{"@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/1363951794885238528.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2015ja022299"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2015JA022299"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015JA022299"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2015JA022299"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2015JA022299"}}],"dc:title":[{"@value":"Middle‐ and low‐latitude ionosphere response to 2015 St. Patrick's Day geomagnetic storm"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>This paper presents a study of the St Patrick's Day storm of 2015, with its ionospheric response at middle and low latitudes. The effects of the storm in each longitudinal sector (Asian, African, American, and Pacific) are characterized using global and regional electron content. At the beginning of the storm, one or two ionospheric positive storm effects are observed depending on the longitudinal zones. After the main phase of the storm, a strong decrease in ionization is observed at all longitudes, lasting several days. The American region exhibits the most remarkable increase in vertical total electron content (vTEC), while in the Asian sector, the largest decrease in vTEC is observed. At low latitudes, using spectral analysis, we were able to separate the effects of the prompt penetration of the magnetospheric convection electric field (PPEF) and of the disturbance dynamo electric field (DDEF) on the basis of ground magnetic data. Concerning the PPEF, Earth's magnetic field oscillations occur simultaneously in the Asian, African, and American sectors, during southward magnetization of the <jats:italic>B<jats:sub>z</jats:sub></jats:italic> component of the interplanetary magnetic field. Concerning the DDEF, diurnal magnetic oscillations in the horizontal component H of the Earth's magnetic field exhibit a behavior that is opposed to the regular one. These diurnal oscillations are recognized to last several days in all longitudinal sectors. The observational data obtained by all sensors used in the present paper can be interpreted on the basis of existing theoretical models.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380853567424284807","@type":"Researcher","foaf:name":[{"@value":"B. Nava"}],"jpcoar:affiliationName":[{"@value":"T/ICT4D, The Abdus Salam International Centre for Theoretical Physics  Trieste Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1383951794885238534","@type":"Researcher","foaf:name":[{"@value":"J. Rodríguez‐Zuluaga"}],"jpcoar:affiliationName":[{"@value":"T/ICT4D, The Abdus Salam International Centre for Theoretical Physics  Trieste Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1383951794885238528","@type":"Researcher","foaf:name":[{"@value":"K. Alazo‐Cuartas"}],"jpcoar:affiliationName":[{"@value":"T/ICT4D, The Abdus Salam International Centre for Theoretical Physics  Trieste Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1383951794885238532","@type":"Researcher","foaf:name":[{"@value":"A. Kashcheyev"}],"jpcoar:affiliationName":[{"@value":"T/ICT4D, The Abdus Salam International Centre for Theoretical Physics  Trieste Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1383951794885238531","@type":"Researcher","foaf:name":[{"@value":"Y. Migoya‐Orué"}],"jpcoar:affiliationName":[{"@value":"T/ICT4D, The Abdus Salam International Centre for Theoretical Physics  Trieste Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1383951794885238535","@type":"Researcher","foaf:name":[{"@value":"S.M. Radicella"}],"jpcoar:affiliationName":[{"@value":"T/ICT4D, The Abdus Salam International Centre for Theoretical Physics  Trieste Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1383951794885238530","@type":"Researcher","foaf:name":[{"@value":"C. Amory‐Mazaudier"}],"jpcoar:affiliationName":[{"@value":"T/ICT4D, The Abdus Salam International Centre for Theoretical Physics  Trieste Italy"},{"@value":"Sorbonne Paris, UPMC University Paris VI, LPP  Paris France"}]},{"@id":"https://cir.nii.ac.jp/crid/1383951794885238533","@type":"Researcher","foaf:name":[{"@value":"R. Fleury"}],"jpcoar:affiliationName":[{"@value":"Lab‐STICC/UMR CNRS  Brest France"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"21699380"},{"@type":"EISSN","@value":"21699402"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Space Physics"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2016-04","prism:volume":"121","prism:number":"4","prism:startingPage":"3421","prism:endingPage":"3438"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2015JA022299"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015JA022299"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2015JA022299"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2015JA022299"}],"createdAt":"2016-03-12","modifiedAt":"2023-09-07","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050291768617207296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Assessing the performance of a Northeast Asia Japan-centered 3-D ionosphere specification technique during the 2015 St. Patrick’s day geomagnetic storm"}]},{"@id":"https://cir.nii.ac.jp/crid/1050293401217315200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Complementing regional ground GNSS-STEC computerized ionospheric tomography (CIT) with ionosonde data assimilation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229808155904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Equatorial and low‐latitude ionospheric response to the 17–18 March 2015 great storm over Southeast Asia longitude sector"}]},{"@id":"https://cir.nii.ac.jp/crid/1360286993149979392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Three Different Episodes of Prompt Equatorial Electric Field Perturbations Under Steady Southward IMF <i>Bz</i> During St. Patrick's Day Storm"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584339750694656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Responses of the African-European equatorial-, low-, mid-, and high-latitude ionosphere to geomagnetic storms of 2013, 2015 St Patrick’s Days, 1 June 2013, and 7 October 2015"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/2015ja022299"},{"@type":"CROSSREF","@value":"10.1002/2017ja024134_references_DOI_Hw1v6aGZm3QhRz5Imo0l9uVMBMK"},{"@type":"CROSSREF","@value":"10.1029/2019ja027069_references_DOI_Hw1v6aGZm3QhRz5Imo0l9uVMBMK"},{"@type":"CROSSREF","@value":"10.1016/j.asr.2022.10.029_references_DOI_Hw1v6aGZm3QhRz5Imo0l9uVMBMK"},{"@type":"CROSSREF","@value":"10.1007/s10291-021-01133-y_references_DOI_Hw1v6aGZm3QhRz5Imo0l9uVMBMK"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01447-8_references_DOI_Hw1v6aGZm3QhRz5Imo0l9uVMBMK"}]}