Routine Monitoring of Changes in the Columbia Glacier, Alaska, with Synthetic Aperture Radar
Author:
Publisher
Elsevier BV
Subject
Computers in Earth Sciences,Geology,Soil Science
Reference15 articles.
1. Glacier snow line mapping using ERS-1 SAR imagery;Adam;Remote Sens. Environ.,1997
2. Bindschadler, R. A., and Rasmussen, L. A. (1983), Finite-difference model predictions of the drastic retreat of Columbia Glacier, Alaska, USGS Professional Paper 1258-D, U.S. Geological Survey, Washington, DC.
3. Brown, C. S., Meier, M. F., and Post, A. (1982), Calving speed of Alaska tidewater glaciers, with application to Columbia Glacier, USGS Professional Paper 1258-C, U.S. Geological Survey, Washington, DC.
4. Brown, C. S., Meier, M. F., and Post, A. (1986), Bed topography inferred from airborne radio-echo sounding of Columbia Glacier, Alaska, USGS Professional Paper 1258-G, U.S. Geological Survey, Washington, DC.
5. Use of SEASAT Synthetic Aperture Radar and LANDSAT Multispectral Scanner Subsystem for Alaskan glaciology studies;Hall;J. Geophys. Res.,1983
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