{"@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/1361137043729235840.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2015ja021217"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2015JA021217"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015JA021217"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2015JA021217"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2015JA021217"}}],"dc:title":[{"@value":"Substorm evolution of auroral structures"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Auroral arcs are often associated with magnetically quiet time and substorm growth phases. We have studied the evolution of auroral structures during global and local magnetic activity to investigate the occurrence rate of auroral arcs during different levels of magnetic activity. The ground‐magnetic and auroral conditions are described by the magnetometer and auroral camera data from five Magnetometers — Ionospheric radars — All‐sky cameras Large Experiment stations in Finnish and Swedish Lapland. We identified substorm growth, expansion, and recovery phases from the local electrojet index (<jats:italic>I</jats:italic><jats:italic>L</jats:italic>) in 1996–2007 and analyzed the auroral structures during the different phases. Auroral structures were also analyzed during different global magnetic activity levels, as described by the planetary <jats:italic>K</jats:italic><jats:italic>p</jats:italic> index. The distribution of auroral structures for all substorm phases and <jats:italic>K</jats:italic><jats:italic>p</jats:italic> levels is of similar shape. About one third of all detected structures are auroral arcs. This suggests that auroral arcs occur in all conditions as the main element of the aurora. The most arc‐dominated substorm phases occur in the premidnight sector, while the least arc‐dominated substorm phases take place in the dawn sector. Arc event lifetimes and expectation times calculated for different substorm phases show that the longest arc‐dominated periods are found during growth phases, while the longest arc waiting times occur during expansion phases. Most of the arc events end when arcs evolve to more complex structures. This is true for all substorm phases. Based on the number of images of auroral arcs and the durations of substorm phases, we conclude that a randomly selected auroral arc most likely belongs to a substorm expansion phase. A small time delay, of the order of a minute, is observed between the magnetic signature of the substorm onset (i.e., the beginning of the negative bay) and the auroral breakup (i.e., the growth phase arc changing into a dynamic display). The magnetic onset was observed to precede the structural change in the auroral display. A longer delay of a few minutes was found between the beginning of the growth phase and the first detected auroral structure.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380285711829727620","@type":"Researcher","foaf:name":[{"@value":"N. Partamies"}],"jpcoar:affiliationName":[{"@value":"Arctic Research Finnish Meteorological Institute  Helsinki Finland"},{"@value":"Department of Geophysics The University Centre in Svalbard  Longyearbyen Norway"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043729235840","@type":"Researcher","foaf:name":[{"@value":"L. Juusola"}],"jpcoar:affiliationName":[{"@value":"Arctic Research Finnish Meteorological Institute  Helsinki Finland"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043729235842","@type":"Researcher","foaf:name":[{"@value":"D. Whiter"}],"jpcoar:affiliationName":[{"@value":"Arctic Research Finnish Meteorological Institute  Helsinki Finland"},{"@value":"Department of Physics and Astronomy University of Southampton  Southampton UK"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043729235843","@type":"Researcher","foaf:name":[{"@value":"K. Kauristie"}],"jpcoar:affiliationName":[{"@value":"Arctic Research Finnish Meteorological Institute  Helsinki Finland"}]}],"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":"2015-07","prism:volume":"120","prism:number":"7","prism:startingPage":"5958","prism:endingPage":"5972"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2015JA021217"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015JA021217"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2015JA021217"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2015JA021217"}],"createdAt":"2015-06-25","modifiedAt":"2023-09-01","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001338207801472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Simultaneous observation of auroral substorm onset in Polar satellite global images and ground-based all-sky images"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229806250240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Energetic electron precipitation and auroral morphology at the substorm recovery phase"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704784848512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Occurrence and average behavior of pulsating aurora"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580229812901376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"An automated auroral detection system using deep learning: real-time operation in Tromsø, Norway"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842098768640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Eastward-expanding auroral surges observed in the post-midnight sector during a multiple-onset substorm"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/2015ja021217"},{"@type":"CROSSREF","@value":"10.1002/2016ja023484_references_DOI_WcZu6pOsF8jP6oyOadUZDDqVZRS"},{"@type":"CROSSREF","@value":"10.1002/2017ja024039_references_DOI_WcZu6pOsF8jP6oyOadUZDDqVZRS"},{"@type":"CROSSREF","@value":"10.1186/s40623-018-0843-3_references_DOI_DxYjrFJd3TC2A7NV1T0TPRsiL1H"},{"@type":"CROSSREF","@value":"10.1038/s41598-022-11686-8_references_DOI_WcZu6pOsF8jP6oyOadUZDDqVZRS"},{"@type":"CROSSREF","@value":"10.1186/s40623-015-0350-8_references_DOI_WcZu6pOsF8jP6oyOadUZDDqVZRS"}]}