<mets:mets OBJID="oai:generic.eprints.org:4887" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:mods="http://www.loc.gov/mods/v3" LABEL="Eprints Item" xsi:schemaLocation="http://www.loc.gov/METS/ http://www.loc.gov/standards/mets/mets.xsd http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-0.xsd" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mets="http://www.loc.gov/METS/"><mets:metsHdr CREATEDATA="2009-01-07T11:21:49Z"><mets:agent TYPE="ORGANIZATION" ROLE="CUSTODIAN"><mets:name>CoastWeb Library</mets:name></mets:agent></mets:metsHdr><mets:dmdSec ID="DMD_oai:generic.eprints.org:4887_mods"><mets:mdWrap MDTYPE="mods"><mets:xmlData><mods:titleInfo><mods:title>Modern-climate analogues for paleoclimatic variations in eastern interior Alaska during the past 14,000 years: atmospheric-circulation controls of regional temperature and moisture responses</mods:title></mods:titleInfo><mods:name type="personal"><mods:namePart type="given">Mary E.</mods:namePart><mods:namePart type="family">Edwards</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">Cary J.</mods:namePart><mods:namePart type="family">Mock</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">Bruce P.</mods:namePart><mods:namePart type="family">Finney</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">Valery A.</mods:namePart><mods:namePart type="family">Barber</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">Patrick J.</mods:namePart><mods:namePart type="family">Bartlein</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods: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</mods:abstract><mods:originInfo><mods:dateIssued encoding="iso8061">2001-01</mods:dateIssued></mods:originInfo><mods:genre>Article</mods:genre></mets:xmlData></mets:mdWrap></mets:dmdSec><mets:amdSec ID="TMD_oai:generic.eprints.org:4887"><mets:rightsMD ID="rights_oai:generic.eprints.org:4887_mods"><mets:mdWrap MDTYPE="mods"><mets:xmlData><mods:useAndReproduction>
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