{"@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/1363670319765235584.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2016gl070078"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016GL070078"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016GL070078"}}],"dc:title":[{"@value":"Single‐station monitoring of volcanoes using seismic ambient noise"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Seismic ambient noise cross correlation is increasingly used to monitor volcanic activity. However, this method is usually limited to volcanoes equipped with large and dense networks of broadband stations. The single‐station approach may provide a powerful and reliable alternative to the classical “cross‐station” approach when measuring variation of seismic velocities. We implemented it on the Piton de la Fournaise in Reunion Island, a very active volcano with a remarkable multidisciplinary continuous monitoring. Over the past decade, this volcano has been increasingly studied using the traditional cross‐correlation technique and therefore represents a unique laboratory to validate our approach. Our results, tested on stations located up to 3.5 km from the eruptive site, performed as well as the classical approach to detect the volcanic eruption in the 1–2 Hz frequency band. This opens new perspectives to successfully forecast volcanic activity at volcanoes equipped with a single three‐component seismometer.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670319765235458","@type":"Researcher","foaf:name":[{"@value":"Raphael S. M. De Plaen"}],"jpcoar:affiliationName":[{"@value":"Faculté des Sciences, de la Technologie et de la Communication University of Luxembourg  Luxembourg Luxembourg"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319765235456","@type":"Researcher","foaf:name":[{"@value":"Thomas Lecocq"}],"jpcoar:affiliationName":[{"@value":"Royal Observatory of Belgium  Uccle Belgium"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319765235585","@type":"Researcher","foaf:name":[{"@value":"Corentin Caudron"}],"jpcoar:affiliationName":[{"@value":"Department of Earth Sciences University of Cambridge  Cambridge UK"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319765235584","@type":"Researcher","foaf:name":[{"@value":"Valérie Ferrazzini"}],"jpcoar:affiliationName":[{"@value":"Observatoire Volcanologique du Piton de la Fournaise, Institut de Physique du Globe de Paris, Sorbonne Paris Cité Paris VII ‐ Denis Diderot University, CNRS  Réunion France"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319765235457","@type":"Researcher","foaf:name":[{"@value":"Olivier Francis"}],"jpcoar:affiliationName":[{"@value":"Faculté des Sciences, de la Technologie et de la Communication University of Luxembourg  Luxembourg Luxembourg"}]}],"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":"2016-08-28","prism:volume":"43","prism:number":"16","prism:startingPage":"8511","prism:endingPage":"8518"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016GL070078"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016GL070078"}],"createdAt":"2016-08-11","modifiedAt":"2023-09-16","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050565162986618752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Shallow volcanic reservoirs and pathways beneath Aso caldera revealed using ambient seismic noise tomography"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183245511936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Complex Near‐Surface Rheology Inferred From the Response of Greater Tokyo to Strong Ground Motions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584340520684672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-resolution spatial elastic wave velocity variation detected using multiple-linear-array microtremor measurements"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707120218624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Nonlinear Earthquake Response of Marine Sediments With Distributed Acoustic Sensing"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/2016gl070078"},{"@type":"CROSSREF","@value":"10.1186/s40623-018-0941-2_references_DOI_4VTXm2eKqOcxxJGOpeCZdQCZWBW"},{"@type":"CROSSREF","@value":"10.1029/2018jb015697_references_DOI_4VTXm2eKqOcxxJGOpeCZdQCZWBW"},{"@type":"CROSSREF","@value":"10.1080/08123985.2024.2323473_references_DOI_4VTXm2eKqOcxxJGOpeCZdQCZWBW"},{"@type":"CROSSREF","@value":"10.1029/2022gl100122_references_DOI_4VTXm2eKqOcxxJGOpeCZdQCZWBW"}]}