{"@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/1390001205223608832.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2151/sola.2013-029"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/sola/9/0/9_2013-029/_pdf"}},{"identifier":{"@type":"NAID","@value":"130004448607"}}],"dc:title":[{"@language":"en","@value":"Numerical Examination of the Diurnal Variation of Summer Precipitation over Southern China"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"Diurnal variation of precipitation is frequently observed over southern China in summer. We investigate it using the regional version of the nonhydrostatic icosahedral atmospheric model (NICAM), with particular focus on the interactions among land, cloud, and radiation processes. The NICAM almost exactly reproduces the diurnal variation of precipitation but slightly overestimates its amplitude. The simulated spatial distribution of precipitation is very similar to that observed by the Tropical Rainfall Measuring Mission 3B42 product. Precipitating region propagates inland from the coast during 14-20 LT.<br>We perform sensitivity experiments to study the effects of surface conditions, cloud, and radiation interactions, and the results are as follows. 1) When volumetric soil moisture is reduced, surface temperature increases and surface evaporation decreases. Water vapor inflow increases owing to enhanced land-sea contrast; however, the decrease in surface evaporation counteracts this increase, thus decreasing precipitation. 2) When cloud amount is reduced, net downward radiation and surface temperature increase. Precipitation does not appear to vary with cloud conditions. <br>The zone of the horizontal convergence of water vapor flux propagates inland in the afternoon, although local evaporation has a greater impact than water vapor inflow on the diurnal variation of precipitation."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420282801203676032","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"00255142"},{"@type":"NRID","@value":"1000000255142"},{"@type":"ORCID","@value":"0000-0003-3580-8897"},{"@type":"NRID","@value":"9000237753345"},{"@type":"NRID","@value":"9000363410460"},{"@type":"NRID","@value":"9000363483094"},{"@type":"NRID","@value":"9000363409305"},{"@type":"NRID","@value":"9000363409497"},{"@type":"NRID","@value":"9000016677454"},{"@type":"NRID","@value":"9000363408060"},{"@type":"NRID","@value":"9000363408460"},{"@type":"NRID","@value":"9000363407260"},{"@type":"NRID","@value":"9000363408345"},{"@type":"NRID","@value":"9000408857853"},{"@type":"NRID","@value":"9000363480371"},{"@type":"NRID","@value":"9000345262186"},{"@type":"NRID","@value":"9000404264073"},{"@type":"NRID","@value":"9000409480680"},{"@type":"NRID","@value":"9000397856599"},{"@type":"NRID","@value":"9000408915818"},{"@type":"NRID","@value":"9000257767941"},{"@type":"NRID","@value":"9000257768665"},{"@type":"NRID","@value":"9000283593815"},{"@type":"NRID","@value":"9000016772697"},{"@type":"NRID","@value":"9000363409427"},{"@type":"NRID","@value":"9000363409365"},{"@type":"NRID","@value":"9000363404975"},{"@type":"NRID","@value":"9000363504097"},{"@type":"NRID","@value":"9000363410134"},{"@type":"NRID","@value":"9000363408058"},{"@type":"NRID","@value":"9000363406923"},{"@type":"NRID","@value":"9000288831342"},{"@type":"NRID","@value":"9000363480394"},{"@type":"NRID","@value":"9000399382466"},{"@type":"NRID","@value":"9000392818776"},{"@type":"NRID","@value":"9000411568492"},{"@type":"NRID","@value":"9000411532968"},{"@type":"NRID","@value":"9000369724335"},{"@type":"NRID","@value":"9000404156904"},{"@type":"NRID","@value":"9000363410850"},{"@type":"NRID","@value":"9000363406134"},{"@type":"NRID","@value":"9000242877460"},{"@type":"NRID","@value":"9000316214815"},{"@type":"NRID","@value":"9000414745637"},{"@type":"NRID","@value":"9000009089809"},{"@type":"NRID","@value":"9000415348767"},{"@type":"NRID","@value":"9000364842130"},{"@type":"NRID","@value":"9000363410927"},{"@type":"NRID","@value":"9000363411093"},{"@type":"NRID","@value":"9000363481630"},{"@type":"NRID","@value":"9000363408048"},{"@type":"NRID","@value":"9000363406441"},{"@type":"NRID","@value":"9000240188058"},{"@type":"NRID","@value":"9000002584097"},{"@type":"NRID","@value":"9000363405702"},{"@type":"NRID","@value":"9000363408064"},{"@type":"NRID","@value":"9000242878036"},{"@type":"NRID","@value":"9000283236668"},{"@type":"NRID","@value":"9000363410528"},{"@type":"NRID","@value":"9000339140590"},{"@type":"NRID","@value":"9000250466295"},{"@type":"NRID","@value":"9000363479087"},{"@type":"NRID","@value":"9000257768700"},{"@type":"NRID","@value":"9000006194004"},{"@type":"NRID","@value":"9000363410517"},{"@type":"NRID","@value":"9000363410410"},{"@type":"NRID","@value":"9000364841883"},{"@type":"NRID","@value":"9000363410987"},{"@type":"NRID","@value":"9000364841383"},{"@type":"NRID","@value":"9000364841598"},{"@type":"NRID","@value":"9000363409422"},{"@type":"NRID","@value":"9000363405354"},{"@type":"NRID","@value":"9000363481413"},{"@type":"NRID","@value":"9000413545678"},{"@type":"NRID","@value":"9000283236777"},{"@type":"NRID","@value":"9000369724274"},{"@type":"NRID","@value":"9000001264229"},{"@type":"NRID","@value":"9000363409419"},{"@type":"NRID","@value":"9000363405373"},{"@type":"NRID","@value":"9000363492633"},{"@type":"NRID","@value":"9000363479352"},{"@type":"NRID","@value":"9000381494767"},{"@type":"NRID","@value":"9000305636951"},{"@type":"NRID","@value":"9000402246590"},{"@type":"NRID","@value":"9000257767689"},{"@type":"NRID","@value":"9000283593369"},{"@type":"NRID","@value":"9000363410533"},{"@type":"NRID","@value":"9000363410231"},{"@type":"NRID","@value":"9000363409847"},{"@type":"NRID","@value":"9000363407471"},{"@type":"NRID","@value":"9000363408093"},{"@type":"NRID","@value":"9000363479158"},{"@type":"NRID","@value":"9000242878032"},{"@type":"NRID","@value":"9000414812288"},{"@type":"NRID","@value":"9000283236870"},{"@type":"NRID","@value":"9000257767930"},{"@type":"NRID","@value":"9000415106034"},{"@type":"NRID","@value":"9000304608434"},{"@type":"NRID","@value":"9000363410856"},{"@type":"NRID","@value":"9000363410917"},{"@type":"NRID","@value":"9000363409412"},{"@type":"NRID","@value":"9000363403797"},{"@type":"NRID","@value":"9000363403843"},{"@type":"NRID","@value":"9000363408727"},{"@type":"NRID","@value":"9000363406640"},{"@type":"NRID","@value":"9000363407158"},{"@type":"NRID","@value":"9000363405988"},{"@type":"NRID","@value":"9000250464937"},{"@type":"NRID","@value":"9000312727740"},{"@type":"NRID","@value":"9000411562603"},{"@type":"NRID","@value":"9000363409424"},{"@type":"NRID","@value":"9000363405597"},{"@type":"NRID","@value":"9000363410123"},{"@type":"NRID","@value":"9000363406608"},{"@type":"NRID","@value":"9000363406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Masaki"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Atmosphere