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<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>Patrick L. Barnard</dc:contributor>
  <dc:contributor>Cheryl Hapke</dc:contributor>
  <dc:creator>Patrick W. Limber</dc:creator>
  <dc:date>2015</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;In California, sea-level rise during the 21&lt;/span&gt;&lt;sup&gt;st&lt;/sup&gt;&lt;span&gt;&amp;nbsp;century threatens to accelerate coastal cliff recession rates. To forecast such changes for managers and policymakers, models must play a key role. In this paper, we extend a ~70-year long dataset of measured historic sea cliff retreat rates in Southern California into the 21&lt;/span&gt;&lt;sup&gt;st&lt;/sup&gt;&lt;span&gt;&amp;nbsp;century using a suite of simple analytical and empirical models. Ensemble results suggest that coastal cliff recession rates could increase on average by 0.09-0.22 m yr&lt;/span&gt;&lt;sup&gt;-1&lt;/sup&gt;&lt;span&gt;&amp;nbsp;for a 0.5-1.0 m rise in sea level by 2100, 27-67% faster than historical rates. The basic models used herein will serve as a baseline against which more complex, process-based and statistical (Bayesian) forecasts will be compared. The application of different models, with varying levels of detail, to the same geomorphic problem will provide a comprehensive forecast and address the question of how to reduce model complexity while minimizing uncertainty.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1142/9789814689977_0245</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>World Scientific</dc:publisher>
  <dc:title>Towards forecasting the retreat of California’s coastal cliffs during the 21st century</dc:title>
  <dc:type>text</dc:type>
</oai_dc:dc>