{"@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/1360846639280896000.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2016jc012023"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016JC012023"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016JC012023"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Factors responsible for the limited inland extent of sand deposits on <scp>L</scp>eyte <scp>I</scp>sland during 2013 <scp>T</scp>yphoon <scp>H</scp>aiyan"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Previous geological studies suggest that the maximum inland extent of storm‐induced sand deposits is shorter, but their thickness is larger, than those of tsunami‐induced sand deposits. However, factors that determine the maximum extent and thickness of storm deposits are still uncertain. We conducted numerical simulations of storm surge, waves, and sediment transport during Typhoon Haiyan in order to understand the distribution and sedimentary processes responsible for storm deposits. Numerical results showed that wave‐induced currents slightly offshore were strong, but attenuated rapidly in the inland direction after wave breaking. Therefore, sediments were not transported far inland by waves and storm surge. Consequently, the maximum inland extent of storm deposits was remarkably shorter than the inland extent of inundation. We also revealed that vegetation (roughness coefficient) and typhoon intensity greatly affect the calculation of maximum extent and thickness distribution of storm deposits. As the duration of wave impact on a coast is relatively long during a storm (hours, compared to minutes for a tsunami), sediments are repeatedly supplied by multiple waves. Therefore, storm deposits tend to be thicker than tsunami deposits, and multiple layers can form in the internal sedimentary structure of the deposits. We infer that limitation of the sand deposit to within only a short distance inland from the shoreline and multiple layers found in a deposit can be used as appropriate identification proxies for storm deposits.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380846639280896000","@type":"Researcher","foaf:name":[{"@value":"M. Watanabe"}],"jpcoar:affiliationName":[{"@value":"School of Engineering Tohoku University Sendai Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847867399198594","@type":"Researcher","foaf:name":[{"@value":"J. D. Bricker"}],"jpcoar:affiliationName":[{"@value":"International Research Institute of Disaster Science, Tohoku University Sendai Japan"},{"@value":"Department of Hydraulic Engineering, Faculty of Civil Engineering and Geosciences Delft University of Technology Delft Netherlands"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847867399198592","@type":"Researcher","foaf:name":[{"@value":"K. Goto"}],"jpcoar:affiliationName":[{"@value":"International Research Institute of Disaster Science, Tohoku University Sendai Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847867399198593","@type":"Researcher","foaf:name":[{"@value":"F. Imamura"}],"jpcoar:affiliationName":[{"@value":"International Research Institute of Disaster Science, Tohoku University Sendai Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"21699275"},{"@type":"EISSN","@value":"21699291"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Oceans"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2017-04","prism:volume":"122","prism:number":"4","prism:startingPage":"2795","prism:endingPage":"2812"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016JC012023"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016JC012023"}],"createdAt":"2017-03-02","modifiedAt":"2023-09-09","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=550","dc:title":"550"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781904356864","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16J01953"},{"@type":"JGN","@value":"JP16J01953"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-16J01953/"}],"notation":[{"@language":"ja","@value":"地質学と津波工学の融合による津波堆積物認定手法の高度化"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002214348980352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Local amplification of storm surge by Super Typhoon Haiyan in Leyte Gulf"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002218336398848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Track analysis, simulation, and field survey of the 2013 Typhoon Haiyan storm surge"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229804594304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Combined infragravity wave and sea‐swell runup over fringing reefs by super typhoon Haiyan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232169494912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Coastal geomorphic conditions and styles of storm surge washover deposits from Southern Thailand"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232523511680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Source of high tsunamis along the southernmost Ryukyu trench inferred from tsunami stratigraphy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145138426368","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Physical criteria for distinguishing sandy tsunami and storm deposits using modern examples"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146617460864","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tracking hurricane-generated storm surge with washover fan stratigraphy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691040755584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Historical tsunami and storm deposits during the last five centuries on the Sanriku coast, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707168503168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Storm surge mapping of typhoon Haiyan and its impact in Tanauan, Leyte, Philippines"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707474875520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunami history over the past 2000 years on the Sanriku coast, Japan, determined using gravel deposits to estimate tsunami inundation behavior"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619739169024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sediment transport due to the 2011 Tohoku-oki tsunami at Sendai: Results from numerical modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619797338752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Contrasting styles of Hurricane Irene washover sedimentation on three east coast barrier islands: Cape Lookout, North Carolina; 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parameters"}]},{"@id":"https://cir.nii.ac.jp/crid/1390570176043963520","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Progress in tsunami sedimentology"},{"@language":"ja","@value":"津波堆積学の進展"},{"@language":"ja-Kana","@value":"ツナミ タイセキガク ノ シンテン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390860332468666112","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tsunami Deposit and Environmental Change Associated with the 1498 Meio Earthquake Recorded at Yonezu Pond, Hamamatsu City, Japan"},{"@language":"ja","@value":"静岡県浜松市の米津池跡で見られる1498年明応地震に伴う津波堆積物と環境変化"},{"@language":"ja-Kana","@value":"シズオカケン ハママツシ ノ ベイ ツチ アト デ ミラレル 1498ネンメイオウジシン ニ トモナウ ツナミ タイセキブツ ト カンキョウ ヘンカ"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266960772736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleo-tsunami history along the northern 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