Abstract The Southern Ocean has warmed substantially, and up to early 21st century,
Antarctic stratospheric ozone depletion and increasing atmospheric CO 2 have conspired to …

Phytoplankton blooms in coastal oceans can be beneficial to coastal fisheries production
and ecosystem function, but can also cause major environmental problems,—yet detailed …

A holistic review is given of the Southern Ocean dynamic system, in the context of the crucial
role it plays in the global climate and the profound changes it is experiencing. The review …

The ocean absorbs> 90% of anthropogenic heat in the Earth system, moderating global
atmospheric warming. However, it remains unclear how this heat uptake is distributed by …

How the ocean circulation changes in a warming climate is an important but poorly
understood problem. Using a global ocean model, we decompose the problem into distinct …

Western boundary currents (WBCs) of the Southern Hemisphere transport heat poleward
and are regions of rapid ocean warming. However, the mechanisms responsible for the …

The severity of marine heatwaves (MHWs) that are increasingly impacting ocean
ecosystems, including vulnerable coral reefs, has primarily been assessed using remotely …

Mesoscale ocean eddies, an important element of the climate system, impact ocean
circulation, heat uptake, gas exchange, carbon sequestration and nutrient transport. Much of …

Climate change is expected to elicit widespread alterations to nutrient and light supply,
which interact to influence phytoplankton growth and their seasonal cycles. Using 25 years …

Coupled climate simulations that span several hundred years cannot be run at a high‐
enough spatial resolution to resolve mesoscale ocean dynamics. Recently, several studies …