<?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:creator>Richard M. Iverson</dc:creator>
  <dc:date>2018</dc:date>
  <dc:description>&lt;div class="NLM_sec NLM_sec_level_1"&gt;&lt;p&gt;The original paper concerns the formulation and use of depth-integrated equations of motion to model the dynamics of shallow flows that entrain or deposit bed material. A recurring theme of the original paper is the authors’ criticism of related theoretical results published by Iverson and Ouyang (&lt;a class="ref showRefEvent" href="https://ascelibrary.org/doi/10.1061/%28ASCE%29HY.1943-7900.0001519#" data-rid="c5" data-mce-href="https://ascelibrary.org/doi/10.1061/%28ASCE%29HY.1943-7900.0001519"&gt;2015&lt;/a&gt;). This discussion explains why that criticism is misguided.&lt;/p&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1061/(ASCE)HY.1943-7900.0001519</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Society of Civil Engineers</dc:publisher>
  <dc:title>Discussion of “Shallow water hydro-sediment-morphodynamic equations for fluvial processes” by Zhixian Cao, Chunchen Xia, Gareth Pender, and Qingquan Liu</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>