"en","@value":"SOLA"}],"dc:publisher":[{"@language":"en","@value":"Meteorological Society of Japan"},{"@language":"ja","@value":"公益社団法人 日本気象学会"}],"prism:publicationDate":"2010","prism:volume":"6A","prism:number":"SpecialEdition","prism:startingPage":"13","prism:endingPage":"16"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://www.jstage.jst.go.jp/article/sola/6A/SpecialEdition/6A_SpecialEdition_13/_pdf"}],"availableAt":"2010","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002214351569792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The role of ocean‐atmosphere interaction in <scp>T</scp>yphoon <scp>S</scp>inlaku (2008) using a regional coupled data assimilation system"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004236560264704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Relationship between Convective Bursts and Warm-Core Intensification in a Nonhydrostatic Simulation of Typhoon 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