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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>

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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	1.4	<!--
34
35			To add News items, please copy the following block outside these comments and
36			replace the ===DATE=== and ===MESSAGE=== place-holders with your date and your
37			text:
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40
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42			===MESSAGE===<br /><br />
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45			-->
46	cnh	1.7	<p><b>December 9th 2003 :</b><br /></p>
47
48			<blockquote>
49			The new continuous testing page at <a href="http://mitgcm.org/testing.html">http://mitgcm.org/testing.html</a>
50			provides information on the status of the latest development code. The page
51			shows summary pass/fail ratios for the MITgcm regression tests on various platforms.
52	edhill	1.8	Details on the platforms being tested and detailed information on the status of individual
53	cnh	1.7	regression tests can be viewed from links on the test page.
54			<br /><br />
55			</blockquote>
56	edhill	1.4
57			<p><b>October 27th 2003 :</b><br /></p>
58	edhill	1.1
59	edhill	1.2	<blockquote>
60			<b><a href="http://paoc.mit.edu/cmi/">MIT Climate Modeling Initiative
61			(CMI)</a></b> web pages introduce the MITgcm model, its applications, and
62	edhill	1.4	the development team.<br /><br />
63	edhill	1.2	</blockquote>
64
65	edhill	1.4	<p><b>October 21st 2003 :</b><br /></p>
66	edhill	1.1
67	edhill	1.2	<blockquote>
68			MITgcm and ECCO-JPL team <b><a
69	edhill	1.1	href="http://www.sgi.com/newsroom/press_releases/2003/october/linux.html">
70			feature as showcase application</a></b> in NASA-SGI large shared
71	edhill	1.4	memory system program.<br /><br />
72	edhill	1.2	</blockquote>
73
74	edhill	1.1	</body>
75			</html>
76