Turbulent mixing from breaking oceanic internal waves drives a vertical transport of water,
heat and other climatically important tracers in the ocean, thereby playing an important role …

This study presents the global climate model IPSL‐CM6A‐LR developed at Institut Pierre‐
Simon Laplace (IPSL) to study natural climate variability and climate response to natural and …

This paper describes the main characteristics of CNRM‐CM6‐1, the fully coupled
atmosphere‐ocean general circulation model of sixth generation jointly developed by …

Abstract Dansgaard–Oeschger (D–O) events, millennial-scale climate oscillations between
stadial and interstadial conditions (of up to 10–15∘ C in amplitude at high northern …

Turbulent mixing in the ocean is key to regulate the transport of heat, freshwater and
biogeochemical tracers, with strong implications for Earth's climate. In the deep ocean, tides …

We present results from an ensemble of eight climate models, each of which has carried out
simulations of the early Eocene climate optimum (EECO,∼ 50 million years ago). These …

Vertical mixing is often regarded as the Achilles' heel of ocean models. In particular, few
models include a comprehensive and energy‐constrained parameterization of mixing by …

Based on the fifth phase of the Coupled Model Intercomparison Project (CMIP5)-generation
previous Institut Pierre Simon Laplace (IPSL) Earth system model, we designed a new …

The ocean is one of the most important sinks for anthropogenic CO2 emissions. Here, I use
an ocean circulation inverse model (OCIM), ocean biogeochemical models, and pCO2 …

The effects of horizontal resolution and wave drag damping on the semidiurnal M 2 tidal
energetics are studied for two realistically-forced global HYbrid Coordinate Ocean Model …