{"@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/1362825895266676992.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.5194/angeo-19-889-2001"}},{"identifier":{"@type":"URI","@value":"https://angeo.copernicus.org/articles/19/889/2001/angeo-19-889-2001.pdf"}}],"dc:title":[{"@value":"Precipitating clouds observed by 1.3-GHz boundary layer radars in equatorial Indonesia"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Abstract. Temporal variations of precipitating clouds in equatorial Indonesia have been studied based on observations with 1357.5 MHz boundary layer radars at Serpong (6.4° S, 106.7° E) near Jakarta and Bukittinggi (0.2° S, 100.3° E) in West Sumatera. We have classified precipitating clouds into four types: stratiform, mixed stratiform-convective, deep convective, and shallow convective clouds, using the Williams et al. (1995) method. Diurnal variations of the occurrence of precipitating clouds at Serpong and Bukittinggi have showed the same characteristics, namely, that the precipitating clouds primarily occur in the afternoon and the peak of the stratiform cloud comes after the peak of the deep convective cloud. The time delay between the peaks of stratiform and deep convective clouds corresponds to the life cycle of the mesoscale convective system. The precipitating clouds which occur in the early morning at Serpong are dominated by stratiform cloud. Concerning seasonal variations of the precipitating clouds, we have found that the occurrence of the stratiform cloud is most frequent in the rainy season, while the occurrence of the deep convective cloud is predominant in the dry season.Key words. Meteorology and atmospheric dynamics (convective processes; precipitation; tropical meteorology)\n                    </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004057903099782","@type":"Researcher","foaf:name":[{"@value":"F. Renggono"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895266676998","@type":"Researcher","foaf:name":[{"@value":"H. Hashiguchi"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895266676999","@type":"Researcher","foaf:name":[{"@value":"S. Fukao"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895266676994","@type":"Researcher","foaf:name":[{"@value":"M. D. Yamanaka"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895266676992","@type":"Researcher","foaf:name":[{"@value":"S.-Y. Ogino"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895266676997","@type":"Researcher","foaf:name":[{"@value":"N. Okamoto"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895266676996","@type":"Researcher","foaf:name":[{"@value":"F. Murata"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895266677000","@type":"Researcher","foaf:name":[{"@value":"B. P. Sitorus"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895266677002","@type":"Researcher","foaf:name":[{"@value":"M. Kudsy"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895266676993","@type":"Researcher","foaf:name":[{"@value":"M. Kartasasmita"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895266677001","@type":"Researcher","foaf:name":[{"@value":"G. Ibrahim"}]}],"contributor":[{"@id":"https://cir.nii.ac.jp/crid/1890020692793005060","@type":"Researcher","foaf:name":[{"@value":"Agency for the Assessment and Application of Technology (BPPT) ; Agency for the Assessment and Application of Technology (BPPT)"}]},{"@id":"https://cir.nii.ac.jp/crid/1890020692793005068","@type":"Researcher","foaf:name":[{"@value":"Radio Science Center for Space and Atmosphere [Kyoto] (RASC) ; Kyoto University"}]},{"@id":"https://cir.nii.ac.jp/crid/1890020692793005057","@type":"Researcher","foaf:name":[{"@value":"Graduate School of Science and Technology ; Kobe University"}]},{"@id":"https://cir.nii.ac.jp/crid/1890020692793005058","@type":"Researcher","foaf:name":[{"@value":"Frontier Observation Research System for