Two decades of high-resolution satellite observations and climate modeling studies have
indicated strong ocean–atmosphere coupled feedback mediated by ocean mesoscale …

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 …

Gene flow governs the contemporary spatial structure and dynamic of populations as well as
their long-term evolution. For species that disperse using atmospheric or oceanic flows …

This paper investigates marine heatwave (MHW) characteristics in New Zealand's Earth
System Model (NZESM) simulations for present-day conditions and how they are projected …

The concept of utilizing a large temperature difference (> 20° C) between the surface and
deep seawater to generate electricity, known as the ocean thermal energy conversion …

Abstract The Atlantic Meridional Overturning Circulation (AMOC) is frequently used to
diagnose the state of the North Atlantic circulation, but as an integrated quantity the AMOC …

Although global warming is leading to more frequent mass coral bleaching events
worldwide, parts of the Great Barrier Reef (GBR) have consistently escaped severe coral …

Abstract The Southern Indian Ocean (20–120° E, 70–30° S) hosts an exceptional
biodiversity that contributed to the inscription of the French and Australian natural reserves …

Abstract The Atlantic Meridional Overturning Circulation is the main driver of northward heat
transport in the Atlantic Ocean today, setting global climate patterns. Whether global …