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1 <div align="left">
2
3 <span class="style1"><a href="http://www.reading.ac.uk/oceandiva">
4 ECCO2 results on OceanDIVA</a></span>
5
6 <p class="style6">
7
8 ECCO2 cube78 results have been added to the <a
9 href="http://www.reading.ac.uk/oceandiva"> OceanDIVA</a> server for
10 visualization and intercomparison with other model and data products.
11 Example OceanDIVA output for September 2004 is available <a
12 href="http://ecco2.jpl.nasa.gov/data1/cube/products/OceanDIVA">
13 here</a>.
14 </p>
15
16 <hr><!--horizontal bar break-->
17 <span class="style1"><a href="http://ecco2.org/results/face_3_carbon.html">
18 Arctic Ocean carbon flux studies with cs510 solutions</a></span>
19
20 <p class="style6">
21 <a href="mailto:mmanizza@ocean.mit.edu">Manfredi Manizza</a>,
22 <a href="mailto:stephd@ocean.mit.edu">Stephanie Dutkiewicz</a> and
23 <a href="mailto:mick@mit.edu">Mick Follows</a> are starting to use cs510
24 ocean and sea-ice solutions in the Arctic ocean region as part of an effort to
25 better understand and model the Arctic terrestrial, atmospheric and ocean carbon cycle.</p>
26
27 <hr><!--horizontal bar break-->
28 <span class="style1"><a href="http://ecco2.org/results/mode_water_8.html">
29 Studying the genesis of MODE waters with 1/8 degree lat-lon solutions</a></span>
30
31 <p class="style6">
32 <a href="mailto:gmaze@ocean.mit.edu">Guillaume Maze</a> and
33 <a href="mailto:jmarsh@mit.edu">John Marshall</a> are using the 1/8 degree latitude-longitude solutions
34 to look at the mechanical and thermodynamical air-sea processes that create MODE waters.</p>
35
36 <hr><!--horizontal bar break-->
37 <span class="style1"><a href="http://ecco2.org/results/sub_grid_eddies.html">
38 Representation of sub-grid-scale eddy and mixed-layer processes</a></span>
39
40 <p class="style6">
41 <a href="mailto:dfer@mit.edu">David Ferreira</a>,
42 <a href="mailto:raffaele@mit.edu">Raffaele Ferrari</a>,
43 <a href="mailto:baylor@mit.edu">Baylor Fox-Kemper</a> and
44 <a href="mailto:jmarsh@mit.edu">John Marshall</a> are calculating eddy
45 statistics and estimating eddy forcings on the large scale circulation
46 to improve understanding of these phenomena. These estimates are being
47 used to guide development of new parameterizations for processes that
48 are poorly resolved in current generation climate models.</p>
49
50 <hr><!--horizontal bar break-->
51 <span class="style1">Figures</span>
52
53 <p class="style6"><a href="http://ecco2.org/results/arctic_ssh/">Arctic sea level</a>
54
55 <p class="style6"><a href="http://ecco2.org/results/GRACE/">Comparison with GRACE</a>
56
57 <p class="style6"><a href="http://ecco2.org/results/resolution/">Impact of resolution</a>
58
59 <p class="style6"><a href="http://ecco2.org/results/SSH/SSH.html">SSH</a>
60
61 <p class="style6"><a href="http://ecco.jpl.nasa.gov/cube_sphere/ecco2/">
62 Comparison of ECCO2 solution with drifter and TOPEX/JASON data</a></p>
63
64 <hr><!--horizontal bar break-->
65 <span class="style1">Animations</span>
66
67 <p class="style6"><a href="http://ecco2.org/results/IceCube/">Sea-ice movies</a></p>
68
69 <p class="style6"><a href="http://ecco2.org/results/SST/">SST Animations</a>
70
71 <p class="style6"><a href="http://ecco2.org/results/VTS_01_1.VOB">
72 Video: Ocean models for predicting Earth's climate changes</a></p>
73
74 <hr><!--horizontal bar break-->
75 <span class="style1">Posters</span>
76
77 <p class="style6"><a
78 href="http://ecco2.org/results/Climate_Weather_poster_05.16.html">
79 Using High-End Computers to Model Our Climate and Weather</a>
80
81 <p class="style6"><a href="http://ecco2.org/results/x05-039_Menemenlis_RTD.pdf">
82 Towards routine eddy-permitting estimates of the global ocean and sea-ice circulations</a>
83
84 <p class="style6"><a href="http://ecco2.org/results/ECCO_poster.pdf">
85 NAS Poster: Supercomputers Improve Estimates of Ocean Climate</a></p></div>

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