Viewable by the world
Group Access to Chombo
Can VIEW the space: chombo-editors ,  chombo-admin ,  anonymous , 
Can EDIT the space: chombo-admin ,  chombo-editors , 
Can ADMINISTER the space: chombo-admin , 
Individual Access to Chombo
Can VIEW the space: [email protected] ,  [email protected] , 
Can EDIT the space: [email protected] ,  [email protected] , 
Can ADMINISTER the space: [email protected] ,  [email protected] , 

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Old Version 11

changes.mady.by.user Daniel Martin

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New Version 12

changes.mady.by.user Daniel Martin

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Background

Understanding the Dynamics dynamics of large ice sheets (like Greenland and Antarctica) are is crucial to projections of future sea level rise. The dynamics of ice sheets span a wide range of scales. There are localized regions (like grounding lines and ice streams) where very fine spatial resolution (better than 1 km) is needed to accurately resolve the dynamics. At the same time, there are large regions (much of the interior of Antarctica, for example) where such fine resolution is unnecessary and represents a waste of computational resources.  This makes it a prime candidate for adaptive mesh refinement.

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