Member Since 1983
Terry J. Wilson
Professor, Ohio State University Main Campus
AGU Research
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Experiential learning opens pathways for early career researchers to engage in complex, interdisciplinary modeling of ice sheet and sea level change
ONLINE POSTER SESSION FOR EDUCATION II
education | 24 january 2024
Stephanie A. Konfal, Terry J. Wilson, Holger Steff...
One of the most important topics in polar geoscience and for society around the globe is the contribution of ice sheets to global sea level. An integr...
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Crustal and Uppermost Mantle Azimuthal Seismic Anisotropy of Antarctica From Ambient Noise Tomography
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
10 january 2024
Zhengyang Zhou, Douglas Wiens, Andrew Nyblade, Ric...

Seismic anisotropy provides essential information for characterizing the orientation of deformation and flow in the crust and mantle. The isotropic...

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The role of the solid Earth in Antarctica’s contribution to future global sea levels
ANTARCTIC ICE-OCEAN INTERACTION AND ICE SHEET RETREAT: PAST, PRESENT, AND FUTURE III ORAL
cryosphere | 13 december 2023
Natalya A. Gomez, Maryam Yousefi, David Pollard, R...
The response of the Antarctic Ice Sheet (AIS) to climate change is the largest uncertainty in projecting future sea level rise over the coming centuri...
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Tidally Modulated Glacial Seismicity at the Foundation Ice Stream, West Antarctica
JOURNAL OF GEOPHYSICAL RESEARCH: EARTH SURFACE
03 july 2023
Erica M. Lucas, Andrew Nyblade, Richard C. Aster, ...

We investigate the occurrence of repeating glacial seismicity near the grounding line of the Foundation Ice Stream and further upstream using conti...

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Crustal and Uppermost Mantle Azimuthal Seismic Anisotropy of Antarctica from Ambient Noise Tomography
SEISMOLOGY CONTRIBUTIONS: STRUCTURAL SEISMOLOGY IX POSTER
seismology | 16 december 2022
Zhengyang Zhou, Douglas Wiens, Andrew Nyblade, Ric...
Seismic anisotropy provides essential information for characterizing the orientation of past or current deformation or flow direction in the crust and...
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Upper Mantle Attenuation and Velocity Anomalies beneath Antarctica Constrained by Teleseismic Body Waves
SEISMOLOGY CONTRIBUTIONS: STRUCTURAL SEISMOLOGY IV ORAL
seismology | 15 december 2022
Jialin Li, Douglas Wiens, Andrew Nyblade, Richard ...
The seismic attenuation and velocity structure of the upper mantle beneath Antarctica is important for estimating mantle temperature, and thus viscosi...
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Complex Seasonal and Secular Signals in Antarctic GNSS Time Series
GEODESY FOR CLIMATE RESEARCH III POSTER
geodesy | 13 december 2022
David M. Saddler, Terry J. Wilson, Michael G. Bevi...
The POLENET/ANET network of continuously operating GNSS instruments spans the drainage basin system of the West Antarctic Ice Sheet and the margins of...
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Repeating Glacial Seismicity at the Foundation Ice Stream, West Antarctica
ENVIRONMENTAL SEISMOLOGY: A GEOPHYSICAL TOOL TO STUDY SURFACE AND NEAR-SURFACE PROCESSES IV POSTER
seismology | 12 december 2022
Erica M. Lucas, Andrew Nyblade, Richard C. Aster, ...
We investigate the occurrence of glacial seismicity located near the grounding line of the Foundation Ice Stream and further upstream using continuous...
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