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Ice Flow in the Humboldt, Petermann, and Ryder Glaciers, North GreenlandRadar Interferometry, ice-penetrating radar profiles, and an elevation model are used to determine the catchment area, rates of ice discharge, and approximate states of balance for three large outlet glaciers in northeast Greenland.
Document ID
20060041081
Acquisition Source
Jet Propulsion Laboratory
Document Type
Reprint (Version printed in journal)
External Source(s)
hdl:2014/18934
Authors
Joughin, I.
Fahnestock, M.
Kwok, R.
Gogineni, P.
Allen, C.
Date Acquired
August 23, 2013
Publication Date
January 1, 1998
Publication Information
Publication: Journal of Glaciology
Subject Category
Communications And Radar
Distribution Limits
Public
Copyright
Other
Keywords
interferometry
Ice Flow in the Humboldt Petermann Ryder Glaciers North Greenland Radar

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