{"@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/1360588380154635776.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/b978-0-323-96026-7.00194-6"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:B9780323960267001946?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:B9780323960267001946?httpAccept=text/plain"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Convection-Permitting Climate Models"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380588380154635654","@type":"Researcher","foaf:name":[{"@value":"D. Takasuka"}]},{"@id":"https://cir.nii.ac.jp/crid/1380588380154636170","@type":"Researcher","foaf:name":[{"@value":"T. Miyakawa"}]},{"@id":"https://cir.nii.ac.jp/crid/1380588380154636164","@type":"Researcher","foaf:name":[{"@value":"A.F. Prein"}]},{"@id":"https://cir.nii.ac.jp/crid/1380588380154635652","@type":"Researcher","foaf:name":[{"@value":"D. Klocke"}]}],"publication":{"publicationIdentifier":[{"@type":"ISBN","@value":"9780124095489"}],"prism:publicationName":[{"@value":"Reference Module in Earth Systems and Environmental Sciences"}],"dc:publisher":[{"@value":"Elsevier"}],"prism:publicationDate":"2025"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license","https://doi.org/10.15223/policy-017","https://doi.org/10.15223/policy-037","https://doi.org/10.15223/policy-012","https://doi.org/10.15223/policy-029","https://doi.org/10.15223/policy-004"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:B9780323960267001946?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:B9780323960267001946?httpAccept=text/plain"}],"createdAt":"2025-04-15","modifiedAt":"2025-04-15","project":[{"@id":"https://cir.nii.ac.jp/crid/1040018351905270784","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"24K00707"},{"@type":"JGN","@value":"JP24K00707"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-24K00707/"}],"notation":[{"@language":"ja","@value":"熱帯の卓越気候変動と日本付近の顕著気象現象の結びつきを中長期変調させる要因は何か"},{"@language":"en","@value":"Decadal modulation of East Asian climate extremes tied to tropical climate variability"}]},{"@id":"https://cir.nii.ac.jp/crid/1040299826878724224","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23K22568"},{"@type":"JGN","@value":"JP23K22568"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23K22568/"}],"notation":[{"@language":"ja","@value":"北西太平洋モンスーンの変動に伴う大気海洋の熱収支変化の影響とその解像度依存性"},{"@language":"en","@value":"Impacts and resolution dependencies of air-sea heat budget fluctuation associated with the northwestern Pacific monsoon"}]},{"@id":"https://cir.nii.ac.jp/crid/1040582540341819648","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"24K22893"},{"@type":"JGN","@value":"JP24K22893"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-24K22893/"}],"notation":[{"@language":"ja","@value":"全球雲解像気候モデリングに基づく極端降水の温暖化応答とその階層構造の解明"},{"@language":"en","@value":"Global warming response of extreme rainfall and the associated hierarchical structure based on global cloud-resolving climate modeling"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050564289060608640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Application of a Monte Carlo integration method to collision and coagulation growth processes of hydrometeors in a bin‐type model"},{"@value":"Application of a Monte-Carlo integration method to collision and coagulation growth processes of hydrometeors in a bin-type model"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845760771110528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A Triggering Mechanism for Rapid Intensification of Tropical Cyclones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214552381568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deep moist atmospheric convection in a subkilometer global simulation"}]},{"@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/1360011142933994112","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Madden-Julian Oscillation Event Realistically Simulated by a Global Cloud-Resolving Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142935298688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A new dynamical framework of nonhydrostatic global model using the icosahedral grid"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142937043584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Development of a turbulence closure model for geophysical fluid problems"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142938607360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A cloud resolving model as a cloud parameterization in the NCAR Community Climate System Model: Preliminary results"}]},{"@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/1360011143929113984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Time-Splitting Methods for Elastic Models Using Forward Time Schemes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144378636288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Orogenic Propagating Precipitation Systems over the United States in a Global Climate Model with Embedded Explicit Convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144481678720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Simulation of Effects of Atmospheric Aerosols on Deep Turbulent Convective Clouds Using a Spectral Microphysics Mixed-Phase Cumulus Cloud Model. Part I: Model Description and Possible Applications"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145439899264","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modeled Impact of Anthropogenic Warming on the Frequency of Intense Atlantic Hurricanes"}]},{"@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/1360013171861892352","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Value of High-Resolution Met Office Regional Climate Models in the Simulation of Multihourly Precipitation Extremes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016866668365056","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Diagnosing ocean feedbacks to the MJO: SST‐modulated surface fluxes and the moist static energy budget"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017285914956288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Possible Role of the Diurnal Cycle in Land Convection in the Barrier Effect on the MJO by the Maritime Continent"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017286825730304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Eddy Diffusivity and Countergradient Transport in the Convective Atmospheric Boundary Layer"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021390748505088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Numerical Accuracy Necessary for Large-Eddy Simulation of Planetary Boundary Layer Turbulence Using the Discontinuous Galerkin Method"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025034149813760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Forecasting Convection with a “Scale-Aware” Tiedtke Cumulus Parameterization Scheme at Kilometer Scales"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025437724172672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Implementation of an Urban Parameterization Scheme