Article-Journal

Mesoscale eddies contain the bulk of the ocean’s kinetic energy (KE), but fundamental questions remain on the cross-scale KE transfers …

A method for estimating 26°N overturning from time-varying satellite altimetry and time-averaged boundary profiles of dynamic height.

Water-mass transformation by turbulent mixing is a key part of the deep-ocean overturning, as it drives the upwelling of dense waters …

A model-based evaluation of how the choice of referencing geostrophic velocities at AMOC transport mooring arrays can influence the resultant transport estimate, with a focus on the MOVE latitude of 16°N and the RAPID latitude of 26.5°N.

Mesoscale eddies are ubiquitous dynamical features that tend to propagate westward and disappear along ocean western boundaries. Using …

The Labrador Sea is a fascinating and difficult environment in which to work. In the winter, wind speeds can gust upwards of 200 km/hr, …

A 4-month glider mission was analyzed to assess turbulent dissipation in an anticyclonic eddy at the western boundary of the …

Update on the Atlantic meridional overturning circulation (AMOC) in the annual State of the Climate report. This issue includes estimates using XBT data compared against mooring-derived transport estimates.

Determining whether the Atlantic Meridional Overturning Circulation (AMOC)’s transport is in decline is challenging due to the …