wires at the same site. The different trends during this period are partially due to transient effects, but these effects tend to diminish with time. The difference may be primarily due to crevassing or other inhomogenei

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Date: 2011-05-06 21:19:52 Ice sheet Barclay Kamb Meltwater Till Basal sliding Whillans Ice Stream Geology Antarctica Ice sheet dynamics Glaciology Physical geography Glacier		wires at the same site. The different trends during this period are partially due to transient effects, but these effects tend to diminish with time. The difference may be primarily due to crevassing or other inhomogenei Add to Reading List Source URL: s3.amazonaws.com Download Document from Source Website File Size: 2,53 MB Share Document on Facebook

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