{"@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/1360853567796982016.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2020gl088763"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GL088763"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2020GL088763"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2020GL088763"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"New Critical Length for the Onset of Self‐Aggregation of Moist Convection"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Convective self‐aggregation (CSA) in an idealized modeling framework is key to understanding the role of clouds. To investigate the existence of characteristic length of CSA onset, we conducted systematic cloud‐resolving simulations, with a scope covering the horizontal domain size and resolution. In the high‐resolution simulation, CSA can occur with a square domain larger than ~500 km. Based on the competition between two near‐surface horizontal divergent flows, we discuss the characteristic length existence. While the flow induced by radiative cooling in the subsidence region acts as positive feedback for moisture perturbation and scales with the domain size, the other flow induced by evaporative cooling of falling rain in the convective region acts as negative feedback and does not scale. The study suggests characteristic length existence for the organization of moist convection, even in real‐world conditions.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380853567796982147","@type":"Researcher","foaf:name":[{"@value":"Tomoro Yanase"}],"jpcoar:affiliationName":[{"@value":"RIKEN Center for Computational Science Kobe Japan"},{"@value":"Disaster Prevention Research Institute Kyoto University Kyoto Japan"},{"@value":"Graduate School of Science Kyoto University Kyoto Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1420845751150736640","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"40447892"},{"@type":"NRID","@value":"1000040447892"},{"@type":"NRID","@value":"9000240186658"},{"@type":"NRID","@value":"9000405665222"},{"@type":"NRID","@value":"9000242878755"},{"@type":"NRID","@value":"9000018337112"},{"@type":"NRID","@value":"9000346964632"},{"@type":"NRID","@value":"9000380963005"},{"@type":"NRID","@value":"9000250471920"},{"@type":"NRID","@value":"9000249538173"},{"@type":"NRID","@value":"9000380962994"},{"@type":"NRID","@value":"9000329440487"},{"@type":"NRID","@value":"9000399535618"},{"@type":"NRID","@value":"9000293836671"},{"@type":"NRID","@value":"9000380461682"},{"@type":"NRID","@value":"9000410513234"},{"@type":"NRID","@value":"9000242878546"},{"@type":"NRID","@value":"9000408953286"},{"@type":"NRID","@value":"9000399535626"},{"@type":"NRID","@value":"9000270296153"},{"@type":"NRID","@value":"9000258444887"},{"@type":"NRID","@value":"9000287286151"},{"@type":"NRID","@value":"9000283593354"},{"@type":"NRID","@value":"9000363501296"},{"@type":"NRID","@value":"9000409848208"},{"@type":"NRID","@value":"9000409848203"},{"@type":"NRID","@value":"9000270296136"},{"@type":"NRID","@value":"9000359884902"},{"@type":"NRID","@value":"9000288830800"},{"@type":"NRID","@value":"9000250465235"},{"@type":"NRID","@value":"9000263033113"},{"@type":"NRID","@value":"9000375855751"},{"@type":"NRID","@value":"9000237754482"},{"@type":"NRID","@value":"9000270296004"},{"@type":"NRID","@value":"9000288830792"},{"@type":"NRID","@value":"9000345307954"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/seiya_ni"}],"foaf:name":[{"@value":"Seiya Nishizawa"}],"jpcoar:affiliationName":[{"@value":"RIKEN Center for Computational Science Kobe Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1420001326223926656","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"70415991"},{"@type":"NRID","@value":"1000070415991"},{"@type":"NRID","@value":"9000363489146"},{"@type":"NRID","@value":"9000257704160"},{"@type":"NRID","@value":"9000345287073"},{"@type":"NRID","@value":"9000258441092"},{"@type":"NRID","@value":"9000257828106"},{"@type":"NRID","@value":"9000291598476"},{"@type":"NRID","@value":"9000350631657"},{"@type":"NRID","@value":"9000312727741"},{"@type":"NRID","@value":"9000398963387"},{"@type":"NRID","@value":"9000241729952"},{"@type":"NRID","@value":"9000414217124"},{"@type":"NRID","@value":"9000257768675"},{"@type":"NRID","@value":"9000368922363"},{"@type":"NRID","@value":"9000414813245"},{"@type":"NRID","@value":"9000330332130"},{"@type":"NRID","@value":"9000314065185"},{"@type":"NRID","@value":"9000257827673"},{"@type":"NRID","@value":"9000243581523"}],"foaf:name":[{"@value":"Hiroaki Miura"}],"jpcoar:affiliationName":[{"@value":"RIKEN Center for Computational Science Kobe Japan"},{"@value":"Graduate School of Science University of Tokyo Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380853567796982016","@type":"Researcher","foaf:name":[{"@value":"Tetsuya Takemi"}],"jpcoar:affiliationName":[{"@value":"Disaster Prevention Research Institute Kyoto University Kyoto Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380853567796982144","@type":"Researcher","foaf:name":[{"@value":"Hirofumi Tomita"}],"jpcoar:affiliationName":[{"@value":"RIKEN Center for Computational Science Kobe Japan"},{"@value":"RIKEN Cluster for Pioneering Research Kobe Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2020-08-13","prism:volume":"47","prism:number":"16"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://creativecommons.org/licenses/by/4.0/"],"url":[{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GL088763"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2020GL088763"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2020GL088763"}],"createdAt":"2020-08-13","modifiedAt":"2024-08-11","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782014031744","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"19H01974"},{"@type":"JGN","@value":"JP19H01974"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-19H01974/"}],"notation":[{"@language":"ja","@value":"大気乱流および積雲対流のスケール間相互作用"},{"@language":"en","@value":"multi-scale