The Southern Ocean plays a pivotal role in the global overturning circulation, a system of surface and
deep currents linking all oceans and one of the fundamental determinants of the planet's climate.
Not exact matches
These revealed a surprising
link between stratospheric winds and ocean
currents as
deep as 2 kilometers beneath the waves.
Since
deeper waters will be warmer, there is a possible
link to the global ocean circulating
currents that results in warmer water in polar regions.
EMBRACE aims to significantly improve the parameterization of
deep convection and its
link to important modes of tropical climate variability in
current ESMs.
Specifically, if the variability controlling the
current hiatus is
linked to longer - term sequestration of heat into the
deep ocean, this might require us to recalibrate future projections.
Because of this second difficulty, a measure of the
Deep Western Boundary
Current (DWBC) transport has traditionally been considered a shortcut to the measure of the AMOC: while the upper limb of the AMOC was considered inextricably
linked to the much more energetic wind - driven circulation, the lower limb was considered to be «channeled» through the DWBC.