{"@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/1361981471209547136.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1175/jcli-d-12-00178.1"}},{"identifier":{"@type":"URI","@value":"http://journals.ametsoc.org/jcli/article-pdf/26/5/1772/4022000/jcli-d-12-00178_1.pdf"}}],"dc:title":[{"@value":"Diurnal Cycle in Different Weather Regimes and Rainfall Variability over Borneo Associated with ENSO"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n               <jats:p>The interannual variability of precipitation over the island of Borneo in association with El Niño–Southern Oscillation (ENSO) has been studied by using the Global Precipitation Climatology Centre (GPCC) gridded rain gauge precipitation, the NOAA Climate Prediction Center (CPC) Morphing Technique (CMORPH) satellite estimated precipitation, the Quick Scatterometer (QuikSCAT) satellite estimated sea winds, and the National Centers for Environmental Prediction (NCEP)–National Center for Atmospheric Research (NCAR) reanalysis data. Analysis of the GPCC precipitation shows a dipolar structure of wet southwest versus dry central and northeast in precipitation anomalies associated with El Niño over Borneo Island during the austral summer [December–February (DJF)]. By using the 0.25° and 3-hourly CMORPH precipitation, it is found that rainfall over Borneo is strongly affected by the diurnal cycle of land–sea breezes. The spatial distribution of rainfall over Borneo depends on the direction of monsoonal winds. Weather typing analysis indicates that the dipolar structure of rainfall anomalies associated with ENSO is caused by the variability in the frequency of occurrence of different weather types. Rainfall is enhanced in the coastal region where sea breezes head against off-shore synoptic-scale low-level winds (i.e., in the lee side or wake area of the island), which is referred to here as the “wake effect.” In DJF of El Niño years, the northwesterly austral summer monsoon in southern Borneo is weaker than normal over the Maritime Continent and easterly winds are more frequent than normal over Borneo, acting to enhance rainfall over the southwest coast of the island. This coastal rainfall generation mechanism in different weather types explains the dipole pattern of a wet southwest versus dry northeast in the rainfall anomalies over Borneo Island in the El Niño years.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381981471209547138","@type":"Researcher","foaf:name":[{"@value":"Jian-Hua Qian"}],"jpcoar:affiliationName":[{"@value":"Department of Environmental, Earth, and Atmospheric Sciences, University of Massachusetts, Lowell, Massachusetts, and International Research Institute for Climate and Society, Columbia University, Palisades, New York"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981471209547136","@type":"Researcher","foaf:name":[{"@value":"Andrew W. Robertson"}],"jpcoar:affiliationName":[{"@value":"International Research Institute for Climate and Society, Columbia University, Palisades, New York"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981471209547137","@type":"Researcher","foaf:name":[{"@value":"Vincent Moron"}],"jpcoar:affiliationName":[{"@value":"International Research Institute for Climate and Society, Columbia University, Palisades, New York, and CEREGE, UMR 6635 CNRS, Aix-Marseilles University, Aix en Provence, and Institut Universitaire de France, Paris, France"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"08948755"},{"@type":"EISSN","@value":"15200442"}],"prism:publicationName":[{"@value":"Journal of Climate"}],"dc:publisher":[{"@value":"American Meteorological Society"}],"prism:publicationDate":"2013-02-27","prism:volume":"26","prism:number":"5","prism:startingPage":"1772","prism:endingPage":"1790"},"reviewed":"false","url":[{"@id":"http://journals.ametsoc.org/jcli/article-pdf/26/5/1772/4022000/jcli-d-12-00178_1.pdf"}],"createdAt":"2012-09-21","modifiedAt":"2020-12-07","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360567180087425664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Interpretation of El Niño–Southern Oscillation‐related precipitation anomalies in north‐western Borneo using isotopic tracers"}]},{"@id":"https://cir.nii.ac.jp/crid/1390850247500160256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Impact of Diurnal Precipitation over Sumatra Island, Indonesia, on Synoptic Disturbances and its Relation to the Madden-Julian Oscillation"},{"@language":"ja","@value":"インドネシア・スマトラ島上の日周期降水が総観規模擾乱へ与える影響とマッデン・ジュリアン振動との関係"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317008513152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Maritime continent coastlines controlling Earth’s climate"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1175/jcli-d-12-00178.1"},{"@type":"CROSSREF","@value":"10.2151/jmsj.2021-007_references_DOI_HGXQD42x7ou4yg3cqK82LrbYoDe"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0174-9_references_DOI_HGXQD42x7ou4yg3cqK82LrbYoDe"},{"@type":"CROSSREF","@value":"10.1002/hyp.13164_references_DOI_HGXQD42x7ou4yg3cqK82LrbYoDe"}]}