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   dcterms:identifier "observed-shifts-in-streamflow-timing";
   gcis:figureNumber "21.1"^^xsd:string;
   dcterms:title "Observed Shifts in Streamflow Timing"^^xsd:string;
   gcis:recommendedCitation "adapted from Fritze et al. 2011"^^xsd:string;
   gcis:hasCaption "Reduced June flows in many Northwest snow-fed rivers is a signature of warming in basins that\r\n    have a significant snowmelt contribution. The fraction of annual flow occurring in June increased slightly in rain-dominated\r\n    coastal basins and decreased in mixed rain-snow basins and snowmelt-dominated basins over the period 1948 to\r\n    2008. The high flow period is in June for most\r\n    Northwest river basins; decreases in summer flows can make it more difficult to meet a variety of competing human and natural\r\n    demands for water. (Figure source: adapted from Fritze et al.\r\n    2011)."^^xsd:string;
   dcterms:rights [ rdf:value "Copyright protected. Obtain permission from the original figure source."^^xsd:string; ];
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