Thwaites Interdisciplinary Margin Evolution - The Role of Shear Margin Dynamics in the Future Evolution of Thwaites Drainage Basin (TIME)
TIME is an ice-based project using state-of-the-art geophysical techniques to observe rapidly deforming parts of Thwaites Glacier (shear margins) which may have significant control over future stability of the West Antarctic Ice Sheet (WAIS). The TIME project will observe rapidly deforming parts of Thwaites Glacier which may have significant control over the future evolution of WAIS, and use these new observations to improve ice sheet models used to predict future sea level rise.