Abstract The Antarctic Ice Sheet (AIS) is out of equilibrium with the current anthropogenic‐
enhanced climate forcing. Paleoenvironmental records and ice sheet models reveal that the …

Oceanographic observations and models show that the heat brought by the warm modified
Circumpolar Deep Water (mCDW) intrusion accelerates the melting of the Antarctic ice shelf …

Melting ice shelves around Antarctica control the massive input of freshwater into the ocean
and play an intricate role in global heat redistribution. The Amery Ice Shelf regulates …

Intrusion of warm modified Circumpolar Deep Water (mCDW) is critical to heat transport onto
the continental shelf around Antarctica, with substantial impacts on basal melting of ice …

Analyses of hydrographic observation data sets revealed that modified Circumpolar Deep
Water (mCDW) tends to flood the western flank (73–78° E, 67–68° S) of the Four Ladies …

Basal melting of ice shelves is inherently difficult to quantify through direct observations, yet
it is a critical factor controlling Antarctic mass balance and global sea‐level rise. While much …

The mass balance of the Antarctic Ice Sheet (AIS) is important to global sea-level change.
The AIS loses mass mainly through basal melting and subsequent calving of the Antarctic …

The bathymetry under the Amery Ice Shelf steers the flow of ocean currents transporting
ocean heat, and thus is a prerequisite for precise modeling of ice‐ocean interactions …

Water mass transformation (WMT) around the Antarctic margin controls Antarctica Bottom
Water formation and the abyssal limb of the global meridional overturning circulation …

We provide a detailed description of the spatial distribution, seasonality and transformation
of the main water masses within MacKenzie Polynya (MP) in Prydz Bay, East Antarctica …