{"@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/1360004229808702336.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2017jc012695"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2017JC012695"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2017JC012695"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Preparing for the Future Nankai Trough Tsunami: A Data Assimilation and Inversion Analysis From Various Observational Systems"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>The future Nankai Trough tsunami is one of the imminent threats to the Japanese coastal communities that could potentially cause a catastrophic event. As a part of the countermeasure efforts for such an occurrence, this study analyzes the efficacy of combining tsunami data assimilation (DA) and waveform inversion (WI). The DA is used to continuously refine a wavefield model whereas the WI is used to estimate the tsunami source. We consider a future scenario of the Nankai Trough tsunami recorded at various observational systems, including ocean bottom pressure (OBP) gauges, global positioning system (GPS) buoys, and ship height positioning data. Since most of the OBP gauges are located inside the source region, the recorded tsunami signals exhibit significant offsets from surface measurements due to coseismic seafloor deformation effects. Such biased data are not applicable to the standard DA, but can be taken into account in the WI. On the other hand, the use of WI for the ship data may not be practical because a considerably large precomputed tsunami database is needed to cope with the spontaneous ship locations. The DA is more suitable for such an observational system as it can be executed sequentially in time and does not require precomputed scenarios. Therefore, the combined approach of DA and WI allows us to concurrently make use of all observational resources. Additionally, we introduce a bias correction scheme for the OBP data to improve the accuracy, and an adaptive thinning of observations to determine the efficient number of observations.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004229808702730","@type":"Researcher","foaf:name":[{"@value":"Iyan E. Mulia"}],"jpcoar:affiliationName":[{"@value":"UTokyo Ocean Alliance, University of Tokyo Tokyo Japan"},{"@value":"Now at Earthquake Research Institute University of Tokyo Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229808702344","@type":"Researcher","foaf:name":[{"@value":"Daisuke Inazu"}],"jpcoar:affiliationName":[{"@value":"Department of Marine Resources and Energy Tokyo University of Marine Science and Technology Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229808702720","@type":"Researcher","foaf:name":[{"@value":"Takuji Waseda"}],"jpcoar:affiliationName":[{"@value":"UTokyo Ocean Alliance, University of Tokyo Tokyo Japan"},{"@value":"Graduate School of Frontier Sciences University of Tokyo Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229808702472","@type":"Researcher","foaf:name":[{"@value":"Aditya Riadi Gusman"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute, University of Tokyo Tokyo 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":"2017-10","prism:volume":"122","prism:number":"10","prism:startingPage":"7924","prism:endingPage":"7937"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2017JC012695"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2017JC012695"}],"createdAt":"2017-09-14","modifiedAt":"2023-09-09","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781971057280","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"17K12998"},{"@type":"JGN","@value":"JP17K12998"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-17K12998/"}],"notation":[{"@language":"ja","@value":"東京湾における津波による流速・水深変化・船舶の避難域の決定"},{"@language":"en","@value":"Determination of potential tsunami-induced current velocity, bathymetric change, and vessel safe zone in Tokyo 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