<?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>Belen Martrat</dc:contributor>
  <dc:contributor>Michael N. Evans</dc:contributor>
  <dc:contributor>Diane Thompson</dc:contributor>
  <dc:contributor>D. Reynolds</dc:contributor>
  <dc:contributor>Jason A. Addison</dc:contributor>
  <dc:creator>Helen V. McGregor</dc:creator>
  <dc:date>2016</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;The oceans make up 71% of the Earth’s surface area and are a major component of the global climate system. They are the world’s primary heat reservoir, and knowledge of the global ocean response to past and present radiative forcing is important for understanding climate change. PAGES’ Ocean2k working group aims to place marine climate of the past century within the context of the previous 2000 years (2k). Phase 1 (2011-2015) focused on constraining the forcing mechanisms most consistent with reconstructed sea surface temperature (SST) over the 2k interval (McGregor et al. 2015; Tierney et al. 2015). The 1st Ocean2k workshop assisted in the transition to Ocean2k Phase 2 (2015-2017), with the workshop goal to develop, coordinate and significantly advance community-identified and -driven activities.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.22498/pages.24.1.44</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>PAGES International Project Office</dc:publisher>
  <dc:title>Data, age uncertainties and ocean δ&lt;sup&gt;18&lt;/sup&gt;O under the spotlight for Ocean2k Phase 2</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>