into the Regional Climate Model COSMO-CLM"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025437724708608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A colorful look at climate sensitivity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025439361204992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evaluation of five global AI models for predicting weather in Eastern Asia and Western Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283689328037120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Madden‐Julian Oscillation event remotely accelerates ocean upwelling to abruptly terminate the 1997/1998 super El Niño"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617507624704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Advanced risk-based event attribution for heavy regional rainfall events"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617910129536","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A review on regional convection‐permitting climate modeling: Demonstrations, prospects, and challenges"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617913233152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Description of Global-Scale Circulation Cells in the Tropics with a 40–50 Day Period"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617913239936","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evaluation of Precipitating Hydrometeor Parameterizations in a Single-Moment Bulk Microphysics Scheme for Deep Convective Systems over the Tropical Central Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617914062848","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Reanalysis of Ocean Climate Using Simple Ocean Data Assimilation (SODA)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619535332608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modulation of the boreal wintertime Madden‐Julian oscillation by the stratospheric quasi‐biennial oscillation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620978536960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Seasonal Cycle over the Tropical Pacific in Coupled Ocean–Atmosphere General Circulation Models"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620979957632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evaluating Mesoscale NWP Models Using Kinetic Energy Spectra"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621370397952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Enhanced future changes in wet and dry extremes over Africa at convection-permitting scale"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298343108984064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Resolved Convection Improves the Representation of Equatorial Waves and Tropical Rainfall Variability in a Global Nonhydrostatic Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302864773616640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Asymptotic Matching between Weather and Climate Models"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302867633960064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The influence of convection-permitting regional climate modeling on future projections of extreme precipitation: dependency on topography and timescale"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306912713657216","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Spatial and Temporal Characteristics of Summer Precipitation over Central Europe in a Suite of High-Resolution Climate Models"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567186511655168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Influence of the Stratospheric Quasi-Biennial Oscillation on the Madden–Julian Oscillation during Austral Summer"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092883017600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Predicting the morphology of ice particles in deep convection using the super-droplet method: development and evaluation of SCALE-SDM 0.2.5-2.2.0, -2.2.1, and -2.2.2"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092886865024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The <scp>ICON</scp> (ICOsahedral Non‐hydrostatic) modelling framework of <scp>DWD</scp> and <scp>MPI‐M</scp>: Description of the non‐hydrostatic dynamical core"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092887466240","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Cumulus Parameterization with State-Dependent Entrainment Rate. Part I: Description and Sensitivity to Temperature and Humidity Profiles"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092889126528","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Aerosol Effects of the Condensation Process on a Convective Cloud Simulation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092894054400","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The impact of horizontal resolution on the simulations of convective development over land"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092894767104","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tropical Cyclone Minimum Sea Level Pressure/Maximum Sustained Wind Relationship for the Western North Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092894774016","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Environmental Factors Contributing to Tropical Cyclone Genesis over the Western North Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574093720960896","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evaluation of the convection-resolving regional climate modeling approach in decade-long simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094381297536","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Detailed Microphysical Model Within a Two-Dimensional Dynamic Framework: Model Description and Preliminary Results"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095132429440","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Responses of Tropical and Subtropical High-Cloud Statistics to Global Warming"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095323657088","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effects of Horizontal and Vertical Grid Spacing on Mixing in Simulated Squall Lines and Implications for Convective Strength and Structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095350741120","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Resolution Dependence of Explicitly Modeled Convective Systems"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095530709632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An Efficient Numerical Solution to the Stochastic Collection Equation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095835308032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Cloud‐aerosol interactions for boundary layer stratocumulus in the Lagrangian Cloud Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096047042176","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Single Precision in the Dynamical Core of a Nonhydrostatic Global Atmospheric Model: Evaluation Using a Baroclinic Wave Test