Fun at Antarctic grounding lines: Ice-shelf channels and sediment transport
Meltwater beneath the polar ice sheets drains, in part, through subglacial conduits. Landforms created by such drainages are abundant in areas formerly covered by ice sheets during the last glacial maximum. However, observations of subglacial conduit dynamics under a contemporary ice sheet are lacki...
Main Authors: | , , , , , , , , , , , , , |
---|---|
Format: | Conference Object |
Language: | unknown |
Published: |
2017
|
Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/49626/ https://epic.awi.de/id/eprint/49626/1/EGU2017-12173.pdf https://hdl.handle.net/10013/epic.7f3243c8-40b5-4436-81e4-48df805f2ba5 https://hdl.handle.net/ |