Articles | Volume 12, issue 2
https://doi.org/10.5194/tc-12-521-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-12-521-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Increased West Antarctic and unchanged East Antarctic ice discharge over the last 7 years
Alex S. Gardner
CORRESPONDING AUTHOR
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA
Geir Moholdt
Norwegian Polar Institute, Fram Centre, 9296 Tromsø, Norway
Ted Scambos
National Snow and Ice Data Center (NSIDC), University of Colorado at Boulder, Boulder, CO 80303, USA
Mark Fahnstock
Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK 99775, USA
Stefan Ligtenberg
Institute for Marine and Atmospheric research Utrecht (IMAU), Utrecht University, Utrecht, the Netherlands
Michiel van den Broeke
Institute for Marine and Atmospheric research Utrecht (IMAU), Utrecht University, Utrecht, the Netherlands
Johan Nilsson
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA
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Discussed (final revised paper)
Discussed (final revised paper)
Latest update: 14 Dec 2024
Short summary
We map present-day Antarctic surface velocities from Landsat imagery and compare to earlier estimates from radar. Flow accelerations across the grounding lines of West Antarctica's Amundsen Sea Embayment, Getz Ice Shelf and the western Antarctic Peninsula, account for 89 % of the observed increase in ice discharge. In contrast, glaciers draining the East Antarctic have been remarkably stable. Our work suggests that patterns of mass loss are part of a longer-term phase of enhanced flow.
We map present-day Antarctic surface velocities from Landsat imagery and compare to earlier...