Studies through a borehole drilled through Thwaites near its grounding line indicate that conditions there: a stable column with strong density stratification, would tend to suppress basal melting below what is observed taking place. In essence, this study indicates that modeling of destabilization of the ice sheet under current conditions is too conservative. Thwaites is resting on bedrock that is below sea level and descends as you move inland, making it inherently unstable and prone to catastrophic collapse. No pay wall.
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Suppressed basal melting in the eastern Thwaites Glacier grounding zone - Nature
Despite observations from a hot-water-drilled access hole showing warm ocean waters beneath Thwaites Glacier Eastern Ice Shelf, the basal melt rate is strongly suppressed due to the low current speeds and strong density stratification.