Case"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584344407903744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Learning skillful medium-range global weather forecasting"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588381080632704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A protocol and analysis of year-long simulations of global storm-resolving models and beyond"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588383702701056","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Climate Change Feedbacks in Aquaplanet Experiments With Explicit and Parametrized Convection for Horizontal Resolutions of 2,525 Up to 5 km"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588384967087360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"“Gray Zone” Simulations Using a Three-Dimensional Planetary Boundary Layer Parameterization in the Weather Research and Forecasting Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588385277369856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Real-Time Ultrafinescale Forecast Support during the Special Observing Period of the MAP"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588386544616192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Importance of Regional Climate Model Grid Spacing for the Simulation of Heavy Precipitation in the Colorado Headwaters"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588388465578624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modelling strategies for performing convection-permitting climate simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588388465637504","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Scale Awareness, Resolved Circulations, and Practical Limits in the MYNN–EDMF Boundary Layer and Shallow Cumulus Scheme"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588388979381504","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Convection‐permitting models: a step‐change in rainfall forecasting"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848661487857280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modeling of Cloud Microphysics: Can We Do Better?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567863731200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Nonhydrostatic icosahedral atmospheric model (NICAM) for global cloud resolving simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567865828736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Climatology of Atmospheric Wavenumber Spectra of Wind and Temperature Observed by Commercial Aircraft"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567870994304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global Cloud-Resolving Models"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855568555359104","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"SIMULATED CLIMATOLOGY OF A GENERAL CIRCULATION MODEL WITH A HYDROLOGIC CYCLE<sup>1</sup>"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855568697097472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Impact of Model Resolution on Tropical Cyclone Simulation Using the HighResMIP–PRIMAVERA Multimodel Ensemble"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855568890269696","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Climatological Skill of a Regional Model over Complex Terrain"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569125990016","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Impact of Graupel Parameterization Schemes on Idealized Bow Echo Simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569495649152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Simulation of Three-Dimensional Convective Storm Dynamics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569858298496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Simulation of an Evolving Convective Boundary Layer Using a Scale-Dependent Dynamic Smagorinsky Model at Near-Gray-Zone Resolutions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570138817792","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Northward Propagation Mechanisms of the Boreal Summer Intraseasonal Oscillation in the ERA-Interim and SP-CCSM"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570153326208","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Intraseasonal Variability in a Cloud-Permitting Near-Global Equatorial Aquaplanet Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570402768512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"GENERAL CIRCULATION EXPERIMENTS WITH THE PRIMITIVE EQUATIONS"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570564325760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A simple model of the atmospheric boundary layer; sensitivity to surface evaporation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570681832448","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Towards climate simulations at cloud-resolving scales"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570729900800","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The simulation of the diurnal cycle of convective precipitation over land in a global model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571440086400","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Met Office Unified Model Global Atmosphere 7.0/7.1 and JULES Global Land 7.0 configurations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857598078557312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The double ITCZ bias in CMIP5 models: interaction between SST, large-scale circulation and precipitation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707130720512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Climate of High-obliquity Exoterrestrial Planets with a Three-dimensional Cloud System Resolving Climate Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707357317632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Large Ensemble Simulation for Investigating Predictability of Precursor Vortices of Typhoon Faxai in 2019 With a 14‐km Mesh Global Nonhydrostatic Atmospheric Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861711811759104","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Monsoons, ITCZs, and the Concept of the Global Monsoon"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861714256871680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Near-Surface Wind Convergence over the Gulf Stream—The Role of SST Revisited"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865818732606208","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Mixed Scheme for Subgrid-Scale Fluxes in Cloud-Resolving Models"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869858642843520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Local impact analysis of climate change on precipitation extremes: are high-resolution climate models needed for realistic simulations?