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

Abstract The Western Indian Ocean (WIO) is a region where biodiversity is increasingly
being impacted by anthropogenic marine debris, but information is scattered widely in the …

An observed warming of the Tasman Sea in recent decades has been linked to a poleward
shift of the maximum wind stress curl, and a strengthening of the poleward flow along the …

The upper ocean circulation of the Pacific and Indian Oceans is connected through both the
Indonesian Throughflow north of Australia and the Tasman leakage around its south. The …

Coupled ocean–atmosphere simulations are carried out for the Mozambique Channel, the
Agulhas Current system, and the Benguela upwelling system to assess the ocean surface …

The Southern Ocean Subtropical Front (STF) is thought to play a key role in the global
climate system. Theory suggests that the latitude of the STF regulates the volume of saline …

The interoceanic transfer of seawater between the Indian Ocean and the Atlantic,'Agulhas
leakage', forms a choke point for the overturning circulation in the global ocean. Here, by …

For the past 50 years it has been assumed that the principal pathway for the deep limb of the
Atlantic Meridional Overturning Circulation (AMOC) is the Deep Western Boundary Current …

The shedding of Agulhas rings is the primary process connecting the Indian and Atlantic
oceans. The rings transport warm and salty waters that feed the surface limb of the Atlantic …

Agulhas leakage, the transport of warm and salty waters from the Indian Ocean into the
South Atlantic, has been suggested to increase under anthropogenic climate change, due to …