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modifying a file on data5 in order to update faulks with a change
1 | bbaker | 1.2 | <div align="left"> <span class="style1"><a href="http://www.reading.ac.uk/oceandiva"> ECCO2 Results on OceanDIVA</a></span> <p class="style6"> ECCO2 cube78 results have been added to the <a href="http://www.reading.ac.uk/oceandiva"> OceanDIVA</a> server for visualization and intercomparison with other model and data products. Example OceanDIVA output for September 2004 is available <a href="http://ecco2.jpl.nasa.gov/data1/cube/products/OceanDIVA"> here</a>. </p> <hr><!--horizontal bar break--> <span class="style1"><a href="http://ecco2.org/results/face_3_carbon.html"> Arctic Ocean carbon flux studies with cs510 solutions</a></span> <p class="style6"> <a href="mailto:mmanizza@ocean.mit.edu">Manfredi Manizza</a>, <a href="mailto:stephd@ocean.mit.edu">Stephanie Dutkiewicz</a> and <a href="mailto:mick@mit.edu">Mick Follows</a> are starting to use cs510 ocean and sea-ice solutions in the Arctic ocean region as part of an effort to better understand and model the Arctic terrestrial, atmospheric and ocean carbon cycle.</p> <hr><!--horizontal bar break--> <span class="style1"><a href="http://ecco2.org/results/mode_water_8.html"> Studying the genesis of MODE waters with 1/8 degree lat-lon solutions</a></span> <p class="style6"> <a href="mailto:gmaze@ocean.mit.edu">Guillaume Maze</a> and <a href="mailto:jmarsh@mit.edu">John Marshall</a> are using the 1/8 degree latitude-longitude solutions to look at the mechanical and thermodynamical air-sea processes that create MODE waters.</p> <hr><!--horizontal bar break--> <span class="style1"><a href="mailto:http://ecco2.org/results/sub_grid_eddies.html"> Representation of sub-grid-scale eddy and mixed-layer processes</a></span> <p class="style6"> <a href="mailto:dfer@mit.edu">David Ferreira</a>, <a href="mailto:raffaele@mit.edu">Raffaele Ferrari</a>, <a href="mailto:baylor@mit.edu">Baylor Fox-Kemper</a> and <a href="mailto:jmarsh@mit.edu">John Marshall</a> are calculating eddy statistics and estimating eddy forcings on the large scale circulation to improve understanding of these phenomena. These estimates are being used to guide development of new parameterizations for processes that are poorly resolved in current generation climate models.</p> <hr><!--horizontal bar break--> <span class="style1">Figures</span> <p class="style6"><a href="http://ecco2.org/results/arctic_ssh/">Arctic sea level</a> <p class="style6"><a href="http://ecco2.org/results/GRACE/">Comparison with GRACE</a> <p class="style6"><a href="http://ecco2.org/results/resolution/">Impact of resolution</a> <p class="style6"><a href="http://ecco2.org/results/SSH/">SSH</a> <p class="style6"><a href="http://ecco.jpl.nasa.gov/cube_sphere/ecco2/"> Comparison of ECCO2 solution with drifter and TOPEX/JASON data</a></p> <hr><!--horizontal bar break--> <span class="style1">Animations</span> <p class="style6"><a href="http://ecco2.org/results/IceCube/">Sea-ice movies</a></p> <p class="style6"><a href="http://ecco2.org/results/SST/">SST Animations</a> <p class="style6"><a href="http://ecco2.org/results/VTS_01_1.VOB"> Video: Ocean models for predicting Earth's climate changes</a></p> <hr><!--horizontal bar break--> <span class="style1">Posters</span> <p class="style6"><a href="http://ecco2.org/results/Climate_Weather_poster_05.16.jpg"> Using High-End Computers to Model Our Climate and Weather</a> <p class="style6"><a href="http://ecco2.org/results/x05-039_Menemenlis_RTD.pdf"> Towards routine eddy-permitting estimates of the global ocean and sea-ice circulations</a> <p class="style6"><a href="http://ecco2.org/results/ECCO_poster.pdf"> NAS Poster: Supercomputers Improve Estimates of Ocean Climate</a></p></div> |
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