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The fall transition of Oregon shelf watersReid, Brad 17 October 1986 (has links)
A long and gradual transition between the summer and winter
oceanic regimes was observed off Oregon during the autumn of 1980.
Hydrographic sections and a single current meter mooring between
August and December show the ocean possessed characteristics during
fall that have not been observed during other seasons: a slow ascension of
the poleward undercurrent and the appearance of a large bottom
boundary layer.
The decay of summer's southward surface flow was achieved by a
series of modest northward wind events during late summer as the effects
of southward winds were becoming diminished. The northward wind
events had progressively stronger influence on surface currents. The
barotropic current fluctuations that are a signature of the summer regime
continued during the transitional period. The weekly-to-monthly
averaged flow was barotropic during much of the transition.
Hydrographic sections and time series of alongshore current shear
and temperature show that the leveling of the frontal layer was achieved
gradually over a two month time scale.
The winter regime was established during eleven days of
continuous northward wind stress in early November. / Graduation date: 1987 Read more
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The time-averaged circulation of the north Pacific Ocean : an analysis based on inverse methodsZaron, Edward D. 25 August 1995 (has links)
The time-averaged velocity field in the North Pacific was estimated in two
sets of inverse calculations. The planetary geostrophic equations were the basis for
dynamical models of the flow in each case. The inverse estimates of the circulation
were obtained by minimizing a positive-definite cost function, which measured the
inconsistency of the model's predictions against a set of observations comprised of
a large, high-quality hydrographic data set, and surface fluxes of heat, fresh water,
and momentum.
In the first part of this work, four solution methods for the generalized inverse
of a linear planetary geostrophic model of the North Pacific are compared.
A conjugate gradient solver applied to the equation for the generalized inverse,
expressed in terms of a representer expansion, was the most computationally efficient
solution method. The other methods, in order of decreasing efficiency, were,
a conjugate gradient descent solver (preconditioned with the inverse of the model
operators), a direct solver for the representer coefficients, and a second conjugate
gradient descent solver (preconditioned so that the diagonal elements of the cost
Redacted for Privacy
function Hessian were unity). All but the last method were successful at minimizing
the penalty function.
Inverse estimates of the circulation based on the linear planetary geostrophic
model were stable to perturbations in the data, and insensitive to assumptions
regarding the model forcing and boundary condition uncertainties. A large calculation,
which involved approximately 18,000 observations and 60,000 state variables,
indicated that the linear model is remarkably consistent with the observations.
The second part of this work describes an attempt to use a nonlinear planetary
geostrophic model (which included realistic bottom topography, lateral momentum
mixing, out-cropping layers, and air-sea fluxes of heat, freshwater, and
momentum) to assimilate the same hydrographic data set as above. Because of
the nonlinearity in the model, descent methods (rather than a representer-based
method) were used to solve the inverse problem. The nonlinearity of the model and
the poor conditioning of the cost function Hessian confounded the minimization
process. A solver for the tangent-linearization of the planetary geostrophic system
should be used as a preconditioner if calculations of this type are attempted in the
future. / Graduation date: 1996 Read more
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