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Sea-level rise Ice-sheet uncertainty Gravity measurements of the ice-mass loss in Greenland and Antarctica are complicated by glacial isostatic adjustment. Simultaneous estimates of both signals confirm the negative trends in ice-sheet mass balance, but not their magnitude.
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.173.2931 http://polarmet.osu.edu/PolarMet/PMGFulldocs/bromwich_nicolas_ngeo_2010.pdf |
| Summary: | Sea-level rise Ice-sheet uncertainty Gravity measurements of the ice-mass loss in Greenland and Antarctica are complicated by glacial isostatic adjustment. Simultaneous estimates of both signals confirm the negative trends in ice-sheet mass balance, but not their magnitude. |
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