Population connectivity is inherently bio-physical: it is determined by physical transport and
dispersion, as well as biological processes such as timing of spawning, larval behavior, and …

The oceanic bottom boundary layer extracts energy and momentum from the overlying flow,
mediates the fate of near-bottom substances, and generates bedforms that retard the flow …

Seasonal to interannual variability of satellite derived chlorophyll‐a over the Patagonia shelf
and shelf break in the western South Atlantic are studied based on 7 years of ocean‐color …

Efficient sampling of coastal ocean processes, especially mechanisms such as upwelling
and internal waves and their influence on primary production, is critical for understanding …

Since 1992, upper ocean ADCP current data between New York and Bermuda have been
gathered from the container ship Oleander to identify long‐term changes in the shelf, slope …

Ageostrophic secondary circulation (ASC) in frontal data sets have been previously
diagnosed using only adiabatic versions of Omega equations. This study includes the effect …

Ocean fronts represent productive regions of the ocean, but predator–prey interactions
within these features are poorly understood partially due to the coarse-scale and biases of …

The Patagonian shelf break marks a transition between relative warm‐fresh shelf waters and
relative cold‐salty Subantarctic Water advected northward by the Malvinas Current. From …

Along density surfaces, nutrient concentrations in the Gulf Stream are elevated relative to
concentrations to either side of the current. We assess the source of these elevated nutrient …

We present observations from deployments of a microstructure turbulence instrument (the
Towed Microstructure and Auxiliary Sensor Instrument) aboard a pumping profiling vehicle …