@prefix qx8: <http://data.loterre.fr/ark:/67375/QX8> .
@prefix skos: <http://www.w3.org/2004/02/skos/core#> .
@prefix chc: <http://data.loterre.fr/ark:/67375/CHC> .

qx8:-B03CX7WT-Q
  skos:prefLabel "sea current"@en, "courant marin"@fr ;
  a skos:Concept ;
  skos:narrower qx8:-KNKW3GW9-X .

qx8: a skos:ConceptScheme .
qx8:-KNKW3GW9-X
  skos:definition "The Gulf Stream is a warm and swift Atlantic ocean current that originates in the Gulf of Mexico and flows through the Straits of Florida and up the eastern coastline of the United States, then veers east near 36°N latitude (North Carolina) and moves toward Northwest Europe as the North Atlantic Current. The process of western intensification causes the Gulf Stream to be a northward-accelerating current off the east coast of North America. Around 40°0′N 30°0′W, it splits in two, with the northern stream, the North Atlantic Drift, crossing to Northern Europe and the southern stream, the Canary Current, recirculating off West Africa. The Gulf Stream influences the climate of the coastal areas of the East Coast of the United States from Florida to southeast Virginia (near 36°N latitude), and to a greater degree, the climate of Northwest Europe. A consensus exists that the climate of Northwest Europe is warmer than other areas of similar latitude at least partially because of the strong North Atlantic Current. It is part of the North Atlantic Gyre. Its presence has led to the development of strong cyclones of all types, both within the atmosphere and within the ocean. (Adapted from: <a href=\"https://en.wikipedia.org/wiki/Gulf_Stream\">https://en.wikipedia.org/wiki/Gulf_Stream</a>)"@en, "Le Gulf Stream est un courant océanique chaud, de surface, prenant sa source entre la Floride et les Bahamas, le long de la côte est des États-Unis et qui se disperse dans l'océan Atlantique quelque part au large de la Nouvelle-Écosse et de Terre-Neuve tout en se prolongeant par d'autres courants marins. Il constitue une portion du gyre de l'Atlantique Nord et désigne souvent dans le langage courant et celui des médias la dérive nord atlantique qui baigne les eaux de l'Europe de l'Ouest et du Nord. Le Gulf Stream est constitué de la fusion du courant de Cuba et du courant nord équatorial. (Adapté de : <a href=\"https://fr.wikipedia.org/wiki/Gulf_Stream\">https://fr.wikipedia.org/wiki/Gulf_Stream</a>)"@fr ;
  skos:prefLabel "Gulf Stream"@en, "Gulf Stream"@fr ;
  a skos:Concept ;
  skos:exactMatch <https://en.wikipedia.org/wiki/Gulf_Stream>, <https://fr.wikipedia.org/wiki/Gulf_Stream>, chc:-HS84V56T-T ;
  skos:inScheme qx8: ;
  skos:broader qx8:-B03CX7WT-Q .