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

gcmdsk:48c16952-b6e0-40cd-b6dd-7cdbf5a443a1
  skos:topConceptOf <https://vocab.met.no/GCMDSK> ;
  dc:source <https://gcmd.earthdata.nasa.gov/kms/concept/48c16952-b6e0-40cd-b6dd-7cdbf5a443a1> ;
  skos:closeMatch cfstdn:surface_albedo ;
  skos:exactMatch <https://gcmd.earthdata.nasa.gov/kms/concept/48c16952-b6e0-40cd-b6dd-7cdbf5a443a1> ;
  skos:prefLabel "EARTH SCIENCE > ATMOSPHERE > ATMOSPHERIC RADIATION > ALBEDO"@en ;
  skos:inScheme <https://vocab.met.no/GCMDSK> ;
  skos:definition "Albedo is the ratio of the radiation (radiant energy or luminous energy) reflected by a surface to that incident on it. Snow and cloud surfaces have a high albedo, because most of the energy of the visible solar spectrum is reflected. Vegetation and ocean surfaces have low albedo, because they absorb a large fraction of the energy. Clouds are the chief cause of variations in the Earth's albedo."@en ;
  a skos:Concept .

<https://vocab.met.no/GCMDSK>
  skos:prefLabel "GCMDSK"@en ;
  a skos:ConceptScheme ;
  skos:hasTopConcept gcmdsk:48c16952-b6e0-40cd-b6dd-7cdbf5a443a1 .