{"@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/1050869445406529792.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"HDL","@value":"http://hdl.handle.net/2433/298378"}},{"identifier":{"@type":"DOI","@value":"10.1002/asl.1286"}},{"identifier":{"@type":"URI","@value":"https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/asl.1286"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@language":"en","@value":"Raindrop size distribution variability associated with size-dependent advection in convective precipitation systems"},{"@value":"Raindrop size distribution variability associated with size‐dependent advection in convective precipitation systems"}],"dc:language":"en","description":[{"type":"Abstract","notation":[{"@language":"en","@value":"Raindrop size distribution (DSD) is fundamental for understanding precipitation processes. This study utilized a two-dimensional simulation with bin cloud microphysics parameterizations to investigate the spatiotemporal variability of DSDs owing to the influence of mesoscale circulation associated with the precipitation system. The simulated multicellular convection went through developing, mature, and dissipating stages, with updraft weakening and rainfall area expanding through these stages. The width of the DSD narrowed as rainfall weakened. In addition, a significant bimodal DSD was observed during the dissipating stage. Furthermore, we investigated the spatial distribution of the number density of raindrops corresponding to the maximum, local minimum, and local maximum of the significant bimodal DSD in the dissipating stage. According to the results, the raindrops constituting the maximum, local minimum, and local maximum followed different advection processes. This size-dependent advection effect may have contributed to the bimodal DSD formation."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1070869445406529793","@type":"Researcher","foaf:name":[{"@language":"en","@value":"Okazaki, Megumi"}]},{"@id":"https://cir.nii.ac.jp/crid/1420564276179743232","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"90551383"},{"@type":"NRID","@value":"1000090551383"},{"@type":"ORCID","@value":"0000-0002-0885-169X"},{"@type":"NRID","@value":"9000016856549"},{"@type":"NRID","@value":"9000019191762"},{"@type":"NRID","@value":"9000347224269"},{"@type":"NRID","@value":"9000258524664"},{"@type":"NRID","@value":"9000347187303"},{"@type":"NRID","@value":"9000254329090"},{"@type":"NRID","@value":"9000411218498"},{"@type":"NRID","@value":"9000375915416"},{"@type":"NRID","@value":"9000414514942"},{"@type":"NRID","@value":"9000258523751"},{"@type":"NRID","@value":"9000382634026"},{"@type":"NRID","@value":"9000345210914"},{"@type":"NRID","@value":"9000310333546"},{"@type":"NRID","@value":"9000414515105"},{"@type":"NRID","@value":"9000410756298"},{"@type":"NRID","@value":"9000410756261"},{"@type":"NRID","@value":"9000402255399"},{"@type":"NRID","@value":"9000405671826"},{"@type":"NRID","@value":"9000405671816"},{"@type":"NRID","@value":"9000258524330"},{"@type":"NRID","@value":"9000319056774"},{"@type":"NRID","@value":"9000414515068"},{"@type":"NRID","@value":"9000404541246"},{"@type":"NRID","@value":"9000258523981"},{"@type":"NRID","@value":"9000258266379"},{"@type":"NRID","@value":"9000347187308"},{"@type":"NRID","@value":"9000258522946"},{"@type":"NRID","@value":"9000375904852"},{"@type":"NRID","@value":"9000405666678"},{"@type":"NRID","@value":"9000405671823"},{"@type":"NRID","@value":"9000404629246"},{"@type":"NRID","@value":"9000336038518"},{"@type":"NRID","@value":"9000284633979"},{"@type":"NRID","@value":"9000314383775"},{"@type":"NRID","@value":"9000258523517"},{"@type":"NRID","@value":"9000414515094"},{"@type":"NRID","@value":"9000405666634"},{"@type":"NRID","@value":"9000258522240"},{"@type":"NRID","@value":"9000415324148"},{"@type":"NRID","@value":"9000411205210"},{"@type":"NRID","@value":"9000258523745"},{"@type":"NRID","@value":"9000258522747"},{"@type":"NRID","@value":"9000258523608"},{"@type":"NRID","@value":"9000237871208"},{"@type":"NRID","@value":"9000399373351"},{"@type":"NRID","@value":"9000257828015"},{"@type":"NRID","@value":"9000254826622"},{"@type":"NRID","@value":"9000258522368"},{"@type":"NRID","@value":"9000254825425"},{"@type":"NRID","@value":"9000409182568"},{"@type":"NRID","@value":"9000321630146"},{"@type":"NRID","@value":"9000412366118"},{"@type":"NRID","@value":"9000412112723"},{"@type":"NRID","@value":"9000254959844"},{"@type":"NRID","@value":"9000411272205"},{"@type":"NRID","@value":"9000415324157"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/7000008789"}],"foaf:name":[{"@language":"en","@value":"Yamaguchi, Kosei"}]},{"@id":"https://cir.nii.ac.jp/crid/1070869445406529794","@type":"Researcher","foaf:name":[{"@language":"en","@value":"Yanase, Tomoro"}]},{"@id":"https://cir.nii.ac.jp/crid/1070869445406529792","@type":"Researcher","foaf:name":[{"@language":"en","@value":"Nakakita, Eiichi"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"1530261X"},{"@type":"PISSN","@value":"1530261X"}],"prism:publicationName":[{"@language":"en","@value":"Atmospheric