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<p>The <b>MITgcm</b> (<b>MIT</b> <b>G</b>eneral <b>C</b>irculation |
<p>The <b>MITgcm</b> (<b>MIT</b> <b>G</b>eneral <b>C</b>irculation |
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<b>M</b>odel) is a numerical model for |
<b>M</b>odel) is a numerical model designed for study of the |
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studying the ocean and atmosphere. It is capable of simulating these |
atmosphere, ocean, and climate. Its non-hydrostatic formulation |
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fluids at a wide range of scales and can resolve many different |
enables it to simulate fluid phenomena over a wide range of |
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processes. It has a non-hydrostatic capability (Marshall et al., JGR 1997a |
scales; its adjoint capability enables it to be applied to |
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& b) and uses the finite volume method to accurately represent the |
parameter and state estimation problems. By employing fluid |
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bottom boundary position (Adcroft et al., MWR 1998).<br /><br /></p> |
isomorphisms, one hydrodynamical kernel can be used to simulate |
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flow in both the atmosphere and ocean.</p> |
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<div class="c1"><span class="c3"><b>News</b></span></div> |
<p>You are welcome to <a href="http://mitgcm.org/source_code.html"> |
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download</a> and use MITgcm.</p> |
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<p>Papers charting the development of MITgcm <a |
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href="http://paoc.mit.edu/cmi/publications.htm">can be found here. |
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</a></p> |
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<hr align="center" size="1" width="75%" /> |
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<div class="c1"><br /><span class="c3"><b>News</b></span></div> |
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