Ocean boundary current systems are key components of the climate system, are home to
highly productive ecosystems, and have numerous societal impacts. Establishment of a …

Frontal eddies form on the shoreward edge of boundary currents, on average at weekly
intervals and can last up to several weeks. This duration allows zooplankton production and …

Long-term demographic studies at biogeographic transition zones can elucidate how body
size mediates disturbance responses. Focusing on subtropical reefs in eastern Australia, we …

During 2022, extreme rainfall occurred across southeast Australia, making it the wettest year
on record. The oceanic impact of extreme rainfall events in normally 'dry'regions is not well …

Details of the chlorophyll-a (Chl-a) distribution in the water of the Zhoushan archipelago
were analyzed based on data from the panchromatic multispectral sensor (PMS) of the …

Given the importance of western boundary currents over a wide range of scales in the
ocean, it is crucial that we understand their dynamics to accurately predict future changes …

In western boundary current systems, sharp velocity gradients between the poleward flowing
jet and coastal waters generally act to inhibit cross‐shelf exchange. Downstream of jet …

The world's oceans are undergoing rapid, regionally specific warming. Strengthening
western boundary currents play a role in this phenomenon, with sea surface temperatures …

Mesoscale cyclonic eddies are known to be highly productive. Less well‐known are the
dynamics and productivity of smaller cyclonic eddies, known as frontal eddies, that form on …

Some dramatic consequences of climate change are caused by shifting species interactions
and associated changes to trophic structure and energy flow. In coastal ecosystems, the …