<?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>Leonard F. Konikow</dc:contributor>
  <dc:creator>Christopher E. Neuzil</dc:creator>
  <dc:date>2008</dc:date>
  <dc:description>We thank T. N. Narasimhan for his comment on our paper [Konikow and Neuzil, 2007] and for extending the discussion with a historical perspective, additional examples, and some considerations we did not discuss, including implications for water management. We support and agree with the thrust of his comments.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1029/2008WR007084</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Geophysical Union</dc:publisher>
  <dc:title>Reply to comment by T. N. Narasimhan on “A method to estimate groundwater depletion from confining layers”</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>