{"@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/1361137043935359744.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.5194/essd-8-165-2016"}},{"identifier":{"@type":"URI","@value":"https://essd.copernicus.org/articles/8/165/2016/essd-8-165-2016.pdf"}}],"dc:title":[{"@value":"A long-term record of blended satellite and in situ sea-surface temperature for climate monitoring, modeling and environmental studies"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Abstract. This paper describes a blended sea-surface temperature (SST) data set that is part of the National Oceanic and Atmospheric Administration (NOAA) Climate Data Record (CDR) program product suite. Using optimum interpolation (OI), in situ and satellite observations are combined on a daily and 0.25° spatial grid to form an SST analysis, i.e., a spatially complete field. A large-scale bias adjustment of the input infrared SSTs is made using buoy and ship observations as a reference. This is particularly important for the time periods when volcanic aerosols from the El Chichón and Mt. Pinatubo eruptions are widespread globally. The main source of SSTs is the Advanced Very High Resolution Radiometer (AVHRR), available from late 1981 to the present, which is also the temporal span of this CDR. The input and processing choices made to ensure a consistent data set that meets the CDR requirements are summarized. A brief history and an explanation of the forward production schedule for the preliminary and science-quality final product are also provided. The data set is produced and archived at the newly formed National Centers for Environmental Information (NCEI) in Network Common Data Form (netCDF) at doi:10.7289/V5SQ8XB5.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137043935359744","@type":"Researcher","foaf:name":[{"@value":"Viva Banzon"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043935359747","@type":"Researcher","foaf:name":[{"@value":"Thomas M. Smith"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043935359748","@type":"Researcher","foaf:name":[{"@value":"Toshio Mike Chin"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043935359745","@type":"Researcher","foaf:name":[{"@value":"Chunying Liu"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043935359746","@type":"Researcher","foaf:name":[{"@value":"William Hankins"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"18663516"}],"prism:publicationName":[{"@value":"Earth System Science Data"}],"dc:publisher":[{"@value":"Copernicus GmbH"}],"prism:publicationDate":"2016-04-28","prism:volume":"8","prism:number":"1","prism:startingPage":"165","prism:endingPage":"176"},"reviewed":"false","dc:rights":["https://creativecommons.org/licenses/by/3.0/"],"url":[{"@id":"https://essd.copernicus.org/articles/8/165/2016/essd-8-165-2016.pdf"}],"createdAt":"2016-04-28","modifiedAt":"2025-02-08","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1051693803343107968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Meridional march of diurnal rainfall over Jakarta, Indonesi a, observed with a C-band Doppler radar: An overview of the HARIMAU2010 campaign"},{"@value":"Diurnal land–sea rainfall peak migration over Sumatera Island, Indonesian maritime continent, observed by TRMM satellite and intensive rawinsonde soundings"},{"@value":"Diurnal land-sea rainfall peak migration over Sumatera Island, Indonesian IMC observed by TRMM satellite and intensive rawinsonde soundings"},{"@value":"Diurnal landsea rainfall peak migration over Sumatra Island, Indonesian maritime continent observed by TRMM satellite and intensive rawinsonde soundings"},{"@value":"Forecasting for flood warning"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231382217984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Origin of intraseasonal variability in the eastern equatorial Indian Ocean: intrinsic variability and local and remote wind stress forcings"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004236560232064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ensemble-Based Atmospheric Reanalysis Using a Global Coupled Atmosphere–Ocean GCM"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142868678784","@type":"Article","resourceType":"学術雑誌論文(journal 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