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

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

cfstdn:effective_radius_of_stratiform_cloud_snow_particle
  skos:inScheme <https://vocab.met.no/CFSTDN> ;
  owl:sameAs cfstdn:effective_radius_of_stratiform_cloud_snow_particles ;
  dc:isReplacedBy cfstdn:effective_radius_of_stratiform_cloud_snow_particles ;
  skos:topConceptOf <https://vocab.met.no/CFSTDN> ;
  a skos:Concept ;
  owl:deprecated true ;
  skos:prefLabel "effective_radius_of_stratiform_cloud_snow_particle"@en ;
  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 ;
  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/CF12N203/> ;
  skos:note "deprecated"@en .

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