Abstract:The rapidly melting Totten Glacier of East Antarctica drains a basin
containing ~3.5 m sea-level rise equivalent of ice, but
the Totten Glacier dynamics and interaction with the Southern Ocean
since the Last Glacial Maximum is not well understood. To better
understand the response of the glacier to present and future climate
changes, an accurate reconstruction of the retreat history of the Totten
Glacier is needed. Hence, this study uses a multiproxy approach in
analyzing beryllium isotopes, the first such rec… Show more
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