Full-depth hydrographic sections of the BROKE experiment in 1996 (across the Antarctic
margin from 80 to 150° E; Bindoff et al., 2000) were revisited for the first time during the …

The ice shelves in the Bellingshausen Sea are melting and thinning rapidly due to modified
Circumpolar Deep Water (mCDW) intrusions carrying heat toward ice‐shelf cavities …

Observations of marine debris in Antarctica have been increasing; however, impacts,
distributions, sources, and transport pathways of debris remain poorly understood. Here, we …

The additional water from the Antarctic ice sheet and ice shelves due to climate‐induced
melt can impact ocean circulation and global climate. However, the major processes driving …

Abstract The Antarctic Slope Current is guided by the topographic gradient of the Antarctic
continental slope and creates a dynamical barrier between the continental shelf and the …

Meltwater content and pathways determine the impact of Antarctica's melting ice shelves on
ocean circulation and climate. Using ocean glider observations, we quantify meltwater …

Winds around the Antarctic continental margin are known to exert a strong control on the
local ocean stratification and circulation. However, past work has largely focused on the …

Simple Summary Antarctic macrobenthic communities thriving on the continental shelf have
evolved over thousands of years in perhaps the coldest and most constant environmental …

Mass loss from the Antarctic Ice Sheet is dominated by basal melting–induced warm ocean
water. Ice-sheet mass loss and thinning of buttressing ice shelves occur primarily in the …

Abstract West Antarctic Ice Sheet mass loss is a major source of uncertainty in sea level
projections. The primary driver of this melting is oceanic heat from Circumpolar Deep Water …