Global Change ; Frontier Observation Research System for Global Change"}]},{"@id":"https://cir.nii.ac.jp/crid/1890020692793005056","@type":"Researcher","foaf:name":[{"@value":"Indonesian National Institute of Aeronautics and Space (LAPAN)"}]},{"@id":"https://cir.nii.ac.jp/crid/1890020692793005067","@type":"Researcher","foaf:name":[{"@value":"Indonesian Meteorological, Climatologicall and Geophysical Agency (BMKG)"}]},{"@id":"https://cir.nii.ac.jp/crid/1890020692793005063","@type":"Researcher","foaf:name":[{"@value":"Radio Science Center for Space and Atmosphere [Kyoto] (RASC) ; Kyoto University [Kyoto]"}]},{"@id":"https://cir.nii.ac.jp/crid/1890020692793005064","@type":"Researcher","foaf:name":[{"@value":"EGU, Publication"}]},{"@id":"https://cir.nii.ac.jp/crid/1892836540696320384","@type":"Researcher","foaf:name":[{"@value":"Agency for the Assessment and Application of Technology (BPPT)"}]},{"@id":"https://cir.nii.ac.jp/crid/1892836540696320512","@type":"Researcher","foaf:name":[{"@value":"Radio Science Center for Space and Atmosphere Kyoto (RASC)"}]},{"@id":"https://cir.nii.ac.jp/crid/1892836540696320514","@type":"Researcher","foaf:name":[{"@value":"Graduate School of Science and Technology"}]},{"@id":"https://cir.nii.ac.jp/crid/1892836540696320516","@type":"Researcher","foaf:name":[{"@value":"Kobe University"}]},{"@id":"https://cir.nii.ac.jp/crid/1892836540696320515","@type":"Researcher","foaf:name":[{"@value":"Kyoto University"}]},{"@id":"https://cir.nii.ac.jp/crid/1892836540696320513","@type":"Researcher","foaf:name":[{"@value":"Frontier Observation Research System for Global Change"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"14320576"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/00034029"}],"prism:publicationName":[{"@value":"Annales Geophysicae"}],"dc:publisher":[{"@value":"Copernicus GmbH"}],"prism:publicationDate":"2001-08-31","prism:volume":"19","prism:number":"8","prism:startingPage":"889","prism:endingPage":"897"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://creativecommons.org/licenses/by/3.0/"],"url":[{"@id":"https://angeo.copernicus.org/articles/19/889/2001/angeo-19-889-2001.pdf"}],"createdAt":"2010-06-15","modifiedAt":"2021-01-27","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.OCEAN%5DSciences%20of%20the%20Universe%20%5Bphysics%5D/Ocean,%20Atmosphere","dc:title":"[SDU.OCEAN]Sciences of the Universe [physics]/Ocean, Atmosphere"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.OCEAN%5DSciences%20of%20the%20Universe%20%5Bphysics%5D/Ocean","dc:title":"[SDU.OCEAN]Sciences of the Universe [physics]/Ocean"},{"@id":"https://cir.nii.ac.jp/all?q=Atmosphere","dc:title":"Atmosphere"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.OCEAN%5D%20Sciences%20of%20the%20Universe%20%5Bphysics%5D/Ocean,%20Atmosphere","dc:title":"[SDU.OCEAN] Sciences of the Universe [physics]/Ocean, Atmosphere"},{"@id":"https://cir.nii.ac.jp/all?q=QC801-809","dc:title":"QC801-809"},{"@id":"https://cir.nii.ac.jp/all?q=Science","dc:title":"Science"},{"@id":"https://cir.nii.ac.jp/all?q=Physics","dc:title":"Physics"},{"@id":"https://cir.nii.ac.jp/all?q=QC1-999","dc:title":"QC1-999"},{"@id":"https://cir.nii.ac.jp/all?q=Q","dc:title":"Q"},{"@id":"https://cir.nii.ac.jp/all?q=Geophysics.%20Cosmic%20physics","dc:title":"Geophysics. Cosmic physics"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.STU%5DSciences%20of%20the%20Universe%20%5Bphysics%5D/Earth%20Sciences","dc:title":"[SDU.STU]Sciences of the Universe [physics]/Earth Sciences"},{"@id":"https://cir.nii.ac.jp/all?q=551","dc:title":"551"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.STU%5D%20Sciences%20of%20the%20Universe%20%5Bphysics%5D/Earth%20Sciences","dc:title":"[SDU.STU] Sciences of the Universe [physics]/Earth Sciences"}],"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 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