Not exact matches
A new three - dimensional higher - order thermomechanical ice sheet model: Basic sensitivity, ice
stream development, and ice flow across
subglacial lakes.
Jacobel, R., K. Christianson, H. Horgan, S. Anandakrishnan, R. Alley, A. Muto, B. Petersen, R. Gobel, B. Keisling and L. Snyder, «Geophysical characteristics of
Subglacial Lake Whillans and the ice
stream grounding zone, West Antarctica», bibl.
Subglacial Lake Mercer lies below the confluence of the Whillans and Mercer ice
streams, making its hydrology distinct within the region.
A
subglacial aquifer bed model and water pressure dependent basal sliding relationship for a West Antarctic ice
stream.
Anandakrishnan, S., D.D. Blankenship, R.B. Alley and P.L. Stoffa, Influence of
subglacial geology on the position of a West Antarctic ice
stream from seismic observations.
Tulaczyk, S., Kamb, B., Scherer, R.P., and Engelhardt, H.F., in press, Sedimentary processes at the base of a West Antarctic ice
stream: constraints from textural and compositional properties of
subglacial debris: Journal of Sedimentary Research.
The grounding line is where the ice
stream become afloat, so if a
subglacial lake breaches to the ocean, unless it is deep for the ice
stream to become floating, it will not alter the grounding line in and of itself.
Geothermal activity can affect basal melt dynamics through increased lubrication and enhanced flow of
subglacial streams.
The data reveal streamlined
subglacial bedforms that define a zone of paleo — ice
stream convergence, but, in contrast to previous models, do not show a simple downflow progression of bedform types along paleo — ice
stream troughs.
Robert D. Larter, Alastair G.C. Graham, Karsten Gohl, Gerhard Kuhn, Claus - Dieter Hillenbrand, James A. Smith, Tara J. Deen, Roy A. Livermore, Hans - Werner Schenke;
Subglacial bedforms reveal complex basal regime in a zone of paleo — ice
stream convergence, Amundsen Sea embayment, West Antarctica.