{"@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/1364233269097214976.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1080/16742834.2009.11446773"}},{"identifier":{"@type":"URI","@value":"https://www.tandfonline.com/doi/pdf/10.1080/16742834.2009.11446773"}}],"dc:title":[{"@value":"The Impact of Orographically-Induced Gravity Waves on the Diurnal Cycle of Rainfall over Southeast Kalimantan Island"}],"description":[{"notation":[{"@value":"Precipitation measurements from the Tropical Rainfall Measuring Mission (TRMM) satellite indicate that the southeastern area of Kalimantan (Borneo) Island receives much less rainfall than elsewhere on the island during the period from July to October. Results from sur- face meteorological observations show that the diurnal cycle of rainfall differs greatly between the eastern and western coasts of the island. Rainfall on the western coast of the island is frequent in the afternoon and evening, whereas almost all rainfall on the eastern coast occurs in the morning. Meanwhile, the Global Positioning System (GPS)-derived precipitable water (PW) on the eastern coast shows a substantial decrease in moisture in the af- ternoon and evening. Numerical experiments with a mesoscale model reveal that gravity waves driven by di- urnal heating of the elevated land surface of the moun- tains on Sulawesi Island, which lies approximately 300 kilometers to the east of Kalimantan Island, significantly affect the diurnal cycle of rainfall over southeast Kali- mantan Island. Keywords: diurnal cycle, rainfall, precipitable water, Kalimantan (Borneo) Island, gravity wave Citation: Wu, P., J. I. Hamada, M. D. Yamanaka, et al., 2009: The impact of orographically-induced gravity waves on the diurnal cycle of rainfall over southeast Ka- limantan Island, Atmos. Oceanic Sci. Lett., 2, 35−39."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1384233269097214979","@type":"Researcher","foaf:name":[{"@value":"Peiming Wu"}],"jpcoar:affiliationName":[{"@value":"Institute of Observational Research for Global Change, JAMSTEC, Yokosuka, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1384233269097214980","@type":"Researcher","foaf:name":[{"@value":"Jun-Ichi Hamada"}],"jpcoar:affiliationName":[{"@value":"Institute of Observational Research for Global Change, JAMSTEC, Yokosuka, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1384233269097214976","@type":"Researcher","foaf:name":[{"@value":"Manabu D. Yamanaka"}],"jpcoar:affiliationName":[{"@value":"Institute of Observational Research for Global Change, JAMSTEC, Yokosuka, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1384233269097214978","@type":"Researcher","foaf:name":[{"@value":"Jun Matsumoto"}],"jpcoar:affiliationName":[{"@value":"Institute of Observational Research for Global Change, JAMSTEC, Yokosuka, Japan"},{"@value":"Graduate School of Urban Environmental Sciences, Tokyo Metropolitan University, Hachioji, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1384233269097214977","@type":"Researcher","foaf:name":[{"@value":"Masayuki Hara"}],"jpcoar:affiliationName":[{"@value":"Institute of Observational Research for Global Change, JAMSTEC, Yokosuka, Japan"},{"@value":"Frontier Research Center for Global Change, JAMSTEC, Yokohama, Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"16742834"},{"@type":"EISSN","@value":"23766123"}],"prism:publicationName":[{"@value":"Atmospheric and Oceanic Science Letters"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2009-01-01","prism:volume":"2","prism:number":"1","prism:startingPage":"35","prism:endingPage":"39"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"https://www.tandfonline.com/doi/pdf/10.1080/16742834.2009.11446773"}],"createdAt":"2015-07-23","modifiedAt":"2020-11-16","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/1360004232245179392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Observational study on diurnal precipitation cycle in equatorial Indonesia using 1.3-GHz wind profiling radar network and TRMM precipitation radar"}]},{"@id":"https://cir.nii.ac.jp/crid/1390303000764900224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Exploring the Thunderstorm Predictors in Indonesia"}]},{"@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":"10.1080/16742834.2009.11446773"},{"@type":"OPENAIRE","@value":"doi_dedup___::7f21f623befe0f234c7fc1470d8ae5f3"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0202-9_references_DOI_UaIMvbjc6twrmu7KOMJKMlmPKCA"},{"@type":"CROSSREF","@value":"10.1016/j.jastp.2010.10.003_references_DOI_UaIMvbjc6twrmu7KOMJKMlmPKCA"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0174-9_references_DOI_UaIMvbjc6twrmu7KOMJKMlmPKCA"},{"@type":"CROSSREF","@value":"10.2151/sola.2025-007_references_DOI_UaIMvbjc6twrmu7KOMJKMlmPKCA"}]}