Science Letters"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2025-01","prism:volume":"26","prism:number":"1"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["© 2025 The Author(s). Atmospheric Science Letters published by John Wiley & Sons Ltd on behalf of Royal Meteorological Society.","This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited."],"url":[{"@id":"https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/asl.1286"}],"foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=advection","dc:title":"advection"},{"@id":"https://cir.nii.ac.jp/all?q=bimodal","dc:title":"bimodal"},{"@id":"https://cir.nii.ac.jp/all?q=multicellular%20convection","dc:title":"multicellular convection"},{"@id":"https://cir.nii.ac.jp/all?q=raindrop%20size%20distribution","dc:title":"raindrop size distribution"}],"dcterms:subject":[{"subjectScheme":"Other","notation":[{"@language":"en","@value":"advection"}]},{"subjectScheme":"Other","notation":[{"@language":"en","@value":"bimodal"}]},{"subjectScheme":"Other","notation":[{"@language":"en","@value":"multicellular convection"}]},{"subjectScheme":"Other","notation":[{"@language":"en","@value":"raindrop size distribution"}]}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040862931497062272","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"24KJ1368"},{"@type":"JGN","@value":"JP24KJ1368"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-24KJ1368/"}],"notation":[{"@language":"ja","@value":"層状・対流混合降水系がもたらす粒径分布の立体的時間発展の解明"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001339107202304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A Study of Microphysical Mechanisms for Correlation Patterns between Droplet Radius and Optical Thickness of Warm Clouds with a Spectral Bin Microphysics Cloud Model"},{"@value":"A study of microphysical mechanisms for correlation patterns between droplet radius and optical thickness of warm clouds with a spectral bin microphysics model"}]},{"@id":"https://cir.nii.ac.jp/crid/1050860842077905152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"An analytical representation of raindrop size distribution in a mixed convective and stratiform precipitating system as revealed by field observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144390375296","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Impact of Size Sorting on the Polarimetric Radar Variables"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017287007738624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Comparison of Convective Raindrop Size Distributions in the Eyewall and Spiral Rainbands of Typhoon Lekima (2019)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360286993150557952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Confronting the Challenge of Modeling Cloud and Precipitation Microphysics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617915184384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An Improved Mellor–Yamada Level-3 Model: Its Numerical Stability and Application to a Regional Prediction of Advection Fog"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619041121536","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A New Representation of Collision-Induced Breakup of Raindrops and Its Implications for the Shapes of Raindrop Size Distributions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619940408064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Microphysics of Raindrop Size Spectra: Tropical Continental and Maritime Storms"}]},{"@id":"https://cir.nii.ac.jp/crid/1360303973288449152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evolution of drop size distribution in natural rain"}]},{"@id":"https://cir.nii.ac.jp/crid/1360564063944541568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Collision, Coalescence and Breakup of Raindrops. 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