{"@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/1362825896063403392.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2005gl023041"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2005GL023041"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005GL023041"}}],"dc:title":[{"@value":"Atmospheric response to NO<sub>y</sub> source due to energetic electron precipitation"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We have introduced additional NO<jats:sub>y</jats:sub> sources caused by energetic electron precipitation (EEP) during 1987 into a Chemistry‐Climate model. Comparison of two model runs with and without EEP reveals increase of reactive nitrogen by about 2 ppbv in the middle stratosphere over the tropical and middle latitudes. In the upper stratosphere over the polar winter regions the simulated NO<jats:sub>y</jats:sub> enhancement reaches 10 ppbv. Decreases of the ozone mixing ratio in the stratosphere by up to 5% over midlatitudes and up to 30% over southern high‐latitudes are calculated. A ∼0.5 K cooling in the middle stratosphere over the tropics and up to 2 K over southern high‐latitudes is calculated with detectable changes in the surface air temperatures. These results confirm that the magnitude of the atmospheric response to EEP events can potentially exceed the effects from solar UV fluxes. These mechanisms work in phase outside polar latitudes, but can compensate each other within polar latitudes.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380567007856358032","@type":"Researcher","foaf:name":[{"@value":"E. Rozanov"}],"jpcoar:affiliationName":[{"@value":"Physical‐Meteorological Observatory/World Radiation Center  Davos Switzerland"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896063403397","@type":"Researcher","foaf:name":[{"@value":"L. Callis"}],"jpcoar:affiliationName":[{"@value":"Suffolk Virginia USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896063403393","@type":"Researcher","foaf:name":[{"@value":"M. Schlesinger"}],"jpcoar:affiliationName":[{"@value":"Climate Research Group, Department of Atmospheric Sciences University of Illinois at Urbana‐Champaign  Urbana Illinois USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896063403392","@type":"Researcher","foaf:name":[{"@value":"F. Yang"}],"jpcoar:affiliationName":[{"@value":"National Centers for Environmental Prediction  Camp Springs Maryland USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896063403395","@type":"Researcher","foaf:name":[{"@value":"N. Andronova"}],"jpcoar:affiliationName":[{"@value":"Climate Research Group, Department of Atmospheric Sciences University of Illinois at Urbana‐Champaign  Urbana Illinois USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896063403394","@type":"Researcher","foaf:name":[{"@value":"V. Zubov"}],"jpcoar:affiliationName":[{"@value":"Department of Dynamical Meteorology A. I. Voeikov Main Geophysical Observatory  St. Petersburg Russia"}]}],"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":"2005-07-22","prism:volume":"32","prism:number":"14","prism:startingPage":"L14811"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2005GL023041"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005GL023041"}],"createdAt":"2005-07-21","modifiedAt":"2023-10-31","relatedProduct":[{"@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/1360283691683506688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coupled chemistry climate model simulations of the solar cycle in ozone and temperature"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848655764317824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamic Inner Magnetosphere: A Tutorial and Recent Advances"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417166183168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The science case for the EISCAT_3D radar"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2005gl023041"},{"@type":"CROSSREF","@value":"10.1186/s40645-015-0051-8_references_DOI_F0k8b7NpU8BDd2oEjbL5zVUyVP0"},{"@type":"CROSSREF","@value":"10.5194/angeo-39-883-2021_references_DOI_F0k8b7NpU8BDd2oEjbL5zVUyVP0"},{"@type":"CROSSREF","@value":"10.1029/2007jd009391_references_DOI_F0k8b7NpU8BDd2oEjbL5zVUyVP0"},{"@type":"CROSSREF","@value":"10.1007/978-94-007-0501-2_9_references_DOI_F0k8b7NpU8BDd2oEjbL5zVUyVP0"}]}