{"@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/1361137045755636096.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2015gl065523"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2015GL065523"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015GL065523"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2015GL065523"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2015GL065523"}}],"dc:title":[{"@value":"Substorm‐induced energetic electron precipitation: Impact on atmospheric chemistry"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Magnetospheric substorms drive energetic electron precipitation into the Earth's atmosphere. We use the output from a substorm model to describe electron precipitation forcing of the atmosphere during an active substorm period in April–May 2007. We provide the first estimate of substorm impact on the neutral composition of the polar middle atmosphere. Model simulations show that the enhanced ionization from a series of substorms leads to an estimated ozone loss of 5–50% in the mesospheric column depending on season. This is similar in scale to small to medium solar proton events (SPEs). This effect on polar ozone balance is potentially more important on long time scales (months to years) than the impulsive but sporadic (few SPE/year versus three to four substorms/day) effect of SPEs. Our results suggest that substorms should be considered an important source of energetic particle precipitation into the atmosphere and included in high‐top chemistry‐climate models.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137045755636097","@type":"Researcher","foaf:name":[{"@value":"A. Seppälä"}],"jpcoar:affiliationName":[{"@value":"Finnish Meteorological Institute  Helsinki Finland"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045755636098","@type":"Researcher","foaf:name":[{"@value":"M. A. Clilverd"}],"jpcoar:affiliationName":[{"@value":"British Antarctic Survey/NERC  Cambridge UK"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045755636096","@type":"Researcher","foaf:name":[{"@value":"M. J. Beharrell"}],"jpcoar:affiliationName":[{"@value":"Physics Department Lancaster University  Lancaster UK"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045755636101","@type":"Researcher","foaf:name":[{"@value":"C. J. Rodger"}],"jpcoar:affiliationName":[{"@value":"Physics Department Otago University  Dunedin New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045755636100","@type":"Researcher","foaf:name":[{"@value":"P. T. Verronen"}],"jpcoar:affiliationName":[{"@value":"Finnish Meteorological Institute  Helsinki Finland"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045755636102","@type":"Researcher","foaf:name":[{"@value":"M. E. Andersson"}],"jpcoar:affiliationName":[{"@value":"Finnish Meteorological Institute  Helsinki Finland"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045755636099","@type":"Researcher","foaf:name":[{"@value":"D. A. Newnham"}],"jpcoar:affiliationName":[{"@value":"British Antarctic Survey/NERC  Cambridge UK"}]}],"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":"2015-10-03","prism:volume":"42","prism:number":"19","prism:startingPage":"8172","prism:endingPage":"8176"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2015GL065523"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015GL065523"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2015GL065523"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2015GL065523"}],"createdAt":"2015-09-16","modifiedAt":"2023-09-09","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050283688006764800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Transient ionization of the mesosphere during auroral breakup: Arase satellite and ground-based conjugate observations at Syowa Station"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214350822656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mesospheric ozone destruction by high‐energy electron precipitation associated with pulsating aurora"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168733553408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Simulated seasonal impact on middle atmospheric ozone from high-energy electron precipitation related to pulsating aurorae"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580230586885504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mesospheric ionization during substorm growth phase"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593666113280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reconstructing Solar Wind Profiles Associated With Extreme Magnetic Storms: A Machine Learning Approach"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205222184960","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Response of the Middle Atmosphere in the Southern Hemisphere to Energetic Particle Precipitation in the Latest Reanalysis Data"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/2015gl065523"},{"@type":"CROSSREF","@value":"10.1002/2016jd025015_references_DOI_GyaRtxlN9YZlbGtNcDwOs4JZy5H"},{"@type":"CROSSREF","@value":"10.5194/angeo-39-883-2021_references_DOI_GyaRtxlN9YZlbGtNcDwOs4JZy5H"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-0989-7_references_DOI_GyaRtxlN9YZlbGtNcDwOs4JZy5H"},{"@type":"CROSSREF","@value":"10.1051/swsc/2022012_references_DOI_GyaRtxlN9YZlbGtNcDwOs4JZy5H"},{"@type":"CROSSREF","@value":"10.1029/2021gl096275_references_DOI_GyaRtxlN9YZlbGtNcDwOs4JZy5H"},{"@type":"CROSSREF","@value":"10.2151/sola.13a-001_references_DOI_GyaRtxlN9YZlbGtNcDwOs4JZy5H"}]}