Wilkes subglacial basin ice sheet response to Southern Ocean warming during late Pleistocene interglacials
The response of the East Antarctic Ice Sheet to past intervals of oceanic and atmospheric warming is still not well constrained but is critical for under- standing both past and future sea-level change. Furthermore, the ice sheet in the Wilkes Subglacial Basin appears to have undergone thinning and ice dis- charge events during recent decades.
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