The notion that the Atlantic Meridional Overturning Circulation (AMOC) can have more than
one stable equilibrium emerged in the 1980s as a powerful hypothesis to explain rapid …

Future sea-level change is characterized by both quantifiable and unquantifiable uncertainties.
Effective communication of both types of uncertainty is a key challenge in translating sea-…

While the Atlantic Ocean is ventilated by high-latitude deep water formation and exhibits a
pole-to-pole overturning circulation, the Pacific Ocean does not. This asymmetric global …

Abstract Changes in sea ice significantly modulate climate change because of its high reflective
and strong insulating nature. In contrast to Arctic sea ice, sea ice surrounding Antarctica …

Interocean exchange of heat and salt around South Africa is thought to be a key link in the
maintenance of the global overturning circulation of the ocean. It takes place at the Agulhas …

This study analyses the response of the Atlantic meridional overturning circulation (AMOC)
to LGM forcings and boundary conditions in nine PMIP coupled model simulations, including …

Both historical and idealized climate model experiments are performed with a variety of Earth
system models of intermediate complexity (EMICs) as part of a community contribution to …

The heat and salt input from the Indian to Atlantic Oceans by Agulhas Leakage is found to
influence the Atlantic overturning circulation in a low-resolution Ocean General Circulation …

The first decade of the 21st century was characterized by a hiatus in global surface warming.
Using ocean model hindcasts and reanalyses we show that heat uptake between the …

The stability of the Atlantic meridional overturning circulation (MOC) is investigated for
various climate scenario runs, using data from the CMIP3 archive of coupled atmosphere-ocean …