Upwelling and downwelling play an important role in transporting the heat, carbon, and nutrients that affect Earth’s climate. Many studies have focused on these vertical motions in the ocean. This includes eastern boundary currents and the Southern Ocean.
Previous research has suggested that western boundary currents (WBCs) are associated with vertical water transport. But the strong presence and dynamics of vertical motions in the main WBC areas have not been described to date. Because powerful horizontal water movement and eddies associated with WBCs make it hard to detect direct WBC-associated vertical motions.
In a new study, scientists distinguished patterns across various ocean data sets. They looked at vertical velocity using six ocean data sets spanning January 1992 to December 2009 under different ocean circulation models. Then they categorized five major subtropical WBC regions which are Kuroshio, Gulf Stream, Agulhas, East Australian and Brazil currents.
Strong subsurface upwelling was seen in all major WBC areas in all six of the data sets. Scientists said that upwelling systems are necessary for the WBCs to be in geostrophic balance. They found that vertical motion in the WBC areas is relatively deep and the WBC upwelling can reach the surface mixed layer. This finding suggests that in subtropical regions, WBC upwelling plays a role in the vertical movement of heat and carbon. This could be significant in heat and carbon regulation in the upper ocean and atmosphere over long timescales.
This upwelling and associated circulation in subtropical regions suggest that WBC upwelling is a path through which various biological, chemical and physical processes travel. Scientists note that more research is needed to better understand the dynamics of WBC upwelling and the role it plays in the climate system.