interactions between atmospheric turbulence and cumulus convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1041412325975664896","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"20H05729"},{"@type":"JGN","@value":"JP20H05729"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-20H05729/"}],"notation":[{"@language":"ja","@value":"気候モデルMIROCの雲解像モデル化による第6世代規格への挑戦"},{"@language":"en","@value":"Updating MIROC toward a global cloud-resolving model"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050856995322465792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Convergence of Convective Updraft Ensembles With Respect to the Grid Spacing of Atmospheric Models"}]},{"@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/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/1360011144643544192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"What favors convective aggregation and why?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145101577856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Convection On the Edge"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145244580736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Detailed Investigation of the Self-Aggregation of Convection in Cloud-Resolving Simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145256055424","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Flux Parameterization over Land Surfaces for Atmospheric Models"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145413021696","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Missing iris effect as a possible cause of muted hydrological change and high climate sensitivity in models"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146015049600","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Clouds, Circulation, and Climate Sensitivity in a Radiative‐Convective Equilibrium Channel Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146120249216","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Boundary Layer Diabatic Processes, the Virtual Effect, and Convective Self‐Aggregation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146580764032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Convection and Climate: What Have We Learned from Simple Models and Simplified Settings?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292618546460032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The sensitivity of convective aggregation to diabatic processes in idealized radiative‐convective equilibrium simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619731688832","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Self-Aggregation of Deep Convection and its Implications for Climate"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620436737536","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Estimating Bulk Entrainment With Unaggregated and Aggregated Convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620883942912","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Radiative-convective disequilibrium"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643711079808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ensemble of Radiative‐Convective Equilibrium Simulations Near the Aggregated and Scattered Boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165336410112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Observing Convective Aggregation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574093636626048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Influence of grid aspect ratio on planetary boundary layer turbulence in large-eddy simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095507693056","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Conceptual Model of a Shallow Circulation Induced by Prescribed Low-Level Radiative Cooling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095636223616","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Generalized Smagorinsky model for anisotropic grids"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095944784128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Responses of Clouds and Large‐Scale Circulation to Global Warming Evaluated From Multidecadal Simulations Using a Global Nonhydrostatic Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567867734656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rotating radiative‐convective equilibrium simulated by a cloud‐resolving model"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043418235648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Organization of Tropical Convection in Low Vertical Wind Shears: The Role of Water Vapor"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043833251584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Radiative–convective equilibrium in a three‐dimensional cloud‐ensemble model"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045910381568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sensitivity of Convective Self‐Aggregation to Domain Size"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518690236160","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Self‐aggregation of convection in long channel geometry"}]},{"@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/1361418518922885760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Clouds, circulation and climate sensitivity"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520630219392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Coupled radiative convective equilibrium simulations with explicit and parameterized convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994159673728","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Convergence behavior of idealized convection-resolving simulations of summertime deep moist convection over land"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995508547200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Boundary