_:genid1 <http://www.w3.org/1999/02/22-rdf-syntax-ns#value> "Copyright protected. Obtain permission from the original figure source."^^<http://www.w3.org/2001/XMLSchema#string> .
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<http://52.38.26.42:8080/report/nca3/chapter/water-resources/figure/projected-changes-in-snow-runoff-and-soil-moisture> <http://purl.org/dc/terms/title> "Projected Changes in Snow, Runoff, and Soil Moisture"^^<http://www.w3.org/2001/XMLSchema#string> .
<http://52.38.26.42:8080/report/nca3/chapter/water-resources/figure/projected-changes-in-snow-runoff-and-soil-moisture> <http://data.globalchange.gov/gcis.owl#recommendedCitation> "Cayan et al. 2013"^^<http://www.w3.org/2001/XMLSchema#string> .
<http://52.38.26.42:8080/report/nca3/chapter/water-resources/figure/projected-changes-in-snow-runoff-and-soil-moisture> <http://data.globalchange.gov/gcis.owl#hasCaption> "These projections, assuming continued increases in heat-trapping gas emissions (A2 scenario; Ch. 2: Our Changing Climate), illustrate: a) major losses in the water content of the snowpack that fills western rivers (snow water equivalent, or SWE); b) significant reductions in runoff in California, Arizona, and the central Rocky Mountains; and c) reductions in soil moisture across the Southwest. The changes shown are for mid-century (2041-2070) as percentage changes from 1971-2000 conditions (Figure source: Cayan et al. 2013)."^^<http://www.w3.org/2001/XMLSchema#string> .
<http://52.38.26.42:8080/report/nca3/chapter/water-resources/figure/projected-changes-in-snow-runoff-and-soil-moisture> <http://purl.org/dc/terms/rights> _:genid1 .
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<http://52.38.26.42:8080/report/nca3/chapter/water-resources/figure/projected-changes-in-snow-runoff-and-soil-moisture> <http://purl.org/spar/cito/cites> <http://52.38.26.42:8080/book/c9625c65-c20f-4163-87fe-cebf734f7836> .
<http://52.38.26.42:8080/report/nca3/chapter/water-resources/figure/projected-changes-in-snow-runoff-and-soil-moisture> <http://purl.org/spar/biro/references> <http://52.38.26.42:8080/reference/59cf5a07-b64b-418c-acc6-73b7ff4d7d7e> .
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