Index Catalog // ScholarsArchive@OSU

Ocean to ocean on horseback : being the story of a tour in the saddle from the Atlantic to the Pacific; with especial reference to the early history and development of cities and towns along the route; and regions traversed beyond the Mississippi

Creator:: Glazier, Willard W., 1841-1905
Abstract:: Gerald W. Williams Collection
Resource Type:: Book
Full Text:: ANY OF CAPTAIN GLA· ZIER'S BOOKS RHOULD A DlJRESR ~ THE PUBLISHERS. OCEAN TO OCEAN ON

The story of Oregon and its people

Creator:: Chapman, Charles Hiram, 1859-
Abstract:: Gerald W. Williams Collection
Resource Type:: Book
Full Text:: Bv CHARLES H. CHAPMAN, PH. D. CHICAGO o. P. BARNES, PUBLISHER r Copyright, 1909, BY 0. P

Forcing a three-dimensional, hydrostatic, primitive-equation model for application in the surf zone : 1. formulation

Creator:: Newberger, P. A. and Allen, John S.
Abstract:: An Eulerian analysis for wave forcing of three-dimensional (3D) wave-averaged mean circulation in the surf zone is presented. The objective is to develop a dynamically consistent formulation for applications in a 3D primitive equation model. The analysis is carried out for the case of shallow-water linear waves interacting with wave-averaged...
Resource Type:: Article
Full Text:: problems, Rev. Geophys., 20, 851–875. Newberger, P. A., and J. S. Allen (2007), Forcing a three

Forcing a three-dimensional, hydrostatic, primitive-equation model for application in the surf zone : 2. application to DUCK94

Creator:: Newberger, P. A. and Allen, John S.
Abstract:: A three‐dimensional primitive‐equation model for application to the nearshore surf zone has been developed. This model, an extension of the Princeton Ocean Model (POM), predicts the wave‐averaged circulation forced by breaking waves. All of the features of the original POM are retained in the extended model so that applications can...
Resource Type:: Article
Full Text:: instability. Citation: Newberger, P. A., and J. S. Allen (2007), Forcing a three-dimensional, hydrostatic

An inertial subrange in microstructure spectra

Creator:: Newberger, P. A. and Caldwell, Douglas R.
Abstract:: An inertial subrange was found in spectra calculated from vertical profiles of temperature gradient recorded in the bottom boundary layer of the Oregon shelf. Spectra were calculated for 53-cm vertical segments. An ensemble average of those spectra that were fully resolved and had high Cox number was compared to the...
Resource Type:: Article
Full Text:: Spectra P. A. NEWBERGER AND D. R. CALDWELL School of Oceanography, Oregon State University, Corvallis

On Symmetric Instabilities in Oceanic Bottom Boundary Layers

Creator:: Allen, J. S. and Newberger, P. A.
Abstract:: Model studies of two-dimensional, time-dependent, wind-forced, stratified downwelling circulation on the continental shelf have shown that the near-bottom offshore flow can develop time- and space-dependent fluctuations involving spatially periodic separation and reattachment of the bottom boundary layer and accompanying recirculation cells. Based primarily on the observation that the potential vorticity...
Resource Type:: Article
Full Text:: AND P. A. NEWBERGER College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis

Downwelling Circulation on the Oregon Continental Shelf. Part I: Response to Idealized Forcing

Creator:: Allen, J. S. and Newberger, P. A.
Abstract:: Time-dependent downwelling on the Oregon continental shelf is studied with a two-dimensional approximation, that is, spatial variations across shelf and with depth, using the Blumberg-Mellor, finite-difference, stratified, hydrostatic, primitive equation model. The time-dependent response of a coastal ocean at rest to constant, downwelling-favorable wind stress is examined. Topography and stratification...
Resource Type:: Article

On Intermediate Models for Stratified Flow

Creator:: Allen, J. S. and Newberger, P. A.
Abstract:: Intermediate models contain physics between that in the primitive equations and that in the quasigeostrophic equations. The specific objective here is to investigate the absolute and relative accuracy of several intermediate models for stratified flow by a comparison of numerical finite-difference solutions with those of the primitive equations (PE) and...
Resource Type:: Article

On Intermediate Models for Barotropic Continental Shelf and Slope Flow Fields. Part II: Comparison of Numerical Model Solutions in Doubly Periodic Domains

Creator:: Barth, J. A., Allen, J. S., and Newberger, P. A.
Abstract:: As part of a program to improve understanding of the dynamics of the complicated, vigorous eddy and jet flow fields recently observed over the continental shelf and slope, we investigate the potential of intermediate models for use in both process and data assimilation studies of these flows. Intermediate models incorporate...
Resource Type:: Article

Nonlinear shear instabilities of alongshore currents over barred beaches

Creator:: Slinn, Donald N., Allen, J. S., Newberger, P. A., and Holman, Robert A.
Abstract:: The nonlinear dynamics of finite amplitude shear instabilities of alongshore currents in the nearshore surf zone over barred beach topography are studied using numerical experiments. These experiments extend the recent study of Allen et al. [1996], which utilized plane beach (constant slope) topography by including shore-parallel sandbars. The model involves...
Resource Type:: Article

ScholarsArchive@OSU

Ocean to ocean on horseback : being the story of a tour in the saddle from the Atlantic to the Pacific; with especial reference to the early history and development of cities and towns along the route; and regions traversed beyond the Mississippi

The story of Oregon and its people

Forcing a three-dimensional, hydrostatic, primitive-equation model for application in the surf zone : 1. formulation

Forcing a three-dimensional, hydrostatic, primitive-equation model for application in the surf zone : 2. application to DUCK94

An inertial subrange in microstructure spectra

On Symmetric Instabilities in Oceanic Bottom Boundary Layers

Downwelling Circulation on the Oregon Continental Shelf. Part I: Response to Idealized Forcing

On Intermediate Models for Stratified Flow

On Intermediate Models for Barotropic Continental Shelf and Slope Flow Fields. Part II: Comparison of Numerical Model Solutions in Doubly Periodic Domains

Nonlinear shear instabilities of alongshore currents over barred beaches

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