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    <p>The <b>MITgcm</b> (<b>MIT</b> <b>G</b>eneral <b>C</b>irculation 
      <b>M</b>odel) is a numerical model for
      studying the ocean and atmosphere. It is capable of simulating these
      fluids at a wide range of scales and can resolve many different
      processes. It has a non-hydrostatic capability (Marshall et al., JGR 1997a
      &amp; b) and uses the finite volume method to accurately represent the
      bottom boundary position (Adcroft et al., MWR 1998).<br /><br /></p>

    <div class="c1"><b>MITgcm</b></div>

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    <p><b>December 9th 2003&nbsp;:</b><br /></p>

        <blockquote>
          The new continuous testing page at <a
          href="http://mitgcm.org/testing.html">
          http://mitgcm.org/testing.html</a> provides information on the status
          of the latest development code. The page shows summary pass/fail
          ratios for the MITgcm regression tests on various platforms.  Details
          on the platforms being tested and detailed information on the status
          of individual regression tests can be viewed from links on the test
          page.  <br /><br />
        </blockquote>

    <p><b>October 27th 2003&nbsp;:</b><br /></p>

        <blockquote>
      <b><a href="http://paoc.mit.edu/cmi/">MIT Climate Modeling Initiative
              (CMI)</a></b> web pages introduce the MITgcm model, its
              applications, and the development team.<br /><br />
        </blockquote>
    
    <p><b>October 21st 2003&nbsp;:</b><br /></p>

        <blockquote>
          MITgcm and ECCO-JPL team <b><a
            href="http://www.sgi.com/newsroom/press_releases/2003/october/linux.html">
            feature as showcase application</a></b> in NASA-SGI large shared
            memory system program.<br /><br />
        </blockquote>
        
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24
25	edhill	1.6	<p>The <b>MITgcm</b> (<b>MIT</b> <b>G</b>eneral <b>C</b>irculation
26			<b>M</b>odel) is a numerical model for
27	edhill	1.1	studying the ocean and atmosphere. It is capable of simulating these
28			fluids at a wide range of scales and can resolve many different
29			processes. It has a non-hydrostatic capability (Marshall et al., JGR 1997a
30			& b) and uses the finite volume method to accurately represent the
31			bottom boundary position (Adcroft et al., MWR 1998).<br /><br /></p>
32
33	edhill	1.9	<div class="c1"><b>MITgcm</b></div>
34
35	edhill	1.4	<!--
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38			replace the ===DATE=== and ===MESSAGE=== place-holders with your date and your
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47			-->
48	cnh	1.7	<p><b>December 9th 2003 :</b><br /></p>
49
50			<blockquote>
51	edhill	1.9	The new continuous testing page at <a
52			href="http://mitgcm.org/testing.html">
53			http://mitgcm.org/testing.html</a> provides information on the status
54			of the latest development code. The page shows summary pass/fail
55			ratios for the MITgcm regression tests on various platforms. Details
56			on the platforms being tested and detailed information on the status
57			of individual regression tests can be viewed from links on the test
58			page. <br /><br />
59	cnh	1.7	</blockquote>
60	edhill	1.4
61			<p><b>October 27th 2003 :</b><br /></p>
62	edhill	1.1
63	edhill	1.2	<blockquote>
64	edhill	1.9	<b><a href="http://paoc.mit.edu/cmi/">MIT Climate Modeling Initiative
65			(CMI)</a></b> web pages introduce the MITgcm model, its
66			applications, and the development team.<br /><br />
67	edhill	1.2	</blockquote>
68
69	edhill	1.4	<p><b>October 21st 2003 :</b><br /></p>
70	edhill	1.1
71	edhill	1.2	<blockquote>
72			MITgcm and ECCO-JPL team <b><a
73	edhill	1.1	href="http://www.sgi.com/newsroom/press_releases/2003/october/linux.html">
74			feature as showcase application</a></b> in NASA-SGI large shared
75	edhill	1.4	memory system program.<br /><br />
76	edhill	1.2	</blockquote>
77
78	edhill	1.1	</body>
79			</html>
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