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revision 1.32 by jmc, Fri Feb 29 02:44:13 2008 UTC revision 1.33 by jmc, Tue Nov 3 23:20:16 2009 UTC
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31        isomorphisms, one hydrodynamical kernel can be used to simulate        isomorphisms, one hydrodynamical kernel can be used to simulate
32        flow in both the atmosphere and ocean.</p>        flow in both the atmosphere and ocean.</p>
33    
34      <p>You are welcome to <a href="http://mitgcm.org/source_code.html">      <p>You are welcome to <a href="http://mitgcm.org/public/source_code.html">
35        download</a> and use MITgcm.</p>        download</a> and use MITgcm.</p>
36    
37      <p>Papers charting the development of MITgcm <a      <p>Papers charting the development of MITgcm <a
# Line 53  Line 53 
53        </blockquote>        </blockquote>
54        -->        -->
55    
       <p><b>January 15, 2008&nbsp;:</b></p>  
       <blockquote>  
       Breaking News: Hidden up-to-date Documentation escaped from hide-out:  
       <br>  
       <A href="http://mitgcm.org/r2_manual/latest/">Latest Online Documentation</A>  
       <br>  
       <img src="docfest2008.jpeg" alt="DocFestJan2008" border="0" width="86" height="86" />  
       </blockquote>  
   
       <p><b>March 19, 2007&nbsp;:</b></p>  
       <blockquote>  
       Breaking News:  The MITgcm is now able to generate Sea-Ice Donuts.  
       In a push to move forward MITgcm on the path of fundamental science and climate  
       understanding, David Ferreira and Jean-Michel Campin  
       simulated a Sea-ice Donut using a coupled AquaPlanet configuration (see  
       movie <A href=movies/Sea_Ice_Donut_x1.mpg>here</A>).  
       This experiment was initialized with  the T and S fields from  
       a previous Aquaplanet run which has polar sea-ice caps. These  
       caps are associated with salt-compensated temperature inversions in the upper  
       ocean. The new run is initialized without sea-ice and within a month, large  
       sea-ice caps grow over the poles, rejecting salt. This triggers convection which  
       in turns brings relatively warm water to the surface and melts the ice close  
       to the poles. Here we have a <A href=movies/Sea_Ice_Donut_x1.mpg>donut</A>.  
       Look out for that chapter on aqua-planets in the next IPCC report!  
       </blockquote>  
   
       <p><b>Feb 04, 2007&nbsp;:</b></p>  
       <blockquote>  
        News is back by popular request. New advection schemes are currently  
        being tested. Some preliminary results from the new schemes can be seen  
        <A href=news/advection_testing_jan07/advection_testing.html>  
        here.  
        </A>  
        The plots show a tracer being transported and stretched in the  
        MITgcm advect_xz verification test. Both new schemes (OS7MP  
        and Prather second-order scheme with limiting) have very low implied  
        diffusivity.  
        We are currently evaluating the  
        schemes to assess their implied diffusivity, with a bottle of  
        Jean-Michel's favorite Belgian  
        beer going to the the least diffusive scheme - watch this space!  
       </blockquote>  
   
       <p><b>March 9, 2005&nbsp;:</b></p>  
       <blockquote>  
        A short article entitled  
        "NASA Supercomputer Improves Prospects for Ocean Climate Research"  
        in the current EOS (volume 86, number 9, March 1 2005)  
        gives a succinct overview of some of the advanced high-resolution  
        state-estimation work being undertaken with MITgcm by members  
        of the ECCO consortium. The article describes  
        ground-breaking computational  
        technologies that have enabled this work and outlines the future goals of  
        this next generation planetary scale assimilation initiative. A pdf containing  
        the article can be found  
        <a href="http://mitgcm.org/articles/EOSecco.pdf">  
        here.  
        </a>  
       </blockquote>  
         
       <p><b>Sep 24, 2004&nbsp;:</b></p>  
       <blockquote>  
         MITgcm is now able to write and (to a lesser extent) read NetCDF files.  
         The framework (the "MNC" package) has been tested by numerous developers  
         on literally dozens of machines and, for the past month, has been a  
         working part of our standard verification suite.  We encourage MITgcm  
         users (especially new users) to try out the MNC package since the model  
         output is now much easier to read and understand.  For further NetCDF  
         information please see:  
         <ul>  
           <li><a href="http://mitgcm.org/cmi_redir.php/package_mnc">  
               Manual entry for the MNC package.</a></li>  
           <li>Directions <a  
               href="http://mitgcm.org/pipermail/mitgcm-support/2004-September/002589.html">  
               from our email archives</a> and <a  
               href="http://mitgcm.org/mwiki/index.php/MNC_Package">from our  
               wiki</a> for installing NetCDF.</li>  
           <li>The <a  
               href="http://my.unidata.ucar.edu/content/software/netcdf/index.html">  
               main NetCDF web site</a>.</li>  
         </ul>  
        </blockquote>  
         
       <p><b>May 20, 2004 at 05:01 EDT&nbsp;:</b></p>  
       <blockquote>  
         Congratulations to Ed and Boo on the birth this  
         morning of a 7lb 1oz, baby girl,  
         <a href="http://eddy.csail.mit.edu/gallery/Alex-Arrives">Alexandra Sophia</a>.  
       </blockquote>  
         
       <p><b>April 13, 2004&nbsp;:</b></p>  
       <blockquote>  
         A new movie by Dimitris Menemenlis and Chris Henze shows ice dynamics  
         over the North Pole. The viscous-plastic behavior of ice sheets subject  
         to wind forcing and ocean currents can be clearly seen in the  
         translucent ice-sheet. The movie can be downloaded from <a  
         href="movies/ice_03.mpg"> here</a> (this one is 91MB!).  A set of web  
         pages with summary information regarding MITgcm simulations being  
         carried out in the ECCO high resolution global ocean state estimation  
         initiative can be found <a href="http://ecco.jpl.nasa.gov/cube_sphere">  
           here</a>.  
       </blockquote>  
   
       <p><b>March 26, 2004 at 01:38 EST&nbsp;:</b></p>  
       <blockquote>  
         Congratulations to Alistair and Sonya on the birth this  
         morning of a 7lb 3oz, 19.5 inches long baby girl, Ariane Jade.  
       </blockquote>  
   
       <p><b>January 22, 2004&nbsp;:</b></p>  
       <blockquote>  
         A spectacular movie by Chris Henze of NASA AMES beautifully captures an  
         eddy permitting expanded cube sphere MITgcm simulation being carried out,  
         as part of the <a href="http://www.ecco-group.org">ECCO</a> project, by  
         Dimitris Menemenlis and others at JPL with help from core MITgcm team members  
         and staff from NASA AMES. The animation  
         shows the speed of ocean currents at 15m depth from the simulation, it can be  
         downloaded <a href=news/cube_6.mpg>here</a> (its 47MB  
         but worth waiting for!). A second animation with different perspectives and  
         rotation can be downloaded <a href=news/cube_7.mpg>here</a>.  
         As described <a href=news/agu_2004/menemenlis_et_al.pdf>here</a> Dimitris Menemenlis  
         will be presenting aspects of this calculation at AGU in Portland.  
         A list of some other AGU 2004 presentation abstracts related to MITgcm can be  
         found <a href=news/agu_2004>here</a>.  
       </blockquote>  
               
56    </body>    </body>
57  </html>  </html>
   

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