Basal channels drive active surface hydrology and transverse ice shelf fracture

Author:

Dow Christine F.1ORCID,Lee Won Sang23ORCID,Greenbaum Jamin S.4ORCID,Greene Chad A.45ORCID,Blankenship Donald D.45,Poinar Kristin6ORCID,Forrest Alexander L.78ORCID,Young Duncan A.4ORCID,Zappa Christopher J.9ORCID

Affiliation:

1. Department of Geography and Environmental Management, University of Waterloo, 200 University Avenue West, Waterloo, Ontario N2L 3G1, Canada.

2. Unit of Ice Sheet and Sea Level Changes, Korea Polar Research Institute, Incheon, Republic of Korea.

3. Polar Sciences, Korea University of Science and Technology, Incheon, Republic of Korea.

4. Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, Austin, TX 78758, USA.

5. Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, Austin, TX 78712, USA.

6. Crysopheric Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA.

7. Civil and Environmental Engineering, University of California, Davis, One Shields Avenue, Davis, CA 95616, USA.

8. Tahoe Environmental Research Center, University of California, Davis, 291 Country Club Drive, Incline Village, NV 89451, USA.

9. Lamont-Doherty Earth Observatory, Columbia University, 61 Route 9W, Palisades, NY 10964, USA.

Abstract

Ice shelf basal channels cause transverse fractures that can be exacerbated by surface rivers, culminating in calving.

Funder

National Science Foundation

Natural Sciences and Engineering Research Council of Canada

Canada Research Chairs Program

Korean Ministry of Oceans and Fisheries

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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