Abstract Antarctic Bottom Water formation, such as in the Weddell Sea, is an efficient vector
for carbon sequestration on time scales of centuries. Possible changes in carbon …

As the climate warms, the grounded ice sheet and floating ice shelves surrounding
Antarctica are melting and releasing additional freshwater into the Southern Ocean …

We investigate feedbacks between subsurface continental shelf ocean temperatures and
Antarctic glacial melt using a coupled climate model. The model was forced with SSP5‐8.5 …

Polynyas facilitate air–sea fluxes, impacting climate-relevant properties such as sea ice
formation and deep water production. Despite their importance, polynyas have been poorly …

We use two coupled climate models, GFDL‐CM4 and GFDL‐ESM4, to investigate the
physical response of the Southern Ocean to changes in surface wind stress, Antarctic …

The Southern Ocean greatly contributes to the regulation of the global climate by controlling
important heat and carbon exchanges between the atmosphere and the ocean. Rates of …

Anthropogenic warming is projected to enhance Arctic freshwater exportation into the
Labrador Sea. This extra freshwater may weaken deep convection and contribute to the …

Multidecadal satellite observations indicate that the Antarctic Ice Sheet (AIS) is losing mass
at an accelerating rate, which has the potential to impact many aspects of the climate …

Two coupled climate models, differing primarily in horizontal resolution and treatment of
mesoscale eddies, were used to assess the impact of perturbations in wind stress and …

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 …