{"@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/1360017289672017664.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2017gl075615"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2017GL075615"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL075615"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2017GL075615"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL075615"}}],"dc:title":[{"@value":"Typhoon‐Induced Ground Deformation"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Geodetic instruments now offer compelling sensitivity, allowing to investigate how solid Earth and surface processes interact. By combining surface air pressure data, nontidal sea level variations model, and rainfall data, we systematically analyze the volumetric deformation of the shallow crust at seven borehole strainmeters in Taiwan induced by 31 tropical cyclones (typhoons) that made landfall to the island from 2004 to 2013. The typhoon's signature consists in a ground dilatation due to air pressure drop, generally followed by a larger ground compression. We show that this compression phase can be mostly explained by the mass loading of rainwater that falls on the ground and concentrates in the valleys towards the strainmeter sensitivity zone. Further, our analysis shows that borehole strainmeters can help quantifying the amount of rainwater accumulating and flowing over a watershed during heavy rainfalls, which is a useful constraint for building hydrological models.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380017280670926344","@type":"Researcher","foaf:name":[{"@value":"M. Mouyen"}],"jpcoar:affiliationName":[{"@value":"Géosciences Rennes, UMR 6118, OSUR, CNRS, Université Rennes 1  Rennes France"}]},{"@id":"https://cir.nii.ac.jp/crid/1380017289672017794","@type":"Researcher","foaf:name":[{"@value":"A. Canitano"}],"jpcoar:affiliationName":[{"@value":"Institute of Earth Sciences Academia Sinica  Taipei Taiwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380017289672017797","@type":"Researcher","foaf:name":[{"@value":"B. F. Chao"}],"jpcoar:affiliationName":[{"@value":"Institute of Earth Sciences Academia Sinica  Taipei Taiwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380017289672017792","@type":"Researcher","foaf:name":[{"@value":"Y.‐J. Hsu"}],"jpcoar:affiliationName":[{"@value":"Institute of Earth Sciences Academia Sinica  Taipei Taiwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380017289672017793","@type":"Researcher","foaf:name":[{"@value":"P. Steer"}],"jpcoar:affiliationName":[{"@value":"Géosciences Rennes, UMR 6118, OSUR, CNRS, Université Rennes 1  Rennes France"}]},{"@id":"https://cir.nii.ac.jp/crid/1380017289672017796","@type":"Researcher","foaf:name":[{"@value":"L. Longuevergne"}],"jpcoar:affiliationName":[{"@value":"Géosciences Rennes, UMR 6118, OSUR, CNRS, Université Rennes 1  Rennes France"}]},{"@id":"https://cir.nii.ac.jp/crid/1380017289672017664","@type":"Researcher","foaf:name":[{"@value":"J.‐P. Boy"}],"jpcoar:affiliationName":[{"@value":"EOST‐IPGS, UMR 7516 CNRS‐Université de Strasbourg  Strasbourg France"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2017-11-14","prism:volume":"44","prism:number":"21"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2017GL075615"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL075615"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2017GL075615"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL075615"}],"createdAt":"2017-11-02","modifiedAt":"2023-09-05","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/2050588892108500864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of vertical nonlinearity on the superconducting gravimeter CT #036 at Ishigakijima, Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/2017gl075615"},{"@type":"CROSSREF","@value":"10.1186/s40623-022-01609-2_references_DOI_L4QimPo8vgX4RU1jc1Az8Yq29zY"}]}