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Outputs (3)

Contrasting Response of West and East Antarctic Ice Sheets to Glacial Isostatic Adjustment (2021)
Journal Article
Coulon, V., Bulthuis, K., Whitehouse, P. L., Sun, S., Haubner, K., Zipf, L., & Pattyn, F. (2021). Contrasting Response of West and East Antarctic Ice Sheets to Glacial Isostatic Adjustment. Journal of Geophysical Research: Earth Surface, 126(7), Article e2020JF006003. https://doi.org/10.1029/2020jf006003

The Antarctic ice sheet (AIS) lies on a solid Earth that displays large spatial variations in rheological properties, with a thin lithosphere and low-viscosity upper mantle (weak Earth structure) beneath West Antarctica and an opposing structure bene... Read More about Contrasting Response of West and East Antarctic Ice Sheets to Glacial Isostatic Adjustment.

Comparing Glacial-Geological Evidence and Model Simulations 1 of Ice Sheet Change since the Last Glacial Period in the Amundsen Sea Sector of Antarctica (2021)
Journal Article
Johnson, J., Pollard, D., Whitehouse, P., Roberts, S., Rood, D., & Schaefer, J. (2021). Comparing Glacial-Geological Evidence and Model Simulations 1 of Ice Sheet Change since the Last Glacial Period in the Amundsen Sea Sector of Antarctica. Journal of Geophysical Research: Earth Surface, 126(6), https://doi.org/10.1029/2020jf005827

Since the Last Glacial Maximum ∼20,000 years ago, the Antarctic Ice Sheet has undergone extensive changes, resulting in a much smaller present-day configuration. Improving our understanding of basic physical processes that played important roles duri... Read More about Comparing Glacial-Geological Evidence and Model Simulations 1 of Ice Sheet Change since the Last Glacial Period in the Amundsen Sea Sector of Antarctica.

A reconciled solution of Meltwater Pulse 1A sources using sea-level fingerprinting (2021)
Journal Article
Lin, Y., Hibbert, F., Whitehouse, P., Woodroffe, S., Purcell, A., Shennan, I., & Bradley, S. (2021). A reconciled solution of Meltwater Pulse 1A sources using sea-level fingerprinting. Nature Communications, 12, Article 2015. https://doi.org/10.1038/s41467-021-21990-y

The most rapid global sea-level rise event of the last deglaciation, Meltwater Pulse 1A (MWP-1A), occurred ∼14,650 years ago. Considerable uncertainty regarding the sources of meltwater limits understanding of the relationship between MWP-1A and the... Read More about A reconciled solution of Meltwater Pulse 1A sources using sea-level fingerprinting.