de to Pa iversi ised f on E changes in climate has been successfully simulated with large-scale numerical ice-sheet models. Since these models are highly sophisticated, they are only applicable on the scientific level as they demand a large amount of CPU time. Based covers an area of more than 13 10...
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.516.6427 http://homepages.ulb.ac.be/~fpattyn/papers/Pattyn2006_CAGEO.pdf |
| Summary: | de to Pa iversi ised f on E changes in climate has been successfully simulated with large-scale numerical ice-sheet models. Since these models are highly sophisticated, they are only applicable on the scientific level as they demand a large amount of CPU time. Based covers an area of more than 13 106 km2 and contains high degree of confidence. Such large-scale models are amount of input data required, such models need much CPU time to calculate. Here, I present an ice-sheet model at low resolution along a flowline through the |
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