<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Gregory T. Pederson</dc:contributor>
  <dc:contributor>Connie A. Woodhouse</dc:contributor>
  <dc:contributor>Edward R Cook</dc:contributor>
  <dc:contributor>Gregory J. McCabe</dc:contributor>
  <dc:contributor>Erika K. Wise</dc:contributor>
  <dc:contributor>Patrick Erger</dc:contributor>
  <dc:contributor>Larry Dolan</dc:contributor>
  <dc:contributor>Marketa McGuire</dc:contributor>
  <dc:contributor>Subhrendu Gangopadhyay</dc:contributor>
  <dc:contributor>Katherine J. Chase</dc:contributor>
  <dc:contributor>Jeremy S. Littell</dc:contributor>
  <dc:contributor>Stephen T. Gray</dc:contributor>
  <dc:contributor>Scott St. George</dc:contributor>
  <dc:contributor>Jonathan M. Friedman</dc:contributor>
  <dc:contributor>David J. Sauchyn</dc:contributor>
  <dc:contributor>Jannine St. Jacques</dc:contributor>
  <dc:contributor>John W. King</dc:contributor>
  <dc:creator>Justin T. Martin</dc:creator>
  <dc:date>2019</dc:date>
  <dc:description>Paleohydrologic records can provide unique, long-term perspectives on streamflow variability and hydroclimate for use in water resource planning.  Such long-term records can also play a key role in placing both present day events and projected future conditions into a broader context than that offered by instrumental observations.  However, relative to other major river basins across the western United States, a paucity of streamflow reconstructions has to date prevented the full application of such paleohydrologic information in the Upper Missouri River Basin.  Here we utilize a set of naturalized streamflow records for the Upper Missouri and an expanded network of tree-ring records to reconstruct streamflow at thirty-one gaging locations across the major headwaters of the basin.  The reconstructions explain an average of 68% of the variability in the observed streamflow records and extend available records of streamflow back to 886 CE on average.  Basin-wide analyses suggest unprecedented hydroclimatic variability over the region during the Medieval period, similar to that observed in the Upper Colorado River Basin, and show considerable synchrony of persistent wet-dry phasing with the Colorado River over the last 1200 years.  Streamflow estimates in individual sub-basins of the Upper Missouri demonstrate increased spatial variability in discharge during the Little Ice Age (~1400-1850 CE) compared with the Medieval Climate Anomaly (~800-1400 CE).  The network of streamflow reconstructions presented here fills a major geographical void in paleohydrologic understanding and now allows for a long-term assessment of hydrological variability over the majority of the western U.S.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.quascirev.2019.105971</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>1200 years of Upper Missouri River streamflow reconstructed from tree rings</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>