| 53 |
</blockquote> |
</blockquote> |
| 54 |
--> |
--> |
| 55 |
|
|
| 56 |
|
<p><b>January 15, 2008 :</b></p> |
| 57 |
|
<blockquote> |
| 58 |
|
Breaking News: Hidden up-to-date Documentation escaped from hide-out: |
| 59 |
|
<br> |
| 60 |
|
<A href="http://mitgcm.org/r2_manual/latest/">Latest Online Documentation</A> |
| 61 |
|
<br> |
| 62 |
|
<img src="docfest2008.jpeg" alt="DocFestJan2008" border="0" width="86" height="86" /> |
| 63 |
|
</blockquote> |
| 64 |
|
|
| 65 |
|
<p><b>March 19, 2007 :</b></p> |
| 66 |
|
<blockquote> |
| 67 |
|
Breaking News: The MITgcm is now able to generate Sea-Ice Donuts. |
| 68 |
|
In a push to move forward MITgcm on the path of fundamental science and climate |
| 69 |
|
understanding, David Ferreira and Jean-Michel Campin |
| 70 |
|
simulated a Sea-ice Donut using a coupled AquaPlanet configuration (see |
| 71 |
|
movie <A href=movies/Sea_Ice_Donut_x1.mpg>here</A>). |
| 72 |
|
This experiment was initialized with the T and S fields from |
| 73 |
|
a previous Aquaplanet run which has polar sea-ice caps. These |
| 74 |
|
caps are associated with salt-compensated temperature inversions in the upper |
| 75 |
|
ocean. The new run is initialized without sea-ice and within a month, large |
| 76 |
|
sea-ice caps grow over the poles, rejecting salt. This triggers convection which |
| 77 |
|
in turns brings relatively warm water to the surface and melts the ice close |
| 78 |
|
to the poles. Here we have a <A href=movies/Sea_Ice_Donut_x1.mpg>donut</A>. |
| 79 |
|
Look out for that chapter on aqua-planets in the next IPCC report! |
| 80 |
|
</blockquote> |
| 81 |
|
|
| 82 |
<p><b>Feb 04, 2007 :</b></p> |
<p><b>Feb 04, 2007 :</b></p> |
| 83 |
<blockquote> |
<blockquote> |
| 84 |
News is back by popular request. New advection schemes are currently |
News is back by popular request. New advection schemes are currently |
Parent Directory
| 
Revision Log
| 
Revision Graph
| 
Patch