The 5-year Ocean Regulation of Climate by Heat and Carbon Sequestration and Transports
(ORCHESTRA) programme and its 1-year extension ENCORE (ENCORE is the National …

Satellite radar interferometry data reveals that the grounding line of Petermann Glacier,
Greenland migrates by several kilometers during the tidal cycle, bringing pressurized …

Recent simulations suggest that submesoscale motions with scales smaller than 30 km and
frequencies greater than 1 day− 1 drive upward vertical heat transport. These simulations …

During the last glacial period (120–12 ka), the Laurentide ice sheet discharged large
numbers of icebergs into the North Atlantic. These icebergs carried sediments that were …

The upper‐ocean relative vorticity has been found to be cyclonically skewed, but altimetry
observations indicate that long‐lifespan mesoscale eddies tend to be anticyclonic. We are …

Abstract In the North Atlantic, relatively coarse grained sediments can be found periodically
throughout sediment cores spanning the Last Glacial Period. These sediments were rafted …

This study presents numerical analogs of laboratory experiments designed to explore the
interaction of broad geophysical flows with irregular small-scale bathymetry. The previously …

Observations indicate that symmetric instability is active in the East Greenland Current
during strong northerly wind events. Theoretical considerations suggest that mesoscale …

Density staircases are observed in an idealized model of a deep western boundary current
upon crossing the equator. We propose that the staircases are generated by the excitement …

The oceans play a central role in regulating climate by absorbing carbon dioxide from the
atmosphere and sequestering heat through ocean biogeochemical (BGC) processes …