Abstract Antarctic Bottom Water (AABW) is a major component of the global overturning
circulation, originating around the Antarctic continental margin. In recent decades AABW has …

Abstract Antarctic Bottom Water (AABW) is pivotal for oceanic heat and carbon
sequestrations on multidecadal to millennial timescales. The Weddell Sea contributes nearly …

The lower limb of the Atlantic overturning circulation is resupplied by the sinking of dense
Antarctic Bottom Water (AABW) that forms via intense air–sea–ice interactions next to …

Abstract Antarctic Bottom Water (AABW), which fills the global ocean abyss, is derived from
dense water that forms in several distinct Antarctic shelf regions. Previous modeling studies …

The natural variability of the Weddell Sea variety of Antarctic Bottom Water (AABW) is
examined in a long-term integration of a coupled climate model. Examination of passive …

Abstract Antarctic Bottom Water (AABW) supplies the lower limb of the global overturning
circulation, ventilates the abyssal ocean and sequesters heat and carbon on multidecadal to …

Despite advances in our understanding of the processes driving contemporary sea level
rise, the stability of the Antarctic ice sheets and their contribution to sea level under projected …

Abstract Antarctic Bottom Water supplies the deep limb of the global overturning circulation
and ventilates the abyssal ocean. Antarctic Bottom Water has warmed, freshened, and …

Abstract Antarctic Bottom Water (AABW) is a critical component of the global climate system,
occupying the abyssal layer of the World Ocean and driving the lower limb of the global …

Antarctic Bottom Water (AABW), the densest water in the global overturning circulation, has
warmed in recent decades, most notably in the Atlantic. Time series recorded within the …