Project Information
Collaborative Research: Geophysical Study of Ice Stream Stick-slip Dynamics
This award supports a three-year study of the ongoing deceleration and stick-slip motion of Whillans Ice Stream (WIS), West Antarctica. Understanding the dynamic behavior of ice streams is essential for predicting the future of the West Antarctic Ice Sheet (WAIS). Despite being one of the best-studied ice streams in Antarctica, the surprising flow characteristics of WIS continue to demand interdisciplinary research. Recent estimates indicate that the WIS may stagnate within 50 years, resulting in a significant change to the mass balance of the Siple Coast sector of West Antarctica. The reasons for the ongoing stagnation are not well known, and are possibly linked (causally or coincidentally) to the stick-slip behavior. Our recent work on WIS stick-slip motion suggest that all slip events nucleate from a common location on the ice stream, suggesting that a relatively small (approximately 10 km in diameter) region of the exerts fundamental control over the flow of this large ice stream (100s of km long and 100 kilometers wide). We hypothesize that this is a region of increased bed strength and our measurements will address that hypothesis. We will deploy a series of GPS receivers and seismometers on the ice stream to accurately locate the nucleation region so that a comprehensive ground based geophysical survey can be conducted to determine the physical properties of bed at the nucleation point. The ground geophysical program will consist of reflection seismic and ice-penetrating radar studies that will better constrain the properties of both the hypothesized higher-friction nucleation zone and the surrounding regions. Slip events also generate seismic energy that can be recorded 100s of km away from the ice stream, thus, the GPS and seismometer deployment will also aid us in relating seismic waveforms directly with the rapid motion that occurs during slip events. The increased ability to relate rupture processes with seismic emissions will allow us to use archived seismic records to explore changes in the behavior of WIS during the later half of the 20th century. Broader impacts of this study include improved knowledge ice sheet dynamics, which remain a poorly constrained component of the climate system, thus, limiting our ability to predict the Earth's response to climate change. The scientific work includes the education of two graduate students and continued training of one post-doctoral scholar, thus helping to train the next generation of polar scientists. We will expose the broader public to polar science through interactions with the media and by take advantaging of programs to include K-12 educators in our field work.
Person Role
Winberry, Paul Investigator
Anandakrishnan, Sridhar Co-Investigator
Alley, Richard Co-Investigator
Wiens, Douglas Investigator
Antarctic Glaciology Award # 0944794
Antarctic Glaciology Award # 0944671
AMD - DIF Record(s)
Data Management Plan
None in the Database
Product Level:
Not provided
Repository Title (link) Format(s) Status
IRIS Geophysical Study of Ice Stream Stick Slip None exist
USAP-DC Whillans Ice Stream Stick-slip None exist
  1. Picotti, S., Vuan, A., Carcione, J. M., Horgan, H. J., & Anandakrishnan, S. (2015). Anisotropy and crystalline fabric of Whillans Ice Stream (West Antarctica) inferred from multicomponent seismic data. Journal of Geophysical Research: Solid Earth, 120(6), 4237–4262. (doi:10.1002/2014jb011591)
  2. Pratt, M. J., Winberry, J. P., Wiens, D. A., Anandakrishnan, S., & Alley, R. B. (2014). Seismic and geodetic evidence for grounding-line control of Whillans Ice Stream stick-slip events. Journal of Geophysical Research: Earth Surface, 119(2), 333–348. (doi:10.1002/2013jf002842)
  3. Picotti, S., Carcione, J. M., & Pavan, M. (2024). Seismic attenuation in Antarctic firn. The Cryosphere, 18(1), 169–186. (doi:10.5194/tc-18-169-2024)
  4. Picotti, S., Carcione, J. M., & Pavan, M. (2023). Seismic attenuation in Antarctic firn. (doi:10.5194/tc-2023-19)

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