Origin of surface undulations at the Kamb Ice Stream grounding line, West Antarctica
The West Antarctic Ice Sheet is drained primarily by five major ice streams, which together control the volume of ice discharged into the ocean across the grounding line. The grounding line of Kamb Ice Stream (KIS) is unusual because the ice stream upstream of it is stagnant. Here, a set of surface...
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| Format: | Others |
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PDXScholar
2012
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| Online Access: | https://pdxscholar.library.pdx.edu/open_access_etds/677 https://pdxscholar.library.pdx.edu/cgi/viewcontent.cgi?article=1676&context=open_access_etds |