Research ArticleGEOLOGY

Basal channels drive active surface hydrology and transverse ice shelf fracture

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Science Advances  13 Jun 2018:
Vol. 4, no. 6, eaao7212
DOI: 10.1126/sciadv.aao7212

Article Information

vol. 4 no. 6

Online ISSN: 
History: 
  • Received for publication August 18, 2017
  • Accepted for publication May 1, 2018

Author Information

  1. Christine F. Dow1,*,
  2. Won Sang Lee2,3,
  3. Jamin S. Greenbaum4,
  4. Chad A. Greene4,5,
  5. Donald D. Blankenship4,5,
  6. Kristin Poinar6,,
  7. Alexander L. Forrest7,8,
  8. Duncan A. Young4 and
  9. Christopher J. Zappa9
  1. 1Department of Geography and Environmental Management, University of Waterloo, 200 University Avenue West, Waterloo, Ontario N2L 3G1, Canada.
  2. 2Unit of Ice Sheet and Sea Level Changes, Korea Polar Research Institute, Incheon, Republic of Korea.
  3. 3Polar Sciences, Korea University of Science and Technology, Incheon, Republic of Korea.
  4. 4Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, Austin, TX 78758, USA.
  5. 5Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, Austin, TX 78712, USA.
  6. 6Crysopheric Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA.
  7. 7Civil and Environmental Engineering, University of California, Davis, One Shields Avenue, Davis, CA 95616, USA.
  8. 8Tahoe Environmental Research Center, University of California, Davis, 291 Country Club Drive, Incline Village, NV 89451, USA.
  9. 9Lamont-Doherty Earth Observatory, Columbia University, 61 Route 9W, Palisades, NY 10964, USA.
  1. *Corresponding author. Email: christine.dow{at}uwaterloo.ca
  • Present address: Department of Earth Science, University at Buffalo, Buffalo, NY 14260, USA.

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