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  • About
  • The Global ETD Search service is a free service for researchers to find electronic theses and dissertations. This service is provided by the Networked Digital Library of Theses and Dissertations.
    Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
1

Ecclesial themes in the theological methodologies of Edward Farley and Karl Barth

Leach, Robert Timothy, January 1997 (has links)
Thesis (M.A.)--Gordon-Conwell Theological Seminary, South Hamilton, Mass., 1997. / Abstract and vita. Includes bibliographical references (leaves [90]-97).
2

Belief in the integrity of the Lowell working women an examination of Harriet Farley's writings /

Crowley, Kathleen M. January 2006 (has links)
Thesis (M.A.)--Villanova University, 2006. / History Dept. Includes bibliographical references.
3

The political career of James A. Farley

Swindeman, Earlene, 1941- January 1967 (has links)
No description available.
4

Current models in Roman, Lutheran, and Reformed prolegomena exposition, analysis, and programmatic assessment /

Lumpp, David Arthur. January 1989 (has links)
Thesis (Th. D.)--Concordia Seminary, 1989. / Includes bibliographical references (leaves 307-322).
5

Meter-scale waves in the E-region Ionosphere: cross-scale coupling and variation with altitude

Young, Matthew Adam 12 July 2019 (has links)
The Sun ionizes a small fraction of Earth's atmosphere above roughly 60 km, producing the plasma that constitutes the ionosphere. Radio signals passing through the ionosphere scatter off of plasma density structures created by the Farley-Buneman instability (FBI). While numerous studies have characterized the FBI's intrinsic nature, its evolution within the broader context of the surrounding plasma remains enigmatic. This dissertation answers two fundamental questions about the FBI: How does it interact with density gradients? How does its non-linear evolution depend on the background plasma? The fourth chapter examines the combined development of the FBI and the gradient drift instability (GDI) using a 2-D simulation of the equatorial ionosphere. A half-kilometer wave perturbs a plasma layer perpendicular to the ambient magnetic field, causing the perturbed layer to develop GDI waves along the gradient aligned with the ambient electric field, as well as FBI waves in a region where the total electric field exceeds a certain threshold. Early radar observations suggested that these two instabilities were distinct phenomena; the reported results illustrate their coupled nature. The fifth chapter presents 2-D simulations in which a one-kilometer plasma wave develops an electric field large enough to trigger meter-scale waves. Such large-scale waves arise via the GDI within the daytime ionospheric gradient around 100-110 km. Typical ionospheric radars only observe meter-scale irregularities but observations show meter-scale waves tracing out larger structures. Simulated meter-scale FBI in the troughs and crests of kilometer-scale GDI matches radar observations of the daytime equatorial ionosphere, answers a question about electric-field saturation raised by rocket observations in the 1980s, and predicts an anomalous cross-field conductivity important to magnetosphere-ionosphere (M-I) coupling. The sixth chapter of this dissertation presents 3-D simulations of the FBI at a range of altitudes and driving electric fields appropriate to the auroral ionosphere, where it plays a role in M-I coupling. Research has thoroughly established the linear theory of FBI but rigorous analysis of radar measurements requires an understanding of the turbulent stage. These simulations explain the change in instability flow direction with altitude, with regard to the direction of background plasma flow.

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