The polar gyres of the Southern Ocean
Collaborators: Andrew Thompson
Characterizing the transport and modification of Circumpolar Deep Water across the gyres of the Southern Ocean.
The transport and modification of Circumpolar Deep Water (CDW) is a key component of the global ocean overturning circulation. CDW is primarily found within the Antarctic Circumpolar Current (ACC) and is a mixture of deep waters from all adjacent ocean basins. Under the influence of strong westerly winds and the Earth’s rotation, this deep water flows upward towards the surface and subsequently splits into two branches: a northward branch, which eventually replenishes the deep waters formed in the northern Atlantic, and a southward branch that contributes to the formation of Antarctic Bottom Water. This work is mainly concerned with the southward branch that transports relatively warm CDW to the continental slope of Antarctica.
Though many studies have investigated the dynamics of the Ross and Weddell gyres in isolation, their role as delivery mechanisms for CDW remains largely unexplored. To address this gap in our understanding, we aim to conduct a series of process-based modeling studies to elucidate the key processes that control the modification of CDW across these gyres. In doing so, we seek to address the following questions
- What is the relative importance of wind-driven upwelling, isopycnal eddy stirring and surface buoyancy fluxes in setting the shape and depth of isopycnals across these gyres?
- How does poleward heat transport across these gyres respond to changes in surface heat, freshwater or momentum fluxes?
Assessing the potential importance of polar gyre asymmetry in the Southern Ocean overturning
In addition to providing a pathway for deep ocean heat transport to the Antarctic margin, the polar gyres of the Southern Ocean also play an important role in the upwelling of CDW and its transformation into either intermediate or abyssal. In this capacity, these gyres are crucial cogs in the overturning circulation of the Southern Ocean. A key aspect of these gyres is their tendency to flatten isopycnals within the ocean interior (Figure 2). However, this detail is often neglected in the canonical zonally-averaged view of the Southern Ocean residual overturning circulation, which typically assumes isopycnal slopes are uniform with latitude. Furthermore, the current overturning framework also neglects inter-basin asymmetries in ocean stratification. Poleward of the circumpolar current, isopycnal depths can differ by hundreds of meters at a given latitude, with the Weddell Sea having much shallower isopycnals than the Ross Sea. Thus, the pathways of upwelled CDW differ substantially across the Ross and Weddell Seas.
Since that water masses created within these gyres are exported globally, these regional asymmetries in stratification may have far-reaching effects for the overturning circulation of the global ocean. As before, we aim to diagnose the importance of the gyre asymmetries by using a suite of idealized models, ranging from simple box models to more complex general circulation models.
Publications: We are at the beginning stages of this project, so stay tuned!