A potentially irreversible threshold in Antarctic ice shelf melting would be crossed if the
ocean cavity beneath the large Filchner–Ronne Ice Shelf were to become flooded with warm …

Sea level rise (SLR) is a long‐lasting consequence of climate change because global
anthropogenic warming takes centuries to millennia to equilibrate for the deep ocean and …

Owing to increasing greenhouse gas emissions, the Antarctic Ice Sheet is vulnerable to
rapid ice loss in the upcoming decades and centuries. This study examines the effectiveness …

Understanding changes in Antarctic ice shelf basal melting is a major challenge for
predicting future sea level. Currently, warm Circumpolar Deep Water surrounding Antarctica …

Understanding how climate change influences ocean-driven melting of the Antarctic ice
shelves is one of the greatest challenges for projecting future sea level rise. The East …

Abstract Filchner‐Ronne Ice Shelf (FRIS) is the world's largest ice shelf by volume. It helps
regulate Antarctica's contribution to global sea level rise, and water mass transformations …

Some ocean modeling studies have identified a potential tipping point from a low to a high
basal melt regime beneath the Filchner–Ronne Ice Shelf (FRIS), Antarctica, with significant …

Tipping points in the Earth system describe critical thresholds beyond which a single
component, part of the system, or the system as a whole changes from one stable state to …

Abstract The Antarctic Slope Front (ASF) is a fundamental feature of the subpolar Southern
Ocean that is still poorly observed. In this study we build a statistical climatology of the …

We provide an updated estimate of the annual‐mean, seasonal cycle and interannual
variability of the transports and properties of the Weddell Sea Bottom Water (WSBW) plume …