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dc.contributor.advisor Lozier, M. Susan en_US
dc.contributor.author Palter, Jaime Beth en_US
dc.date.accessioned 2007-08-24T14:53:19Z
dc.date.available 2007-08-24T14:53:19Z
dc.date.issued 2007-07-26 en_US
dc.identifier.uri http://hdl.handle.net/10161/386
dc.description Dissertation en_US
dc.description.abstract Using a combination of hydrographic data and the trajectories and profiles of isobaric floats, this dissertation evaluates the connections between remote regions in the North Atlantic. First, I establish that the production and advection of the North Atlantic Subtropical Mode Water (STMW) introduces spatial and temporal variability in the subsurface nutrient reservoir of the subtropical gyre. As the mode water is formed, its nutrients are depleted by biological utilization. When the depleted water mass is exported to the gyre, it injects a wedge of low-nutrient water into the upper layers of the ocean. Contrary to intuition, cold winters that promote deep convective mixing and vigorous mode water formation may diminish downstream primary productivity by altering the subsurface delivery of nutrients. Next, the source of elevated nutrient concentrations in the Gulf Stream is assessed. The historical hydrographic data suggest that imported water advected into the Gulf Stream via the tropics supplies an important source of nutrients to the Gulf Stream. Because the high nutrients are likely imported from the tropics, diapycnal mixing need not be invoked to explain the Gulf Stream's high nutrient concentrations, as had been previously hypothesized. Furthermore, nutrients do not increase along the length of the Stream, as would be expected with strong diapycnal mixing.Finally, profiling float data are used to investigate how the Labrador Sea Water enters the Deep Western Boundary Current, one of the primary pathways by which it exits the subpolar gyre. With the trajectories and profiles of an extensive array of P-ALACE floats I evaluate three processes for their role in the entry of Labrador Sea Water in the Deep Western Boundary Current (DWBC): 1) LSW is formed directly in the DWBC, 2) Eddies flux LSW laterally from the interior Labrador Sea to the DWBC, and 3) A horizontally divergent mean flow advects LSW from the interior to the DWBC. Each of the three processes has the potential to remove heat from the boundary current, and both the formation of LSW directly in the boundary current and the eddy heat flux are possible sources of interannual variability in the exported LSW product. en_US
dc.format.extent 4830172 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.subject Physical Oceanography en_US
dc.subject Biology, Oceanography en_US
dc.subject North Atlantic en_US
dc.subject nutrients en_US
dc.subject ocean color en_US
dc.subject Gulf Stream en_US
dc.subject Labrador Sea Water en_US
dc.subject Meridional Overturning Circulation en_US
dc.title On the Horizontal Advection and Biogeochemical Impacts of North Atlantic Mode Waters and Boundary Currents en_US
dc.type Dissertation en_US
dc.department Earth and Ocean Sciences en_US

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