@prefix rdf: <http://www.w3.org/1999/02/22-rdf-syntax-ns#> .
@prefix ns0: <http://opendata.inra.fr/anaeeThes/> .
@prefix skos: <http://www.w3.org/2004/02/skos/core#> .
@prefix owl: <http://www.w3.org/2002/07/owl#> .
@prefix dct: <http://purl.org/dc/terms/> .
@prefix ns1: <http://aims.fao.org/aos/agrovoc/> .
@prefix ns2: <http://www.eionet.europa.eu/gemet/concept/> .
@prefix ns3: <http://art.uniroma2.it/ontologies/vocbench#> .
@prefix metadata_def: <http://data.bioontology.org/metadata/def/> .
@prefix ns4: <http://data.bioontology.org/rest_backup_mappings/> .
ns0:c2_2445
skos:narrower ns0:c2_2460 .
ns0:c2_2460
ns3:hasStatus "Published" ;
metadata_def:mappingLoom "climat" ;
metadata_def:mappingRest <http://data.bioontology.org/rest_backup_mappings/75f834c0-b292-0136-849e-525400026749> ;
metadata_def:mappingSameURI ns0:c2_2460 ;
dct:modified "2017-03-21T13:42:48Z"^^<http://www.w3.org/2001/XMLSchema#dateTime> ;
a owl:NamedIndividual, skos:Concept ;
skos:broader ns0:c2_2445 ;
skos:definition ns0:i_def_077808a9-a80f-4886-93a9-fa74ba1284d0, "The average weather condition in a region of the world. Many aspects of the Earth's geography affect the climate. Equatorial, or low, latitudes are hotter than the polar latitudes because of the angle at which the rays of sunlight arrive at the Earth's surface. The difference in temperature at the equator and at the poles has an influence on the global circulation of huge masses of air. Cool air at the poles sinks and spreads along the surface of the Earth towards the equator. Cool air forces its way under the lower density warmer air in the lower regions, pushing the lighter air up and toward the poles, where it will cool and descend. (Source: WRIGHT)"@en ;
skos:exactMatch ns1:c_1665, <http://www.eionet.europa.eu/gemet/concept/1462> ;
skos:inScheme <http://opendata.inra.fr/anaeeThes/> ;
skos:narrower ns0:c2_2493, ns0:c2_2498, ns0:c2_2500, ns0:c2_2501, ns0:c2_2502, ns0:c2_2503, ns0:c2_2505, ns0:c2_2843, ns0:c2_2911, ns0:c4_4222, ns0:c_1401870919713, ns0:c_1403180758864, ns0:c_1438247248403, ns0:c_1438958489878, ns0:c_1438958547977, ns0:c_1438961017921, ns0:c_7bb48760, ns0:c_9a6c2d49 ;
skos:prefLabel "climat"@fr, "climate"@en .
ns0:c2_2493
skos:broader ns0:c2_2460 .
ns0:c2_2498
skos:broader ns0:c2_2460 .
ns0:c2_2500
skos:broader ns0:c2_2460 .
ns0:c2_2501
skos:broader ns0:c2_2460 .
ns0:c2_2502
skos:broader ns0:c2_2460 .
ns0:c2_2503
skos:broader ns0:c2_2460 .
ns0:c2_2505
skos:broader ns0:c2_2460 .
ns0:c2_2843
skos:broader ns0:c2_2460 .
ns0:c2_2911
skos:broader ns0:c2_2460 .
ns0:c4_4222
skos:broader ns0:c2_2460 .
ns0:c_1401870919713
skos:broader ns0:c2_2460 .
ns0:c_1403180758864
skos:broader ns0:c2_2460 .
ns0:c_1438247248403
skos:broader ns0:c2_2460 .
ns0:c_1438958489878
skos:broader ns0:c2_2460 .
ns0:c_1438958547977
skos:broader ns0:c2_2460 .
ns0:c_1438961017921
skos:broader ns0:c2_2460 .
ns0:c_7bb48760
skos:broader ns0:c2_2460 .
ns0:c_9a6c2d49
skos:broader ns0:c2_2460 .
