@prefix cpm: . @prefix dc: . @prefix dcat: . @prefix dce: . @prefix dct: . @prefix grg: . @prefix iop: . @prefix ns0: . @prefix ns1: . @prefix owl: . @prefix pav: . @prefix prov: . @prefix puv: . @prefix qudt: . @prefix rdf: . @prefix rdfs: . @prefix reg: . @prefix semapv: . @prefix skos: . @prefix sssom: . @prefix void: . rdf:type skos:Concept ; dc:identifier "effective_radius_of_stratiform_cloud_ice_particles" ; dc:modified "2019-05-14 17:27:19.0" ; void:inDataset ; owl:deprecated false ; owl:versionInfo 1 ; 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:exactMatch , , , ; skos:note "accepted"@en ; skos:prefLabel "Effective radius of stratiform cloud ice particles"@en ; skos:related .