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--- mitgcm.org/front_content/news.xml 2003/12/10 17:52:20 1.10 +++ mitgcm.org/front_content/news.xml 2003/12/14 00:49:57 1.11 @@ -22,15 +22,25 @@ <body> - <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 - & b) and uses the finite volume method to accurately represent the - bottom boundary position (Adcroft et al., MWR 1998).<br /><br /></p> + <p>The <b>MITgcm</b> (<b>MIT</b> <b>G</b>eneral <b>C</b>irculation + <b>M</b>odel) is a numerical model designed for study of the + atmosphere, ocean, and climate. Its non-hydrostatic formulation + enables it to simulate fluid phenomena over a wide range of + scales; its adjoint capability enables it to be applied to + parameter and state estimation problems. By employing fluid + isomorphisms, one hydrodynamical kernel can be used to simulate + flow in both the atmosphere and ocean.</p> - <div class="c1"><span class="c3"><b>News</b></span></div> + <p>You are welcome to <a href="http://mitgcm.org/source_code.html"> + download</a> and use MITgcm.</p> + + <p>Papers charting the development of MITgcm <a + href="http://paoc.mit.edu/cmi/publications.htm">can be found here. + </a></p> + + <hr align="center" size="1" width="75%" /> + + <div class="c1"><br /><span class="c3"><b>News</b></span></div> <!--
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