Revealing the former bed of Thwaites Glacier using sea-floor bathymetry

The geometry of the sea floor beyond Thwaites Glacier (TG) is a major control on the routing of warm ocean waters towards the ice stream’s grounding zone, which has led to increased mass loss through sub-ice-shelf melting and resulting accelerated ice flow. Nearshore topographic highs act as pinning...

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Bibliographic Details
Main Authors: Hogan, Kelly A., Larter, Robert D., Graham, Alastair G. C., Arthern, Robert, Kirkham, James D., Totten Minzoni, Rebecca, Jordan, Tom A., Clark, Rachel, Fitzgerald, Victoria, Anderson, John B., Hillenbrand, Claus-Dieter, Nitsche, Frank O., Simkins, Lauren, Smith, James A., Gohl, Karsten, Arndt, Jan Erik, Hong, Jongkuk, Wellner, Julia
Format: Text
Language:English
Published: 2020
Subjects:
Online Access:https://doi.org/10.5194/tc-2020-25
https://tc.copernicus.org/preprints/tc-2020-25/