{"@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/1363670319792947200.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.5194/essd-10-469-2018"}},{"identifier":{"@type":"URI","@value":"https://essd.copernicus.org/articles/10/469/2018/essd-10-469-2018.pdf"}}],"dc:title":[{"@value":"A global space-based stratospheric aerosol climatology: 1979–2016"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Abstract. We describe the construction of a continuous 38-year record of stratospheric\naerosol optical properties. The Global Space-based Stratospheric Aerosol\nClimatology, or GloSSAC, provided the input data to the construction of the\nClimate Model Intercomparison Project stratospheric aerosol forcing data set\n(1979–2014) and we have extended it through 2016 following an identical\nprocess. GloSSAC focuses on the Stratospheric Aerosol and Gas Experiment\n(SAGE) series of instruments through mid-2005, and on the Optical\nSpectrograph and InfraRed Imager System (OSIRIS) and the Cloud-Aerosol Lidar\nand Infrared Pathfinder Satellite Observation (CALIPSO) data thereafter. We\nalso use data from other space instruments and from ground-based, air, and\nballoon borne instruments to fill in key gaps in the data set. The end result\nis a global and gap-free data set focused on aerosol extinction coefficient\nat 525 and 1020 nm and other parameters on an “as available” basis. For\nthe primary data sets, we developed a new method for filling the\npost-Pinatubo eruption data gap for 1991–1993 based on data from the\nCryogenic Limb Array Etalon Spectrometer. In addition, we developed a new\nmethod for populating wintertime high latitudes during the SAGE period\nemploying a latitude-equivalent latitude conversion process that greatly\nimproves the depiction of aerosol at high latitudes compared to earlier\nsimilar efforts. We report data in the troposphere only when and where it is\navailable. This is primarily during the SAGE II period except for the most\nenhanced part of the Pinatubo period. It is likely that the upper troposphere\nduring Pinatubo was greatly enhanced over non-volcanic periods and that\ndomain remains substantially under-characterized. We note that aerosol levels\nduring the OSIRIS/CALIPSO period in the lower stratosphere at mid- and high\nlatitudes is routinely higher than what we observed during the SAGE II\nperiod. While this period had nearly continuous low-level volcanic activity,\nit is possible that the enhancement in part reflects deficiencies in the data\nset. We also expended substantial effort to quality assess the data set and\nthe product is by far the best we have produced. GloSSAC version 1.0 is\navailable in netCDF format at the NASA Atmospheric Data Center at\nhttps://eosweb.larc.nasa.gov/. GloSSAC users should cite this paper and\nthe data set DOI (https://doi.org/10.5067/GloSSAC-L3-V1.0).</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670319792947206","@type":"Researcher","foaf:name":[{"@value":"Larry W. Thomason"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319792947202","@type":"Researcher","foaf:name":[{"@value":"Nicholas Ernest"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319792947207","@type":"Researcher","foaf:name":[{"@value":"Luis Millán"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319792947072","@type":"Researcher","foaf:name":[{"@value":"Landon Rieger"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319792947203","@type":"Researcher","foaf:name":[{"@value":"Adam Bourassa"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319792947073","@type":"Researcher","foaf:name":[{"@value":"Jean-Paul Vernier"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319792947205","@type":"Researcher","foaf:name":[{"@value":"Gloria Manney"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319792947201","@type":"Researcher","foaf:name":[{"@value":"Beiping Luo"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319792947200","@type":"Researcher","foaf:name":[{"@value":"Florian Arfeuille"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319792947204","@type":"Researcher","foaf:name":[{"@value":"Thomas Peter"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"18663516"}],"prism:publicationName":[{"@value":"Earth System Science Data"}],"dc:publisher":[{"@value":"Copernicus GmbH"}],"prism:publicationDate":"2018-03-12","prism:volume":"10","prism:number":"1","prism:startingPage":"469","prism:endingPage":"492"},"reviewed":"false","dc:rights":["https://creativecommons.org/licenses/by/4.0/"],"url":[{"@id":"https://essd.copernicus.org/articles/10/469/2018/essd-10-469-2018.pdf"}],"createdAt":"2018-03-12","modifiedAt":"2025-02-07","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050306506450697472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"High Flux of Small Sulfate Aerosols During the 1970s Reconstructed From the SE-Dome Ice Core in Greenland"},{"@value":"High Flux of Small Sulfate Aerosols During the 1970s Reconstructed From the SE‐Dome Ice Core in Greenland"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025431115329408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Analysis of the global atmospheric background sulfur budget in a multi-model framework"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588381083015040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Last-millennium volcanic forcing and climate  response using SO\n                    <sub>2</sub>\n                    emissions"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282752327488128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Meteorological Research Institute Earth System Model Version 2.0, MRI-ESM2.0: Description and Basic Evaluation of the Physical Component"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.5194/essd-10-469-2018"},{"@type":"CROSSREF","@value":"10.5194/acp-24-5513-2024_references_DOI_GYkhvEOYWgXzgzmeO35oX4aRS0M"},{"@type":"CROSSREF","@value":"10.2151/jmsj.2019-051_references_DOI_GYkhvEOYWgXzgzmeO35oX4aRS0M"},{"@type":"CROSSREF","@value":"10.1029/2022jd036880_references_DOI_GYkhvEOYWgXzgzmeO35oX4aRS0M"},{"@type":"CROSSREF","@value":"10.5194/cp-21-161-2025_references_DOI_GYkhvEOYWgXzgzmeO35oX4aRS0M"}]}