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Abstract: Thwaites Eastern Ice Shelf Cavity Observations Reveal Multi-year Sea Ice Dynamics and Deep-Water Warming in Pine Island Bay, West Antarctica (AGU25)

Thwaites Eastern Ice Shelf Cavity Observations Reveal Multi-year Sea Ice Dynamics and Deep-Water Warming in Pine Island Bay, West Antarctica

Christian Wild1,2, Tasha Snow3,4, Tiago Segabinazzi Dotto5, Peter E D Davis6, Scott Tyler7, Ted A Scambos8, Erin C Pettit2 and Karen J. Heywood9, (1)University of Tübingen, Department of Geosciences, Tübingen, Germany, (2)Oregon State University, College of Earth, Ocean, and Atmospheric Sciences, Corvallis, United States, (3)University of Maryland College Park, College Park, United States, (4)NASA Goddard Space Flight Center, Greenbelt, United States, (5)National Oceanography Centre, Southampton, United Kingdom, (6)NERC British Antarctic Survey, Cambridge, United Kingdom, (7)University of Nevada, Reno, Department of Geological Sciences and Engineering, Reno, NV, United States, (8)University of Colorado, Boulder, Boulder, Colorado, United States, (9)University of East Anglia, Centre for Ocean and Atmospheric Sciences, School of Environmental Science, Norwich, NR4, United Kingdom
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