@prefix dcterms: <http://purl.org/dc/terms/> .
@prefix xsd: <http://www.w3.org/2001/XMLSchema#> .
@prefix gcis: <http://data.globalchange.gov/gcis.owl#> .
@prefix rdf: <http://www.w3.org/1999/02/22-rdf-syntax-ns#> .
@prefix doco: <http://purl.org/spar/doco> .
@prefix cito: <http://purl.org/spar/cito/> .
@prefix biro: <http://purl.org/spar/biro/> .
@prefix prov: <http://www.w3.org/ns/prov#> .

<http://52.38.26.42:8080/report/nca3/chapter/tribal-indigenous-native-lands-resources/figure/thawing-permafrost-in-alaska>
   dcterms:identifier "thawing-permafrost-in-alaska";
   gcis:figureNumber "12.6"^^xsd:string;
   dcterms:title "Thawing Permafrost in Alaska"^^xsd:string;
   gcis:recommendedCitation "Permafrost Lab, Geophysical Institute, University of Alaska Fairbanks"^^xsd:string;
   gcis:hasCaption "The maps show projected ground temperature at a depth of 3.3 feet assuming continued increases in emissions (A2 scenario) and assuming a substantial reduction in emissions (B1 scenario). Blue shades represent areas below freezing at a depth of 3.3 feet and yellow and red shades represent areas above freezing at that depth (see Ch. 22: Alaska for more details). Many Alaska Natives depend on permafrost for ice cellars to store frozen food, and replacing these cellars with electricity-driven freezers is expensive or otherwise infeasible. Permafrost thawing also affects infrastructure like roads and utility lines. (Figure source: Permafrost Lab, Geophysical Institute, University of Alaska Fairbanks)."^^xsd:string;
   dcterms:rights [ rdf:value "Copyright protected. Obtain permission from the original figure source."^^xsd:string; ];
   gcis:isFigureOf <http://52.38.26.42:8080/report/nca3/chapter/tribal-indigenous-native-lands-resources>;
   gcis:isFigureOf <http://52.38.26.42:8080/report/nca3>;

## Geographical extent of the figure content

## Temporal extent of the figure content

   a gcis:Figure, doco:Figure .