<?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>Michael L. Anderson</dc:contributor>
  <dc:creator>Michael D. Dettinger</dc:creator>
  <dc:date>2015</dc:date>
  <dc:description>&lt;p&gt;The San Francisco Bay and Sacramento&amp;ndash;San Joaquin&amp;nbsp;Delta (Delta) are the recipients of inflows from a&amp;nbsp;watershed that spans much of California and that has&amp;nbsp;ties to nearly the entire state. Historically, California&amp;nbsp;has buffered its water supplies and flood risks both&amp;nbsp;within&amp;mdash;and beyond&amp;mdash;the Delta&amp;rsquo;s catchment by developing&amp;nbsp;many reservoirs, large and small, high and&amp;nbsp;low. Most of these reservoirs carry water from wet&amp;nbsp;winter seasons&amp;mdash;when water demands are low and&amp;nbsp;flood risks are high&amp;mdash;to dry, warm seasons (and years)&amp;nbsp;when demands are high and little precipitation falls.&amp;nbsp;Many reservoirs are also used to catch and delay&amp;nbsp;(or spread in time) flood flows that otherwise might&amp;nbsp;cause damage to communities and floodplains. This&amp;nbsp;essay describes the status of surface-water and snowpack&amp;nbsp;storage conditions in California in spring 2015,&amp;nbsp;providing context for better understanding where the&amp;nbsp;state&amp;rsquo;s water stores stand as we enter summer 2015.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.15447/sfews.2015v13iss2art1</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher> University of California at Davis; Delta Stewardship Council</dc:publisher>
  <dc:title>Storage in California’s reservoirs and snowpack in this time of drought</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>