{"@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/1363388844493107712.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2017gl073000"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2017GL073000"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL073000"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2017GL073000"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL073000"}}],"dc:title":[{"@value":"Calibrating the amplitude source location (ASL) method by using active seismic sources: An example from Te Maari volcano, Tongariro National Park, New Zealand"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>A frequently applied amplitude source location (ASL) method is here calibrated and optimized by using active seismic sources located at the surface of a dry stream channel. The ASL produced location discrepancies larger than 1.0 km laterally and 500 m in depth by using independently determined velocity model, attenuation, and site amplification factors (AFs). Sensitivity tests for ASL input parameters show that attenuation and velocity have moderate influence on the location but are easy to independently constrain. AFs are shown to strongly influence the location, and their application may introduce substantial location uncertainties. Model uncertainties are accommodated with either lateral or depth changes depending on the input parameters, station corrections, and the source‐station geometry.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380013168876420741","@type":"Researcher","foaf:name":[{"@value":"B. Walsh"}],"jpcoar:affiliationName":[{"@value":"Volcanic Risk Solutions, Institute of Agriculture and Environment Massey University  Palmerston North Manawatu New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844493107713","@type":"Researcher","foaf:name":[{"@value":"A. D. Jolly"}],"jpcoar:affiliationName":[{"@value":"GNS Science  Lower Hutt Wellington New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844493107714","@type":"Researcher","foaf:name":[{"@value":"J. Procter"}],"jpcoar:affiliationName":[{"@value":"Volcanic Risk Solutions, Institute of Agriculture and Environment Massey University  Palmerston North Manawatu New Zealand"}]}],"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":"2017-04-24","prism:volume":"44","prism:number":"8","prism:startingPage":"3591","prism:endingPage":"3599"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2017GL073000"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL073000"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2017GL073000"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL073000"}],"createdAt":"2017-04-17","modifiedAt":"2023-08-30","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360588379390342272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Complex principal component analysis of volcanic earthquakes at Azuma volcano, Japan, recorded by a distributed acoustic sensing system (DAS) for the hypocenter determination"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869854369203840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Magmatic processes associated with the 2020 eruption of Taal Volcano, Philippines, revealed by local seismic source estimates"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131418080256384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Amplitude Source Location Method With Depth‐Dependent Scattering and Attenuation Structures: Application at Nevado del Ruiz Volcano, Colombia"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842055369344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimation of relative source locations from seismic amplitude : application to earthquakes and tremors at Meakandake volcano, eastern Hokkaido, Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/2017gl073000"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01366-8_references_DOI_ZKAjtcHUs2TcOSb9xQZTZovTqyF"},{"@type":"CROSSREF","@value":"10.1016/j.jvolgeores.2025.108343_references_DOI_ZKAjtcHUs2TcOSb9xQZTZovTqyF"},{"@type":"CROSSREF","@value":"10.1016/j.jvolgeores.2024.108256_references_DOI_ZKAjtcHUs2TcOSb9xQZTZovTqyF"},{"@type":"CROSSREF","@value":"10.1029/2019jb018156_references_DOI_ZKAjtcHUs2TcOSb9xQZTZovTqyF"}]}