{"@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/1360848655214820480.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/qj.2342"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.2342"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/qj.2342"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/qj.2342"}},{"identifier":{"@type":"URI","@value":"https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.2342"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Sensitivity of the atmospheric energy budget to two‐moment representation of cloud microphysics in idealized simulations of convective radiative quasi‐equilibrium"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Sensitivity of the atmospheric energy budget to two‐moment (2M) representation of cloud microphysics in idealized convective radiative quasi‐equilibrium (CRQE) is studied using partial and full 2M schemes. The focus is especially given to the sensitivity to 2M scheme for large hydrometeors. The atmospheric energy budget is found to be sensitive to the first indirect effect, but the energy budget is more sensitive to the 2M treatment for large hydrometeors. The top and bottom of atmosphere (TOA and BOA) energy budgets depend on 2M treatment especially for large ice hydrometeors (snow and graupel). The predicted number concentration of graupel dominates BOA energy budgets by increasing rain size leading to decrease of sensible heat flux, and that of snow dominates TOA energy budgets by enhancing updraught cloud mass flux in both low and middle clouds. In conclusion, the energy budgets are controlled not only by 2M representation of rain but also by representation of large ice hydrometeors. Sensitivity of the energy budget to 2M treatment for large ice hydrometeors is more significant than that for rain because the treatment impacts properties of surface heat fluxes and both low and mid‐level clouds.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420564276165247488","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"60512861"},{"@type":"NRID","@value":"1000060512861"},{"@type":"NRID","@value":"9000017574399"},{"@type":"NRID","@value":"9000003800408"},{"@type":"NRID","@value":"9000311488418"},{"@type":"NRID","@value":"9000006194041"},{"@type":"NRID","@value":"9000237754092"},{"@type":"NRID","@value":"9000283861715"},{"@type":"NRID","@value":"9000256250325"},{"@type":"NRID","@value":"9000250747895"},{"@type":"NRID","@value":"9000240186555"},{"@type":"NRID","@value":"9000242878138"},{"@type":"NRID","@value":"9000255771407"},{"@type":"NRID","@value":"9000256248763"},{"@type":"NRID","@value":"9000256249691"},{"@type":"NRID","@value":"9000241821354"},{"@type":"NRID","@value":"9000020564592"},{"@type":"NRID","@value":"9000255771118"},{"@type":"NRID","@value":"9000016857387"},{"@type":"NRID","@value":"9000022020981"},{"@type":"NRID","@value":"9000022748526"},{"@type":"NRID","@value":"9000397933197"},{"@type":"NRID","@value":"9000256250137"},{"@type":"NRID","@value":"9000255770474"},{"@type":"NRID","@value":"9000018177426"},{"@type":"NRID","@value":"9000021401829"},{"@type":"NRID","@value":"9000257768035"},{"@type":"NRID","@value":"9000309172781"},{"@type":"NRID","@value":"9000270296237"},{"@type":"NRID","@value":"9000288831538"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/yuyabbjp"}],"foaf:name":[{"@value":"Yuya Baba"}],"jpcoar:affiliationName":[{"@value":"Earth Simulator Center, Japan Agency for Marine–Earth Science and Technology  Yokohama Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00359009"},{"@type":"EISSN","@value":"1477870X"}],"prism:publicationName":[{"@value":"Quarterly Journal of the Royal Meteorological Society"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2014-03-21","prism:volume":"141","prism:number":"686","prism:startingPage":"114","prism:endingPage":"127"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://creativecommons.org/licenses/by-nc-nd/4.0/"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.2342"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/qj.2342"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/qj.2342"},{"@id":"https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.2342"}],"createdAt":"2014-02-05","modifiedAt":"2023-09-02","project":[{"@id":"https://cir.nii.ac.jp/crid/1040282257205386368","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"24760480"},{"@type":"JGN","@value":"JP24760480"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-24760480/"}],"notation":[{"@language":"ja","@value":"理想数値実験による都市内熱環境場に及ぼす河川・緑地・風況の影響評価"},{"@language":"en","@value":"Evaluation of effects of river, plant and wind on urban thermal environment using idealized numerical experiment"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011142938142336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Numerical Study of Convection Observed during the Winter Monsoon Experiment Using a Mesoscale Two-Dimensional Model"}]},{"@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/1360011143641952896","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A New Cloud Physics Parameterization in a Large-Eddy Simulation Model of Marine Stratocumulus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144316355456","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Weighted essentially non‐oscillatory scheme for cloud edge problem"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144335280512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Urban Aerosol Impacts on Downwind Convective Storms"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144360176768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Mesoscale and Microscale Structure and Organization of Clouds and Precipitation in Midlatitude Cyclones. 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