@prefix skos: <http://www.w3.org/2004/02/skos/core#> .
@prefix cfstdn: <https://vocab.met.no/CFSTDN/> .
@prefix dc: <http://purl.org/dc/terms/> .
@prefix owl: <http://www.w3.org/2002/07/owl#> .

<https://vocab.met.no/CFSTDN>
  skos:prefLabel "Climate and Forecast Standard Names"@en ;
  a skos:ConceptScheme ;
  skos:hasTopConcept cfstdn:effective_radius_of_stratiform_cloud_graupel_particle .

cfstdn:effective_radius_of_stratiform_cloud_graupel_particles
  skos:prefLabel "effective_radius_of_stratiform_cloud_graupel_particles"@en ;
  a skos:Concept .

cfstdn:effective_radius_of_stratiform_cloud_graupel_particle
  skos:note "deprecated"@en ;
  dc:isReplacedBy cfstdn:effective_radius_of_stratiform_cloud_graupel_particles ;
  owl:deprecated true ;
  skos:definition "The effective radius of a size distribution of particles, such as aerosols, cloud droplets or ice crystals, is the area weighted mean radius of particle size. It is calculated as the ratio of the third to the second moment of the particle size distribution. In an atmosphere model, stratiform cloud is that produced by large-scale convergence (not the convection schemes)."@en ;
  skos:prefLabel "effective_radius_of_stratiform_cloud_graupel_particle"@en ;
  a skos:Concept ;
  skos:inScheme <https://vocab.met.no/CFSTDN> ;
  dc:source <http://cfconventions.org/Data/cf-standard-names/78/build/cf-standard-name-table.html> ;
  skos:exactMatch <http://vocab.nerc.ac.uk/collection/P07/current/CF12N199/> ;
  skos:topConceptOf <https://vocab.met.no/CFSTDN> ;
  owl:sameAs cfstdn:effective_radius_of_stratiform_cloud_graupel_particles .