Abstract The Atlantic Meridional Overturning Circulation (AMOC) is a key component of the
climate through its transport of heat in the North Atlantic Ocean. Decadal changes in the …

Abstract Purpose of Review Assessment of the impact of ocean resolution in Earth System
models on the mean state, variability, and future projections and discussion of prospects for …

GLORYS12 is a global eddy-resolving physical ocean and sea ice reanalysis at 1/12°
horizontal resolution covering the 1993-present altimetry period, designed and implemented …

We present an unprecedented set of high‐resolution climate simulations, consisting of a 500‐
year pre‐industrial control simulation and a 250‐year historical and future climate simulation …

We present a new framework for global ocean–sea-ice model simulations based on phase 2
of the Ocean Model Intercomparison Project (OMIP-2), making use of the surface dataset …

Oceanic transport of heat by ubiquitous mesoscale eddies plays a critical role in regulating
climate variability and redistributing excess heat absorbed by ocean under global warming …

Sharp fronts and eddies that are ubiquitous in the world ocean, as well as features such as
shelf seas and under-ice-shelf cavities, are not captured in climate projections. Such small …

The latest assessment report from the Intergovernmental Panel on Climate Change
concluded that the Atlantic Meridional Overturning Circulation (AMOC) was very likely to …

Fine-scale currents, O (1–100 km, days–months), are actively involved in the transport and
transformation of biogeochemical tracers in the ocean. However, their overall impact on …

The ocean mixed layer is the interface between the ocean interior and the atmosphere or
sea ice and plays a key role in climate variability. It is thus critical that numerical models …