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869861494067712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modeling soil moisture‐precipitation feedback in the Sahel: Importance of spatial scale versus convective parameterization"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869862381711104","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Changes in weather extremes: Assessment of return values using high resolution climate simulations at convection-resolving scale"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869862381787392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Second-Order Bulk Boundary-Layer Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869862382267392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Improving the representation of shallow cumulus convection with the simplified-higher-order-closure–mass-flux (SHOC+MF v1.0) approach"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869862676207104","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tropical cyclones in climate models"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044884772992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Structure and Evolution of Mesoscale Convective Systems: Sensitivity to Cloud Microphysics in Convection‐Permitting Simulations Over the United States"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045273507328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Aspects of the diurnal cycle in a regional climate model"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045540667264","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A framework for testing global non‐hydrostatic models"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045872048384","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Particle Growth and Drop Collection Efficiency of Warm Clouds as Inferred from Joint CloudSat and MODIS Observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518496619520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Breaking the Cloud Parameterization Deadlock"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518760068736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Über ein Variationsprinzip zur Lösung von Dirichlet-Problemen bei Verwendung von Teilräumen, die keinen Randbedingungen unterworfen sind"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518876210816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Resolution Requirements for the Simulation of Deep Moist Convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519524518656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Simulation of a Convective Cloud in a 3-D Model With Explicit Microphysics. Part I: Model Description and Sensitivity Experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520155764864","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Entrainment in Cumulus Clouds: What Resolution is Cloud-Resolving?"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520182466304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The potential impacts of pollution on a nondrizzling stratus deck: Does aerosol number matter more than type?"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520446772480","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"QBO‐MJO Connection"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520621585536","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Numerical Investigation of the Organization and Interaction of the Convective and Stratiform Regions of Tropical Squall Lines"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520843859200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Combined Eddy-Diffusivity Mass-Flux Approach for the Convective Boundary Layer"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520971129088","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Cramming more components onto integrated circuits, Reprinted from Electronics, volume 38, number 8, April 19, 1965, pp.114 ff."}]},{"@id":"https://cir.nii.ac.jp/crid/1361418521151304192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Subseasonal Weather Prediction in a Global Convection-Permitting Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993724103552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"HEALPix: A Framework for High‐Resolution Discretization and Fast Analysis of Data Distributed on the Sphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994471185664","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Turbulence Closure Parameterization and Grid Spacing Effects in Simulated Supercell Storms"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994895187328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An Extended Eddy‐Diffusivity Mass‐Flux Scheme for Unified Representation of Subgrid‐Scale Turbulence and Convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995213229952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Representation of the Subgrid-Scale Turbulent Transport in Convective Boundary Layers at Gray-Zone Resolutions"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995309291520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A new method for large-eddy simulations of clouds with Lagrangian droplets including the effects of turbulent collision"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995525826688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the numerical simulation of buoyant convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995546245632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Simulation of Indian summer monsoon intraseasonal oscillations in a superparameterized coupled climate model: need to improve the embedded cloud resolving model"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995599499520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Resolving Tropical Cyclone Intensity in Models"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995936339840","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Temperature response to future urbanization and climate change"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995978066176","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Theory for Strong, Long-Lived Squall Lines"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470016604928","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Regional Dynamical Downscaling and the CORDEX Initiative"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470465506944","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Storm track response to ocean fronts in a global high-resolution climate model"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470975550976","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Horizontal Kinetic Energy Spectrum and Spectral Budget Simulated by a High-Resolution Troposphere–Stratosphere–Mesosphere GCM"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943368518656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Double‐ITCZ Bias in CMIP3, CMIP5, and CMIP6 Models Based on Annual Mean Precipitation"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943790844032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Sensitivity of Numerically Simulated Cyclic Mesocyclogenesis to Variations in Model Physical and Computational Parameters"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943967705088","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The