@prefix rdf: <http://www.w3.org/1999/02/22-rdf-syntax-ns#> .
@prefix ns0: <http://opendata.inra.fr/anaeeThes/> .
@prefix skos: <http://www.w3.org/2004/02/skos/core#> .
@prefix owl: <http://www.w3.org/2002/07/owl#> .
@prefix dct: <http://purl.org/dc/terms/> .
@prefix ns1: <http://aims.fao.org/aos/agrovoc/> .
@prefix ns2: <http://www.eionet.europa.eu/gemet/concept/> .
@prefix ns3: <http://art.uniroma2.it/ontologies/vocbench#> .
@prefix metadata_def: <http://data.bioontology.org/metadata/def/> .
@prefix ns4: <http://data.bioontology.org/rest_backup_mappings/> .
ns0:c2_2445
skos:narrower ns0:c2_2460 .
ns0:c2_2460
ns3:hasStatus "Published" ;
metadata_def:mappingLoom "climat" ;
metadata_def:mappingRest <http://data.bioontology.org/rest_backup_mappings/75f834c0-b292-0136-849e-525400026749> ;
metadata_def:mappingSameURI ns0:c2_2460 ;
dct:modified "2017-03-21T13:42:48Z"^^<http://www.w3.org/2001/XMLSchema#dateTime> ;
a owl:NamedIndividual, skos:Concept ;
skos:broader ns0:c2_2445 ;
skos:definition ns0:i_def_077808a9-a80f-4886-93a9-fa74ba1284d0, "The average weather condition in a region of the world. Many aspects of the Earth's geography affect the climate. Equatorial, or low, latitudes are hotter than the polar latitudes because of the angle at which the rays of sunlight arrive at the Earth's surface. The difference in temperature at the equator and at the poles has an influence on the global circulation of huge masses of air. Cool air at the poles sinks and spreads along the surface of the Earth towards the equator. Cool air forces its way under the lower density warmer air in the lower regions, pushing the lighter air up and toward the poles, where it will cool and descend. (Source: WRIGHT)"@en ;
skos:exactMatch ns1:c_1665, <http://www.eionet.europa.eu/gemet/concept/1462> ;
skos:inScheme <http://opendata.inra.fr/anaeeThes/> ;
skos:narrower ns0:c2_2493, ns0:c2_2498, ns0:c2_2500, ns0:c2_2501, ns0:c2_2502, ns0:c2_2503, ns0:c2_2505, ns0:c2_2843, ns0:c2_2911, ns0:c4_4222, ns0:c_1401870919713, ns0:c_1403180758864, ns0:c_1438247248403, ns0:c_1438958489878, ns0:c_1438958547977, ns0:c_1438961017921, ns0:c_7bb48760, ns0:c_9a6c2d49 ;
skos:prefLabel "climat"@fr, "climate"@en .
ns0:c2_2493
skos:broader ns0:c2_2460 .
ns0:c2_2498
skos:broader ns0:c2_2460 .
ns0:c2_2500
skos:broader ns0:c2_2460 .
ns0:c2_2501
skos:broader ns0:c2_2460 .
ns0:c2_2502
skos:broader ns0:c2_2460 .
ns0:c2_2503
skos:broader ns0:c2_2460 .
ns0:c2_2505
skos:broader ns0:c2_2460 .
ns0:c2_2843
skos:broader ns0:c2_2460 .
ns0:c2_2911
skos:broader ns0:c2_2460 .
ns0:c4_4222
skos:broader ns0:c2_2460 .
ns0:c_1401870919713
skos:broader ns0:c2_2460 .
ns0:c_1403180758864
skos:broader ns0:c2_2460 .
ns0:c_1438247248403
skos:broader ns0:c2_2460 .
ns0:c_1438958489878
skos:broader ns0:c2_2460 .
ns0:c_1438958547977
skos:broader ns0:c2_2460 .
ns0:c_1438961017921
skos:broader ns0:c2_2460 .
ns0:c_7bb48760
skos:broader ns0:c2_2460 .
ns0:c_9a6c2d49
skos:broader ns0:c2_2460 .