Zheng ITGC:059
Zheng, Y., D. P. Stevens, K. J. Heywood, B. G. M. Webber, and B. Y. Queste. 2022. Reversal of ocean gyres near ice shelves in the Amundsen Sea caused by the interaction of sea ice and wind. The Cryosphere 16, 3005–3019, 2022.
Posts
Clyne ITGC:057
Clyne, Elisabeth. Geophysical Investigation of Basal and Hydrologic Conditions in Glaciers and Ice Shelves. 2021. The Pennsylvania State University ProQuest Dissertations Publishing 2021. 28841701.
Dias dos Santos ITGC:054
Dias dos Santos, T., M. Morlighem, and D. Brinkerhoff. 2022. A new vertically integrated MOno-Layer Higher-Order (MOLHO) ice flow model. The Cryosphere 16, 179–195.
Morlighem ITGC:051
Morlighem, M., D. Goldberg, T. Dias dos Santos, J. Lee, and M. Sagebaum. 2021. Mapping the Sensitivity of the Amundsen Sea Embayment to Changes in External Forcings Using Automatic Differentiation. Geophysical Research Letters 48:23 e2021GL095440.
Watkins ITGC:049
Watkins, R. H., J. N. Bassis, and M. D. Thouless. 2021. Roughness of Ice Shelves Is Correlated With Basal Melt Rates. Geophysical Research Letters 48:21 e2021GL094743.
Slater D. A. ITGC:048
Slater, D. A., D. I. Benn, T. R. Cowton, J. N. Bassis, J. A. Todd. 2021. Calving Multiplier Effect Controlled by Melt Undercut Geometry. Journal of Geophysical Research: Earth Surface 26:7.
It is with deep sorrow we report the death of Professor David Vaughan who was the UK lead on the International Thwaites Glacier Collaboration (ITGC). He was suffering from cancer and passed away peacefully at home in the UK on Thursday 9 February 2023. David retired as British Antarctic Survey (BAS) Director of Science in July 2021 and remained working as the UK lead in the Science Coordination Office (SCO) for the ITGC.
The rapid retreat of Thwaites Glacier in West Antarctica appears to be driven by different processes under its floating ice shelf than researchers previously understood. Novel observations from where the ice enters the ocean show that while melting beneath much of the ice shelf is weaker than expected, melting in cracks and crevasses is much faster. Despite the suppressed melting the glacier is still retreating, and these findings provide an important step forward in understanding the glacier’s contribution to future sea-level rise.
Rosier ITGC:096
Rosier, S. H. R., C. Y. S. Bull, W. L. Woo, and G. H. Gudmundsson. 2023. Predicting ocean-induced ice-shelf melt rates using deep learning. The Cryosphere, 17, 499–518.
Christie ITGC-088
Christie, F. D. W., E. J. Steig, N. Gourmelon, S. F. B. Tett, and R. G. Bingham. 2023. Inter-decadal climate variability induces differential ice response along Pacific-facing West Antarctica. Nature Communications 14:93.
