{"@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/1390282680198001024.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2151/sola.2016-053"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/sola/12/0/12_2016-053/_pdf"}},{"identifier":{"@type":"NAID","@value":"130005249519"}}],"dc:title":[{"@language":"en","@value":"Resolution Dependence of the Diurnal Cycle of Precipitation Simulated by a Global Cloud-System Resolving Model"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"<p>Resolution dependence was found in the simulated diurnal precipitation cycle over land in the tropics. We conducted a series of grid refinement experiments of the atmosphere from 14 km to 0.87 km using a global high-resolution model without any convection parameterizations. In the high-resolution experiment, the peak of the cycle was earlier and precipitation at the peak was higher. The characteristics of the simulated diurnal precipitation cycle changed at a grid spacing of around 2-3 km. The precipitation started to increase in the morning in the high-resolution experiments, suggesting that small-scale moist convection became active in the late morning. In the lower-resolution experiments, convection and precipitation began in the late afternoon. As well as the enhancement of moisture transport from the boundary layer to the middle troposphere, the rapid formation of rain can also be attributed to the difference in diurnal precipitation cycles between lower and higher resolution experiments.</p>"}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420845751155228672","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"80451508"},{"@type":"NRID","@value":"1000080451508"},{"@type":"ORCID","@value":"0000-0002-2678-526X"},{"@type":"NRID","@value":"9000001341291"},{"@type":"NRID","@value":"9000404264071"},{"@type":"NRID","@value":"9000397856597"},{"@type":"NRID","@value":"9000266443984"},{"@type":"NRID","@value":"9000380963000"},{"@type":"NRID","@value":"9000412058313"},{"@type":"NRID","@value":"9000329440494"},{"@type":"NRID","@value":"9000399535622"},{"@type":"NRID","@value":"9000293836672"},{"@type":"NRID","@value":"9000345248255"},{"@type":"NRID","@value":"9000380461686"},{"@type":"NRID","@value":"9000410513235"},{"@type":"NRID","@value":"9000399535627"},{"@type":"NRID","@value":"9000399373123"},{"@type":"NRID","@value":"9000283593355"},{"@type":"NRID","@value":"9000368940158"},{"@type":"NRID","@value":"9000409848207"},{"@type":"NRID","@value":"9000406337145"},{"@type":"NRID","@value":"9000412113122"},{"@type":"NRID","@value":"9000330332131"},{"@type":"NRID","@value":"9000370254203"},{"@type":"NRID","@value":"9000263033114"},{"@type":"NRID","@value":"9000375855752"},{"@type":"NRID","@value":"9000345307956"},{"@type":"NRID","@value":"9000356660453"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/hisashiyashiro"}],"foaf:name":[{"@language":"en","@value":"Yashiro 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the Tibetan Plateau in a Mesoscale Model"},{"@value":"Resolution Dependency of the Diurnal Cycle of Convective Clouds over the Tibetan Plateau in a Mesoscale Model(<Special Issue>The International Workshop on High-Resolution and Cloud Modeling, 2006)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288145100928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"JAMSTEC Model Intercomparision Project (JMIP)"}]},{"@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/1390289920608016000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"On the Semidiurnal Variation in Surface Rainfall Rate over the Tropics in a Global Cloud-Resolving Model Simulation and Satellite Observations"},{"@language":"ja","@value":"全球雲解像モデル実験と衛星観測による熱帯域における地上降水強度の半日周期変動について"},{"@value":"On the Semidiurnal Variation in Surface Rainfall Rate over the Tropics in a Global Cloud-Resolving Model Simulation and Satellite Observations : Special Edition on DYAMOND : The DYnamics of the Atmospheric general circulation Modeled On Non-hydrostatic Domains"}]},{"@id":"https://cir.nii.ac.jp/crid/1390565134840505472","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Climate Statistics in Global Simulations of the Atmosphere, from 80 to 2.5 km Grid Spacing"},{"@language":"ja","@value":"格子間隔80kmから2.5kmの全球大気シミュレーションにおける気候統計量"},{"@value":"Special Edition on DYAMOND : The DYnamics of the Atmospheric general circulation Modeled On Non-hydrostatic Domains : Climate Statistics in Global Simulations of the Atmosphere, from 80 to 2.5 km Grid Spacing"}]},{"@id":"https://cir.nii.ac.jp/crid/1390567901489374720","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"An Energy Balance Model for Low--Level Clouds Based on a Simulation Resolving Mesoscale Motions"},{"@language":"ja","@value":"メソスケールの流れを解像したシミュレーションを基にした下層雲のエネルギー平衡モデルの構築"}]},{"@id":"https://cir.nii.ac.jp/crid/1390581766248779520","@type":"Article","resourceType":"学術雑誌論文(journal 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