A - C
CASERTZ
The CASERTZ geophysical surveys were aimed at understanding geological controls on ice streams of the West Antarctic Ice Sheet, ultimately to help assess the potential for ice sheet collapse. Blankenship et al. (2001) used ice surface elevations and ice thicknesses (reported here) to calculate driving stresses across the ice sheet and thus to identify regions of rapid basal movement by ice streams. Reference: Blankenship, D.D., D.L. Morse, C.A. Finn, R.E. Bell, M.E. Peters, S.D. Kempf, S.M. Hodge, M. Studinger, J.C. Behrendt, and J.M. Brozena. 2001. Geologic controls on the initiation of rapid basal motion for West Antarctic ice streams: A geophysical perspective including new airborne radar sounding and laser altimetry results. The West Antarctic Ice Sheet: Behavior and Environment. Antarctic Research Series 77: 105-121.