Grounding line migration of West Antarctic glaciers, detected by ERS radar interferometry
ERS radar interferometry is a powerful new technique to map the grounding line of outlet glaciers, or more precisely to located the limit of tidal flexing of their floating sections, or hinge line.
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| Language: | English |
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2004
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| Online Access: | http://hdl.handle.net/2014/22289 |
| Summary: | ERS radar interferometry is a powerful new technique to map the grounding line of outlet glaciers, or more precisely to located the limit of tidal flexing of their floating sections, or hinge line. |
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