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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>William Chilton</dc:contributor>
  <dc:contributor>David Small</dc:contributor>
  <dc:contributor>Andra Garner</dc:contributor>
  <dc:contributor>Andrea D. Hawkes</dc:contributor>
  <dc:contributor>Diego Melgar</dc:contributor>
  <dc:contributor>Simon E. Engelhart</dc:contributor>
  <dc:contributor>Lydia M. Staisch</dc:contributor>
  <dc:contributor>Robert C. Witter</dc:contributor>
  <dc:contributor>Alan Nelson</dc:contributor>
  <dc:contributor>Harvey Kelsey</dc:contributor>
  <dc:contributor>Jonathan Allan</dc:contributor>
  <dc:contributor>David S. Bruce</dc:contributor>
  <dc:contributor>Jessica DePaolis</dc:contributor>
  <dc:contributor>Mike Priddy</dc:contributor>
  <dc:contributor>Richard W. Briggs</dc:contributor>
  <dc:contributor>Robert Weiss</dc:contributor>
  <dc:contributor>SeanPaul La Selle</dc:contributor>
  <dc:contributor>Michael J. Willis</dc:contributor>
  <dc:contributor>Benjamin P. Horton</dc:contributor>
  <dc:creator>Tina Dura</dc:creator>
  <dc:date>2025</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Climate-driven sea-level rise is increasing the frequency of coastal flooding worldwide, exacerbated locally by factors like land subsidence from groundwater and resource extraction. However, a process rarely considered in future sea-level rise scenarios is sudden (over minutes) land subsidence associated with great (&amp;gt;M8) earthquakes, which can exceed 1 m. Along the Washington, Oregon, and northern California coasts, the next great Cascadia subduction zone earthquake could cause up to 2 m of sudden coastal subsidence, dramatically raising sea level, expanding floodplains, and increasing the flood risk to local communities. Here, we quantify the potential expansion of the 1% floodplain (i.e., the area with an annual flood risk of 1%) under low (~0.5 m), medium (~1 m), and high (~2 m) earthquake-driven subsidence scenarios at 24 Cascadia estuaries. If a great earthquake occurred today, floodplains could expand by 90 km&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;(low), 160 km&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;(medium), or 300 km&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;(high subsidence), more than doubling the flooding exposure of residents, structures, and roads under the high subsidence scenario. By 2100, when climate-driven sea-level rise will compound the hazard, a great earthquake could expand floodplains by 170 km&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;(low), 240 km&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;(medium), or 370 km&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;(high subsidence), more than tripling the flooding exposure of residents, structures, and roads under the high subsidence scenario compared to the 2023 floodplain. Our findings can support decision-makers and coastal communities along the Cascadia subduction zone as they prepare for compound hazards from the earthquake cycle and climate-driven sea-level rise and provide critical insights for tectonically active coastlines globally.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1073/pnas.2424659122</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>National Academy of Sciences of the United States</dc:publisher>
  <dc:title>Increased flood exposure in the Pacific Northwest following earthquake-driven subsidence and sea-level rise</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>