and Ocean Research Institute, The University of Tokyo"},{"@language":"en","@value":"Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001205223608704","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000257828194"}],"foaf:name":[{"@language":"en","@value":"Kitao Yushi"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Atmosphere and Ocean Research Institute, The University of Tokyo"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"13496476"}],"prism:publicationName":[{"@language":"en","@value":"SOLA"},{"@language":"en","@value":"SOLA"}],"dc:publisher":[{"@language":"en","@value":"Meteorological Society of Japan"},{"@language":"ja","@value":"公益社団法人 日本気象学会"}],"prism:publicationDate":"2013","prism:volume":"9","prism:number":"0","prism:startingPage":"129","prism:endingPage":"133"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"https://www.jstage.jst.go.jp/article/sola/9/0/9_2013-029/_pdf"}],"availableAt":"2013","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011142930420608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Diurnal Cycle of Precipitation in the Tropics Simulated in a Global Cloud-Resolving Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142935358592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Development of the minimal advanced treatments of surface interaction and runoff"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142940931072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A k-distribution-based radiation code and its computational optimization for an atmospheric general circulation model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146017395840","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modelling the diurnal cycle of deep precipitating convection over land with cloud‐resolving models and single‐column models"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617914861184","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Revolutionizing Climate Modeling with Project Athena: A Multi-Institutional, International Collaboration"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292618465712128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A planetary‐scale land–sea breeze circulation in East Asia and the western North Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092886054528","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A parametric model of vertical eddy fluxes in the 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China"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993853644416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Summer Precipitation Frequency, Intensity, and Diurnal Cycle over China: A Comparison of Satellite Data with Rain Gauge Observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995589019648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effects of Diurnal Cycle on a Simulated Asian Summer Monsoon"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369952857984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Diurnal Cycle of the Boundary Layer, Convection, Clouds, and Surface Radiation in a Coastal Monsoon Environment (Darwin, Australia)"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844179091072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Diurnal variation of precipitation over southeastern China: Spatial distribution and its seasonality"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845566973952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Scheme for Parameterizing Ice-Cloud Water Content in General Circulation Models"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318860616960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The TRMM Multisatellite Precipitation Analysis (TMPA): Quasi-Global, Multiyear, Combined-Sensor Precipitation Estimates at Fine Scales"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319765633920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"FY‐2C‐derived diurnal features of clouds in the southern contiguous China"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794468507392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Why Nocturnal Long-Duration Rainfall Presents an Eastward-Delayed Diurnal Phase of Rainfall down the Yangtze River Valley"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269802827776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Atmospheric water vapor transport associated with typical anomalous summer rainfall patterns in China"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206503972480","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A Stretched Icosahedral Grid by a New Grid Transformation"},{"@value":"A Stretched Icosahedral Grid by a New Grid Transformation(<Special Issue>The International Workshop on High-Resolution and Cloud Modeling, 2006)"},{"@value":"A stretched grid on a sphere by new grid transformation"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681480687744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"New Microphysical Schemes with Five and Six Categories by Diagnostic Generation of Cloud Ice"},{"@value":"New Microphysical Schemes with Five and Six Categories by Diagnostic Generation of Cloud Ice(<Special Issue>The International Workshop on High-Resolution and Cloud Modeling, 2006)"},{"@value":"New microphysics schemes with five and six categories by diagnostic generation of cloud ice"},{"@value":"New microphysics with five and six categories with diagnostic generation of cloud ice"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681480945792","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Development of an Improved Turbulence Closure Model for the Atmospheric Boundary Layer"},{"@value":"Improving high-impact numerical weather prediction with lidar and drone observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681482232192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Excitation of Deep Convection to the North of Tropical Storm Bebinca 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