Type of Document	Dissertation
Author	Faure, Vincent
Author's Email Address	vfaure@fsu.edu
URN	etd-07102009-110119
Title	Deep Circulation in the Eastern South Pacific
Degree	Doctor of Philosophy
Department	Oceanography, Department of
Advisory Committee	Advisor Name Title Kevin Speer Committee Chair Doron Nof Committee Member Georges Weatherly Committee Member Philip Froelich Committee Member William Landing Committee Member Carol Anne Clayson Outside Committee Member
Keywords	Deep Currents Eastern South Pacific Ocean Ocean Tracers Helium Inverse Problem Advection-Diffusion
Date of Defense	2008-04-25
Availability	unrestricted
Abstract It has been suggested in older and recent literature that a broad deep eastern boundary flow is linking the equatorial Pacific Ocean to the Southern Ocean. The depth range of this flow corresponds to the Pacific Deep Water (2500m) where it is suggested by the distribution of primordial 3He originating from the East Pacific Rise. In this study, we propose to use a large set of data along with inverse techniques to estimate the stationary advection and diffusion of water properties and tracer concentrations (potential vorticity, potential temperature, salinity, dissolved oxygen and silica concentration) in the area of interest. The various data are combined into an new inverse model first developed by McKeague et al. (2005), Herbei et al. (2006). The model uses a forward advection-diffusion model and Markov Chain Monte-Carlo techniques to give estimates of velocities along and across surfaces of neutral density as well as isopycnal diffusivities. It is composed of 9 layers between the 27.4 and 28 neutral densities. The circulation in the upper layers of the model compares well with direct independent estimates of velocities from subsurface float trajectories (WOCE and Argo). We investigate the water exchange in the deeper layers in regards to the 3He distribution along the Eastern boundary and its mixing with the Antarctic Circumpolar Current. The model is able to estimate vertically dependent rates of oxygen utilization as well as lateral eddy diffusivities of tracers.
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