vertical distribution of wind and turbulent exchange in a neutral atmosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944161410688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Atmospheric Kinetic Energy Spectra from Global High-Resolution Nonhydrostatic Simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945607399040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Process-Oriented MJO Simulation Diagnostic: Moisture Sensitivity of Simulated Convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544418769021312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Improving High-Resolution Weather Forecasts Using the Weather Research and Forecasting (WRF) Model with an Updated Kain–Fritsch Scheme"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419549450496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Elements of the Microphysical Structure of Numerically Simulated Nonprecipitating Stratocumulus"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420139090688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Role of Cloud Microphysics Parameterization in the Simulation of Mesoscale Convective System Clouds and Precipitation in the Tropical Western Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420518788608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Toward Numerical Modeling in the “Terra Incognita”"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544421046757760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Parameterization of Dry Thermals and Shallow Cumuli for Mesoscale Numerical Weather Prediction"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894329340288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Mass-Flux Cumulus Parameterization Scheme across Gray-Zone Resolutions"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894786636416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"CRCP: a Cloud Resolving Convection Parameterization for modeling the tropical convecting atmosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895223226368","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Double-ITCZ Problem in IPCC AR4 Coupled GCMs: Ocean–Atmosphere Feedback Analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895248037888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Physical mechanisms controlling self‐aggregation of convection in idealized numerical modeling simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825896156319360","@type":"Article","resourceType":"preprint","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6)  experimental design and organization"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825896261999104","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rain Reevaporation, Boundary Layer–Convection Interactions, and Pacific Rainfall Patterns in an AGCM"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825896328941440","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Dynamical Downscaling Projections of Twenty-First-Century Atlantic Hurricane Activity: CMIP3 and CMIP5 Model-Based Scenarios"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368878095360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stratospheric Control of the Madden–Julian Oscillation"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368895125888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An eddy‐diffusivity/mass‐flux parametrization for dry and shallow cumulus convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369418962176","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-Dimensional Evolution of Simulated Long-Lived Squall Lines"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369551624192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Energy Cascade in Large-Eddy Simulations of Turbulent Fluid Flows"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370022048256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Diagnostic for Evaluating the Representation of Turbulence in Atmospheric Models at the Kilometric Scale"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370357629568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Implementation of a Nonlinear Subfilter Turbulence Stress Model for Large-Eddy Simulation in the Advanced Research WRF Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370535652352","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Four Theories of the Madden‐Julian Oscillation"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107371049283584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The natural tendency towards symmetry of motion and its application as a principle in meteorology"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843238740224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evidence far a<i>k</i><sup>−5/3</sup>Law Inertial Range in Mesoscale Two-Dimensional Turbulence"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843297217920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Numerical Simulation of Warm Rain Development in an Axisymmetric Cloud Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843719581440","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Grid-Refinement-Based Approach for Modeling the Convective Boundary Layer in the Gray Zone: Algorithm Implementation and Testing"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843817337984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Quantifying and improving sub‐grid diffusion in the boundary‐layer grey zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843971353856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Operational Convective-Scale Numerical Weather Prediction with the COSMO Model: Description and Sensitivities"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844230683392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional numerical study of the height and mean structure of a heated planetary boundary layer"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844396388736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Soil Moisture–Precipitation Feedback in Simulations with Explicit and Parameterized Convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844397805440","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sensitivity of a Simulated Squall Line to Horizontal Resolution and Parameterization of Microphysics"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844503806464","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Terrain-Following Coordinate with Smoothed Coordinate Surfaces"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844691397248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Quantitative precipitation forecasting in the Alps: The advances achieved by the Mesoscale Alpine Programme"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844751391488","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Numerical Modeling of the Dynamics and Microphysics of Warm Cumulus Convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845109278592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Realism of