{"@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/1363670319489943936.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2006gl027086"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2006GL027086"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2006GL027086"}}],"dc:title":[{"@value":"Assessment of composite global sampling: Sea surface wind speed"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Research and forecasts of the weather‐ocean‐climate system demand increasingly higher resolution forcing data. Here we assess the improvement in composite global observations and the feasibility of producing high resolution blended sea winds. The number of the long‐term US sea surface wind speed observing satellites has increased from one in July 1987 to five or more since 2000. Global 0.25° gridded, blended products with temporal resolutions of 6‐hours, 12‐hours and daily have become feasible since mid 2002, mid 1995 and January 1991, respectively (with ≥75% time coverage and ≥90% spatial coverage between 65°S–65°N). If the coverage is relaxed, the feasible times can be extended to earlier periods. These statistics provide practical guidance to produce reliable blended products for different applications, and serve as guidance on the design of future global observing systems.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380016865943960192","@type":"Researcher","foaf:name":[{"@value":"Huai‐Min Zhang"}],"jpcoar:affiliationName":[{"@value":"National Climatic Data Center NOAA NESDIS  Asheville North Carolina USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319489944065","@type":"Researcher","foaf:name":[{"@value":"John J. Bates"}],"jpcoar:affiliationName":[{"@value":"National Climatic Data Center NOAA NESDIS  Asheville North Carolina USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319489944064","@type":"Researcher","foaf:name":[{"@value":"Richard W. Reynolds"}],"jpcoar:affiliationName":[{"@value":"National Climatic Data Center NOAA NESDIS  Asheville North Carolina USA"}]}],"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":"2006-09","prism:volume":"33","prism:number":"17","prism:startingPage":"L17714"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2006GL027086"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2006GL027086"}],"createdAt":"2006-09-13","modifiedAt":"2023-10-31","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050564285797084544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Long-term impacts of ocean wave-dependent roughness on global climate systems"},{"@value":"Long‐term impacts of ocean wave‐dependent roughness on global climate systems"}]},{"@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/1360283690374881664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Impact of downward heat penetration below the shallow seasonal thermocline on the sea surface temperature"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118790842240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of dissolved oxygen and nutrients from the Kuroshio on hypoxia off the Changjiang River estuary"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206503516672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Assessment of Ocean Surface Winds and Tropical Cyclones around Japan by RCMs"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680296562688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"全球大気気候-波浪結合モデルによる海面粗度を通した波浪の気候への影響評価"},{"@language":"en","@value":"OCEAN WAVE-DEPENDENT ROUGHNESS IMPACTS ON CLIMATE SYSTEM BY COUPLED ATMOSPHERIC GLOBAL CLIMATE-WAVE MODEL"},{"@language":"ja-Kana","@value":"ゼン キュウ タイキ キコウ-ハロウ ケツゴウ モデル ニ ヨル カイメンソド オ トオシタ ハロウ ノ キコウ エ ノ エイキョウ ヒョウカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681480379264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Capability of Regional Climate Models in Simulating Coastal Winds and Waves around Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2006gl027086"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0202-9_references_DOI_384JEnbzu6YijLQG8hsDoltFQcl"},{"@type":"CROSSREF","@value":"10.1002/2016jc012621_references_DOI_384JEnbzu6YijLQG8hsDoltFQcl"},{"@type":"CROSSREF","@value":"10.1007/s10872-015-0275-7_references_DOI_384JEnbzu6YijLQG8hsDoltFQcl"},{"@type":"CROSSREF","@value":"10.2151/jmsj.2012-b08_references_DOI_384JEnbzu6YijLQG8hsDoltFQcl"},{"@type":"CROSSREF","@value":"10.2208/kaigan.72.i_1507_references_DOI_384JEnbzu6YijLQG8hsDoltFQcl"},{"@type":"CROSSREF","@value":"10.2151/jmsj.2012-502_references_DOI_384JEnbzu6YijLQG8hsDoltFQcl"},{"@type":"CROSSREF","@value":"10.1007/s00343-021-0440-3_references_DOI_384JEnbzu6YijLQG8hsDoltFQcl"}]}