{"@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/1361137044878844672.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/ncomms6197"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/ncomms6197.pdf"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/ncomms6197"}}],"dc:title":[{"@value":"Missing driver in the Sun–Earth connection from energetic electron precipitation impacts mesospheric ozone"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Energetic electron precipitation (EEP) from the Earth’s outer radiation belt continuously affects the chemical composition of the polar mesosphere. EEP can contribute to catalytic ozone loss in the mesosphere through ionization and enhanced production of odd hydrogen. However, the long-term mesospheric ozone variability caused by EEP has not been quantified or confirmed to date. Here we show, using observations from three different satellite instruments, that EEP events strongly affect ozone at 60–80 km, leading to extremely large (up to 90%) short-term ozone depletion. This impact is comparable to that of large, but much less frequent, solar proton events. On solar cycle timescales, we find that EEP causes ozone variations of up to 34% at 70–80 km. With such a magnitude, it is reasonable to suspect that EEP could be an important part of solar influence on the atmosphere and climate system.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380017282197385494","@type":"Researcher","foaf:name":[{"@value":"M. E. Andersson"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044878844801","@type":"Researcher","foaf:name":[{"@value":"P. T. Verronen"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044878844673","@type":"Researcher","foaf:name":[{"@value":"C. J. Rodger"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044878844672","@type":"Researcher","foaf:name":[{"@value":"M. A. Clilverd"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044878844800","@type":"Researcher","foaf:name":[{"@value":"A. Seppälä"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"20411723"}],"prism:publicationName":[{"@value":"Nature Communications"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2014-10-14","prism:volume":"5","prism:number":"1","prism:startingPage":"5197"},"reviewed":"false","dc:rights":["https://creativecommons.org/licenses/by/4.0","https://creativecommons.org/licenses/by/4.0"],"url":[{"@id":"https://www.nature.com/articles/ncomms6197.pdf"},{"@id":"https://www.nature.com/articles/ncomms6197"}],"createdAt":"2014-10-14","modifiedAt":"2024-06-03","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050007846254847232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Penetration of MeV electrons into the mesosphere accompanying pulsating aurorae"}]},{"@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/1360017282208937728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Localized mesospheric ozone destruction corresponding to isolated proton aurora coming from Earth’s radiation belt"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298757416785408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Statistical Survey of Arase Satellite Data Sets in Conjunction With the Finnish Riometer Network"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306905180879104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"On the Spatial and Temporal Evolution of EMIC Wave‐Driven Relativistic Electron Precipitation: Magnetically Conjugate Observations From the Van Allen Probes and CALET"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654732443264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Energetic electron precipitation associated with pulsating aurora: EISCAT and Van Allen Probe observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360849943103244928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"HO2 Generation Above Sprite‐Producing Thunderstorms Derived from Low‐Noise SMILES Observation Spectra"}]},{"@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"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367078673408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A review of the SCOSTEP’s 5-year scientific program VarSITI—Variability of the Sun and Its Terrestrial Impact"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1038/ncomms6197"},{"@type":"CROSSREF","@value":"10.1002/2016jd025015_references_DOI_ZmJOL1V4T8l0mOeZbpjiqwrp6lw"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00410-1_references_DOI_ZmJOL1V4T8l0mOeZbpjiqwrp6lw"},{"@type":"CROSSREF","@value":"10.1038/s41598-022-20548-2_references_DOI_ZmJOL1V4T8l0mOeZbpjiqwrp6lw"},{"@type":"CROSSREF","@value":"10.1029/2022ja030271_references_DOI_ZmJOL1V4T8l0mOeZbpjiqwrp6lw"},{"@type":"CROSSREF","@value":"10.1029/2023gl107087_references_DOI_ZmJOL1V4T8l0mOeZbpjiqwrp6lw"},{"@type":"CROSSREF","@value":"10.1038/s41598-021-92611-3_references_DOI_ZmJOL1V4T8l0mOeZbpjiqwrp6lw"},{"@type":"CROSSREF","@value":"10.1002/2014ja020690_references_DOI_ZmJOL1V4T8l0mOeZbpjiqwrp6lw"},{"@type":"CROSSREF","@value":"10.1029/2019gl085529_references_DOI_ZmJOL1V4T8l0mOeZbpjiqwrp6lw"},{"@type":"CROSSREF","@value":"10.2151/sola.13a-001_references_DOI_ZmJOL1V4T8l0mOeZbpjiqwrp6lw"}]}