It has been suggested that the upwelling branch of the abyssal overturning circulation is associated with strong flows driven by abyssal mixing along ...

We incorporate memory into a climate emulator by using linear response functions represented as a combination of spatial and temporal modes. Previous ...

We demonstrate a data-driven method for the emulation of distributions of monthly averaged temperature and relative humidity from Earth system models ...

Estimation of the probability of extreme events under climate change is both challenging and crucial for risk management of natural disasters. Earth S...

Current eddy-permitting and eddy-resolving ocean models require explicit dissipation to prevent a spurious accumulation of enstrophy at the grid scale...

Geostrophic eddies exert a strong control on the ocean uptake of heat and carbon, but they have proved hard to accurately parameterize in climate simu...

The middepth ocean, spanning from 1 to 3 kilometers in depth, is characterized by a remarkably exponential stratification profile. Existing conceptual...