  <eprint id="http://library.coastweb.info/id/eprint/4886" xmlns="http://eprints.org/ep2/data/2.0">
    <eprintid>4886</eprintid>
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    <source>35375</source>
    <dir>disk0/00/00/48/86</dir>
    <datestamp>2008-11-03 12:41:40</datestamp>
    <lastmod>2008-11-06 14:58:40</lastmod>
    <status_changed>2008-11-03 12:41:40</status_changed>
    <type>article</type>
    <contact_email>m.e.edwards@soton.ac.uk</contact_email>
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        <uri>http://eprints.soton.ac.uk/35375</uri>
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    <creators>
      <item>
        <name>
          <family>Edwards</family>
          <given>Mary E.</given>
        </name>
        <id></id>
      </item>
      <item>
        <name>
          <family>Mock</family>
          <given>Cary J.</given>
        </name>
        <id></id>
      </item>
      <item>
        <name>
          <family>Finney</family>
          <given>Bruce P.</given>
        </name>
        <id></id>
      </item>
      <item>
        <name>
          <family>Barber</family>
          <given>Valerie A.</given>
        </name>
        <id></id>
      </item>
      <item>
        <name>
          <family>Bartlein</family>
          <given>Patrick J.</given>
        </name>
        <id></id>
      </item>
    </creators>
    <title>Potential analogues for paleoclimatic variations in eastern interior Alaska during the past 14,000 yr: atmospheric-circulation controls of regional temperature and moisture responses</title>
    <ispublished>pub</ispublished>
    <subjects>
      <item>GE</item>
      <item>GB</item>
    </subjects>
    <full_text_status>none</full_text_status>
    <keywords>palaeoclimate, Alaska, Beringia, climate variations, pollen analysis</keywords>
    <note>This novel approach developed modern synoptic analogues for past climatic conditions as indicated by Holocene paleodata. Four midsummer temperature-moisture anomalies were considered; these represent hypotheses that can be tested with model simulations an</note>
    <abstract>The paleoclimatic history of a region can be viewed as a series of surface temperature and moisture anomalies through time. The effects of changes in large-scale climatic controls (e.g., insolation, major circulation controls) can be mediated by the influ</abstract>
    <date_type>published</date_type>
    <date>2001-01-02</date>
    <publication>Quaternary Science Reviews</publication>
    <volume>20</volume>
    <number>1-3</number>
    <pagerange>189-202</pagerange>
    <id_number>doi:10.1016/S0277-3791(00)00123-2</id_number>
    <refereed>TRUE</refereed>
    <issn>0277-3791</issn>
    <official_url>http://dx.doi.org/10.1016/S0277-3791(00)00123-2</official_url>
    <referencetext>Abbott, M.B., 1996. Holocene climatic variability for lake sites in the Bolivian Andes and interior Alaska based on sedimentology and radiocarbon dating by accelerator mass spectrometry. Unpublished Ph.D. Dissertation, University of Minnesota, Minneapolis</referencetext>
    <documents></documents>
  </eprint>