Rainfall in a Very High-Resolution Regional Climate Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319523956864","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Cumulus Parameterization with State-Dependent Entrainment Rate. Part II: Impact on Climatology in a General Circulation Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319790389504","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Using Machine Learning to Parameterize Moist Convection: Potential for Modeling of Climate, Climate Change, and Extreme Events"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320795466240","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tropical Cyclone Intensity Errors Associated with Lack of Two-Way Ocean Coupling in High-Resolution Global Simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320881376896","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A large‐eddy model for cirrus clouds with explicit aerosol and ice microphysics and Lagrangian ice particle tracking"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670321133509632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Advances in simulating atmospheric variability with the ECMWF model: From synoptic to decadal time‐scales"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794424144128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Numerical Study on the Extreme Intensification of Hurricane Patricia (2015)"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794524757632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Observed and model‐simulated diurnal cycles of precipitation over the contiguous United States"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794635492224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A proposal for a redefinition of the turbulent stresses in the filtered Navier–Stokes equations"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795399183616","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Structure of the Madden–Julian Oscillation in the Superparameterized CAM"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269425700864","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Meso-NH Atmospheric Simulation System. Part I: adiabatic formulation and control simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635392","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Pangu-Weather: a 3D high-resolution model for fast and accurate global weather forecast"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635394","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"How can we improve the seamless representation of climatological statistics and weather toward reliable global K-scale climate simulations?"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635396","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effects of horizontal and vertical grid spacing on mixing in simulated squall lines and implications for convective strength and structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635397","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Altitude dependency of future snow cover changes over Central Japan evaluated by a regional climate model"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635406","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the distribution and continuity of water substance in atmospheric circulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635408","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sampling of the structure of turbulence: implications for parameterizations at sub-kilometric scales"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635521","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rediscovery of the doldrums in storm-resolving simulations over the tropical Atlantic"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635524","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tackling errors toward realistic seamless representation in kilometer-scale climate simulations with NICAM"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635528","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"nextGEMS: output of the production simulations for ICON and IFS"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635532","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effects of horizontal resolution, domain size, boundary conditions, and surface heterogeneity on coarse LES of a convective boundary layer"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635543","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Emulation of cloud microphysics in a climate model"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635557","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"SwinRDM: integrate swinRNN with diffusion model towards high-resolution and high-quality weather forecasting"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635558","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Insights into low-latitude cloud feedbacks from high-resolution models"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635562","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Influence of submesoscale topography on daytime precipitation associated with thermally driven local circulations over a mountainous region"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635658","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Large eddy simulation of the atmosphere on various scales"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635660","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Convection-permitting simulations with the E3SM global atmosphere model"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635664","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Dynamical imprints on precipitation cluster statistics across a hierarchy of high-resolution simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635672","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Clouds and convective self-aggregation in a multimodel ensemble of radiative-convective equilibrium simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635784","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The atmospheric boundary layer and the “gray zone” of turbulence: a critical review"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635787","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Climate change 2023: Synthesis report"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635791","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"ENSO and QBO controls the favorableness of the MJO realization cooperatively"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635797","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A short history of the PBL parameterization at ECMWF"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635805","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A comparison of explicit and implicit predictions of convective and stratiform precipitating weather systems with a meso-β-scale numerical model"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635911","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Machine