Layer Height and Buoyancy Determine the Horizontal Scale of Convective Self-Aggregation"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995779711104","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Statistics on High-Cloud Areas and Their Sensitivities to Cloud Microphysics Using Single-Cloud Experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944914488832","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Large‐eddy simulation of stable atmospheric boundary layers with a revised stochastic subgrid model"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944916973312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Convective self‐aggregation, cold pools, and domain size"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419379080448","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Thermodynamic control of anvil cloud amount"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420255977472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An Energy-Balance Analysis of Deep Convective Self-Aggregation above Uniform SST"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420633544704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An Alternative Function For The Wind And Temperature Gradients In Unstable Surface Layers"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420998876416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Radiative‐convective instability"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544421095948288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global variability in radiative-convective equilibrium with a slab ocean under a wide range of CO2 concentrations"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893462905472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Nonrotating Convective Self‐Aggregation in a Limited Area AGCM"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893485268736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global‐scale convective aggregation: Implications for the Madden‐Julian Oscillation"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894939699712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Universality in the Spatial Evolution of Self-Aggregation of Tropical Convection"}]},{"@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/1363107370942130560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Observational Evidence for Relationships between the Degree of Aggregation of Deep Convection, Water Vapor, Surface Fluxes, and Radiation"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843298764800","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Large‐Eddy Simulation of Maritime Deep Tropical Convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843947822592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Convective Self‐Aggregation As a Cold Pool‐Driven Critical Phenomenon"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844171358720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Convective Heating Leads to Self‐Aggregation by Generating Available Potential Energy"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844313179648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Radiative–convective equilibrium model intercomparison project"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845238087936","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Organization of Tropical Convection in Low Vertical Wind Shears: The Role of Cold Pools"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319094182016","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Time‐scales of adjustment to radiative‐convective equilibrium in the tropical atmosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951796218368512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Radiative-Convective Equilibrium with Explicit Two-Dimensional Moist Convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268205430016","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Convective Self-Aggregation in Numerical Simulations: A Review"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680198001024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Resolution Dependence of the Diurnal Cycle of Precipitation Simulated by a Global Cloud-System Resolving 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/1390282681481210240","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"熱帯大気中のクラウドクラスターの起源に関する数値実験"},{"@language":"en","@value":"Numerical Experiments Concerning the Origin of Cloud Clusters in the Tropical Atmosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1390578902349089664","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Role of Convection in Troposphere-Lower Stratosphere Interactions in Radiative-Convective Equilibrium Simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845712986663552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Diurnal Variation of Simulated Cumulus Convection in Radiative-Convective Equilibrium"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714791861483392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Resolution dependence of deep convections in a global simulation from over 10-kilometer to sub-kilometer grid spacing"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996267026447488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Impacts of cloud microphysics on trade wind cumulus : which cloud microphysics processes contribute to the diversity in a large eddy simulation？"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2020gl088763"},{"@type":"KAKEN","@value":"PRODUCT-23530497"},{"@type":"KAKEN","@value":"PRODUCT-23741799"},{"@type":"OPENAIRE","@value":"doi_dedup___::636828cb3b2b72b80fb8c3e4338f4c15"},{"@type":"CROSSREF","@value":"10.1029/2021gl095279_references_DOI_XaqxlW6X6SUbQ68sFnxe0QFG5R6"},{"@type":"CROSSREF","@value":"10.2151/sola.2023-026_references_DOI_XaqxlW6X6SUbQ68sFnxe0QFG5R6"}]}