Ocean net primary production (NPP) results from CO2 fixation by marine phytoplankton,
catalysing the transfer of organic matter and energy to marine ecosystems, supporting most …

Abstract Current Earth system models (ESMs) project dramatic slowing (28–42% by 2100) of
Atlantic Meridional Overturning Circulation and Southern Meridional Overturning Circulation …

The decline in ocean primary production is one of the most alarming consequences of
anthropogenic climate change. This decline could indeed lead to a decrease in marine …

Climatic changes have decreased the stability of the Gulf Stream (GS), increasing the
frequency at which its meanders interact with the Mid‐Atlantic Bight (MAB) continental shelf …

We examine the effects of the submesoscale in mediating the response to projected
warming of phytoplankton new production and export using idealized biogeochemical …

The Gulf of St. Lawrence (GSL), along with the St. Lawrence Estuary, is the largest estuarine
system in North America. It is a biologically productive sea and an important fishing ground …

Subsurface nutrients on the Scotian Shelf, an ocean region at the convergence of the
subpolar and subtropical western boundary currents (ie, Labrador Current (LC) and Gulf …

The high rate of biological productivity in the North Atlantic is stimulated by the advective
supply of nutrients into the region via the Gulf Stream (nutrient stream). It has been proposed …

Anthropogenic climate change footprints in the ocean go beyond the mixed layer depth, with
considerable impacts throughout mesopelagic and deep‐ocean ecosystems. Yet, little is …

Earth system models indicate that the Subarctic Atlantic Ocean ecosystems are uniquely
sensitive to global warming. Nutrients, phytoplankton biomass, and phytoplankton …