Role of Surface Albedo for Explaining Differences of Modeled Greenland Ice Sheet Melt
The Greenland Ice Sheet has been in a state of negative mass balance for the past several decades and is currently responsible for a substantial proportion of global sea-level rise. Accurate projections of ice sheet mass loss are therefore imperative, and a number of regional climate models (RCMs) h...
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| Format: | Thesis |
| Language: | English |
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University of Oregon
2024
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| Online Access: | https://scholarsbank.uoregon.edu/xmlui/handle/1794/29804 |