learning emulation of gravity wave drag in numerical weather forecasting"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635915","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional plane- tary boundary layer parameterization for high-resolution meso- scale simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635931","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"nextGEMS: entering the era of kilometer-scale Earth system modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635932","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Triangular mesh methods for the neutron transport equation"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635933","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Destination Earth – a digital twin in support of climate services"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154635945","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Progress in digital integrated electronics"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154636032","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Pan-European climate at convection-permitting scale: a model intercomparison study"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154636035","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An inter-comparison of icosahedral climate models on the G8 call: ICOMEX project"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154636039","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Numerical solutions for the shape-preserving two-dimensional convection element"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154636040","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tropical cyclones in global storm-resolving models"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154636042","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Fourcastnet: a global data-driven high-resolution weather model using adaptive Fourier neural operators"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154636051","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A numerical investigation of an orogenic mesoscale convective system"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154636052","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Increasing horizontal resolution in numerical weather prediction and climate simulations: illusion or panacea?"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154636053","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Benefit of convection permitting climate model simulations in the representation of convective precipitation"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154636055","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Numerical accuracy of advection scheme necessary for large-eddy simulation of planetary boundary layer turbulence"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154636061","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Land surface model spin-up behavior in the North American land data assimilation system (NLDAS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154636062","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tropicalcyclones and equatorial waves in aconvection-permitting aquaplanetsimulation with off-equatorial SST maximum"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154636065","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Large-eddy simulation of maritime deep tropical convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154636160","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Predicting atmospheric optical properties for radiative transfer computations using neural networks"}]},{"@id":"https://cir.nii.ac.jp/crid/1370588380154636170","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Differences in the cloud, precipitation, and convection representation between the global sub-km mesh simulation and km simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206504122752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"孤立した対流雲の力学的•微物理学的変化の数値モデリング"},{"@language":"en","@value":"Numerical Modeling of Dynamical and Microphysical Evolution of an Isolated Convective Cloud"},{"@value":"Numerical modeling of dynamical and microphysical evolution of an isolated convective cloud—The 19 July 1981 CCOPE cloud"},{"@value":"Numerical modeling of dynamical and microphysical evolution of an isolated convective cloud: the 19 July 1981 CCOPE cloud"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206506494976","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"湿潤対流をシミュレートする場合の静水圧モデルと非静水圧モデルとの比較実験"},{"@language":"en","@value":"Hydrostatic and Non-Hydrostatic Simulations of Moist Convection"},{"@value":"Hydrostatic and non-hydrostatic simulation of moist convection: the applicability of hydrostatic approximation to a high-resolution model"}]},{"@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/1390282681481473792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A 20-Year Climatology of a NICAM AMIP-Type Simulation"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763121592064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Resolution Dependencies of Tropical Convection in a Global Cloud/Cloud-System Resolving Model"},{"@value":"NOTES and CORRESPONDENCE : Resolution Dependencies of Tropical Convection in a Global Cloud/Cloud-System Resolving Model"},{"@value":"Resolution sensitivity of cloud features in organized convection in a global cloud/cloud-system resolving model"}]},{"@id":"https://cir.nii.ac.jp/crid/1390287297546738816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Analysis of Systematic Error in Numerical Weather Prediction of Coastal Fronts in Japan's Kanto Plain"},{"@language":"ja","@value":"日本の関東平野に発生する沿岸前線にみられる系統的な数値予報誤差の解析"}]},{"@id":"https://cir.nii.ac.jp/crid/1390570699998594048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Boreal Summer Intraseasonal Oscillation (BSISO): A Review"},{"@language":"ja","@value":"北半球夏季季節内変動（BSISO）：レビュー"},{"@value":"The boreal summer intraseasonal oscillation: A review"}]},{"@id":"https://cir.nii.ac.jp/crid/1390859238004200064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Flux Adjustment on Seasonal-Scale Sea Surface Temperature Drift in NICOCO"},{"@language":"ja","@value":"NICOCOにおける季節スケールの海面水温ドリフトに対するフラックス調節手法"}]},{"@id":"https://cir.nii.ac.jp/crid/1571698601430777088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The super-droplet method for the numerical simulation of clouds and precipitation : a particle-based and probabilistic microphysics model coupled with a non-hydrostatic model"},{"@value":"The super-droplet method for the numerical simulation of clouds and precipitation"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266975406976","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"DYAMOND : the DYnamics of the Atmospheric general circulation Modeled On Non-hydrostatic Domains"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/b978-0-323-96026-7.00194-6"},{"@type":"KAKEN","@value":"PRODUCT-25648232"},{"@type":"KAKEN","@value":"PRODUCT-25830378"},{"@type":"KAKEN","@value":"PRODUCT-25599704"}]}