Browsing by Subject "Lagrangian pathways"

The Atlantic Meridional Overturning Circulation (AMOC) is characterized as a northward upper limb that carries warm near-surface waters from southern latitudes to the subpolar North Atlantic, and a southward lower limb that transports cold deep waters back to the southern latitudes. Due to its special role in distributing heat, carbon and water masses globally, AMOC as an essential part in the climate system, has long been a strong focus within the ocean community. For decades, AMOC variability has been attributed to changes in deep water production at high latitudes in the North Atlantic through a geostrophic response in the Deep Western Boundary Current (DWBC), the assumed major export pathway of the deep waters. However, recent Lagrangian studies have revealed the importance of eddy-driven interior pathways, challenging the traditional DWBC-dominated spreading pattern, hence the linkage between deep water formation and AMOC. Under the new spreading scheme of the deep waters, this dissertation provides an extended Lagrangian analysis on the spreading pathways of two major deep waters, Labrador Sea Water (LSW) and Iceland Scotland Overflow Water (ISOW), and re-examines the relationships among deep water production, deep water export and the strength of AMOC.

A Lagrangian simulation of newly-formed LSW in an ocean/sea ice model (1/4°) reveals strong recirculation of the water mass in the subpolar gyre, with a small portion exported to the subtropical gyre through an advective-diffusive pathway. Furthermore, no significant correlation between LSW production and its Lagrangian export to the subtropical gyre is found on interannual to decadal time scales, suggesting a negligible or at best modest impact of LSW production on the subtropical AMOC.

In a combined Lagrangian and Eulerian frame, a first comprehensive description of ISOW spreading branches in the eastern North Atlantic is presented with observational data and output from an eddy-resolving ocean model. The major export pathway for ISOW is shown to be the southward branch into the Western European Basin, instead of the branch through the Charlie Gibbs Fracture Zone, the traditional DWBC pathway. Interestingly, these two branches show compensating relationships in the model, a result assumed to reflect these pathways’ interactions with the North Atlantic Current in magnitude and/or position shift.

Finally, with output from ocean circulation models and an ocean reanalysis dataset, the meridional connection of the deep water transport anomalies and their relationships with AMOC are assessed. It is shown that deep water transport anomalies in the subpolar gyre do not propagate coherently to the subtropical gyre in general, particularly so for Upper North Atlantic Deep Water (UNADW, containing LSW). Furthermore, while UNADW and Lower North Atlantic Deep Water (LNADW, containing overflow waters) transports in the subpolar gyre are linked to local AMOC strength on interannual to decadal time scales, in the subtropical gyre only LNADW transport variability shows this linkage, the latter results consistent with observations. These analyses suggest a dominance of gyre-specific, rather than basin-wide, mechanisms for water mass transport variability. Thus, latitudinal coherence in AMOC is likely unrelated to continuity in water mass transport anomalies. An exception to this generalization is possible with strong LNADW transport events.

Taken together, this dissertation emphasizes the importance of interior pathways to the export of deep waters from the subpolar to the subtropical gyre. It also reveals a tenuous linkage between deep water production and AMOC strength at subtropical latitudes on interannual to decadal time scales.

In response to the differential heating of the earth, atmospheric and oceanic flows constantly act to carry surplus energy from low to high latitudes. In the ocean, this poleward energy flux occurs as part of the large scale meridional overturning circulation: warm, shallow waters are transported to high latitudes where they cool and sink, then follow subsurface pathways equatorward until they are once again upwelled to the surface and reheated. In the North Atlantic, the upper limb of this circulation has always been explained in simplistic terms: the Gulf Stream/North Atlantic Current system carries surface waters directly to high latitudes, resulting in elevated sea surface temperatures in the eastern subpolar gyre, and, because the prevailing winds sweeping across the Atlantic are warmed by these waters, anomalously warm temperatures in Western Europe. This view has long been supported by Eulerian measurements of North Atlantic sea surface temperature and surface velocities, which imply a direct and continuous transport of surface waters between the two gyres. However, though the importance of this redistribution of heat from low to high latitudes has been broadly recognized, few studies have focused on this transport within the Lagrangian frame.

The three studies included in this dissertation use data from the observational record and from a high resolution model of ocean circulation to re-examine our understanding of upper limb transport between the subtropical and subpolar gyres. Specifically, each chapter explores intergyre Lagrangian pathways and investigates the impact of those pathways on subpolar property fields. The findings from the studies suggest that intergyre transport pathways are primarily located beneath the surface and that subtropical surface waters are largely absent from the intergyre exchange process, a very different image of intergyre transport than that compiled from Eulerian data alone. As such, these studies also highlight the importance of including 3d Lagrangian information in examinations of transport pathways.