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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

Interpretation of force vector recorder data describing buoy system dynamics

Padhi, Prafulla Kumar. January 1976 (has links)
Originally presented as the author's thesis, (M.S.) in the M.I.T. Dept. of Aeronautics and Astronautics, 1976. / Research sponsored by the Office of Naval Research under Contract N00014-74-C-0163 and N00014-75-C-1065. Bibliography : p. 54.
2

Response of a small spar buoy to ocean waves

Severance, Robert W. January 1972 (has links)
Thesis (Ph. D.)--Florida State University, 1972. / Includes bibliographical references (leaves 87-89).
3

The feasiblity of solar-powered, self-propelled data buoys

Egles, David William January 1987 (has links)
The purpose of this study is to explore the feasibility of a recent development in oceanographic instrumentation known as an active drifter buoy. The active drifter is a self-propelled, solar-powered data buoy which has the capability of influencing its drift rate and direction with the use of a thruster/rudder system. This study examines the active drifters developed thus far, and discusses a series of experiments which provide sufficient information to predict the performance of a buoy offshore. The active drifter was conceived at the Institute of Ocean Sciences at Patricia Bay, B.C. Under the direction of Engineer G.R. Smith, a prototype was built and received limited testing in inshore waters. Seaboy Marine Services Ltd., a manufacturer of data buoys, began its own active drifter program in 1984, and in 1985 made its prototype available to the author for a series of experiments to define its capabilities and provide data for future development. The Seaboy active drifter was named Ranger 1, and had a shallow, spoon-shaped hull with a circular deck to maximize the area available for a photovoltaic array. The buoy was 2m in diameter and had a foil shaped keel 1m deep. A 12 V DC thruster combined with a 36 cm. model airplane propeller propelled the buoy at a speed of 0.50 m/s in calm water. The 210 peak watt solar array charged a bank of six 55 amp hour gelled electrolyte lead acid batteries and provided the power to operate the electronics payload and for propulsion. The Ranger testing program included a measurement of the effective power of the hull at the B.C. Research tow tank facilities. Experiments in the tow tank revealed that a design speed of 0.50 m/s required 4 watts of thrust, and that a static aft trim was required to prevent the buoy from submerging into its own wake. Extensive inshore tests were performed on the Ranger buoy in Elk Lake, near Victoria. These tests showed that the actual power required to propel the buoy at 0.50 m/s was 32 watts. Downwind drift tests showed the buoy travelled at a rate of 5% of the lm wind speed. Upwind, the combined effects of surface drift, waves and wind drag reduced the forward buoy speed by a factor equal to 5.4% of the wind speed, and the maximum speed in which the buoy could make forward headway was 10 m/s. A simulation based on the results of these experiments was performed to predict the performance of an active drifter deployed at Ocean Station Papa (50°N, 145°W). At this site, the average wind speeds are 10.5 m/s, with surface drift currents equal to 3.3% of the wind speed. With an average daily total insolation of 9.6 MJ/m² the buoy would be able to motor 12.7 hours a day. In these conditions, the active drifter could reduce the annual drift rate to 43% of a comparable unpropelled buoy. This is comparable to a deep-drogued spar buoy, indicating no significant improvement inperformance over the less sophisticated buoys commonly in use. The simulation shows that for an active drifter buoy to become a practical alternative to buoys now available, changes must be made in the hull shape to reduce drag and the effects of winds and waves on buoy mobility. / Science, Faculty of / Earth, Ocean and Atmospheric Sciences, Department of / Graduate
4

Interpretation of force vector recorder data describing buoy system dynamics

Padhi, Prafulla Kumar January 1976 (has links)
Thesis. 1976. M.S.--Massachusetts Institute of Technology. Dept. of Aeronautics and Astronautics. / Microfiche copy available in Archives and Aero. / Includes bibliographical references. / by Prafulla K. Padhi. / M.S.
5

System design of a high data rate oceanographic telemetry buoy

Clark, Andrew Malcolm January 1995 (has links)
Thesis (Ph. D.)--University of Hawaii at Manoa, 1995. / Includes bibliographical references (leaves 136-141). / Microfiche. / xi, 141 leaves, bound ill., maps 29 cm
6

Self deployable deep sea moorings /

Berteaux, H. O. Kery, S. M. Walden, R. G. January 1900 (has links)
"January 1992." / "Technical report." "Funding was provided by the Office of Naval Research through Contract no. N00014-90-C-0098." Includes bibliographical references (p. 37-38).
7

On surface circulation of the Eastern North Pacific

Hagan, Denise Ellen. January 1982 (has links)
Thesis (Ph. D.)--Texas A & M University, 1982. / Vita. Includes bibliographical references (leaves 274-278).
8

The velocity field in the northeast Atlantic from satellite- tracked drifting buoys

Giannetti, Paolo. January 1900 (has links)
Thesis (M.S.)--Naval Postgraduate School, 1993. / "September 1993." Includes bibliographical references (p. 70-72).
9

Lagrangian observations of the near-surface circulation in the North Pacific, 1990-1995

Bograd, Steven J. January 1998 (has links)
Thesis (Ph. D.)--University of British Columbia, 1998. / Includes bibliographical references (leaves 186-199).
10

Geoacoustic inversion of subbottom channels using mulitple frequency input parameters

Unknown Date (has links)
This thesis investigates inversion techniques used to determine the geoacoustic properties of a shallow-water waveguide. The data used were obtained in the Shallow Water '06 Modal Mapping Experiment in which four buoys drifted over a system of subbottom channels. The method used was perturbative inversion using modal eigenvalues as input parameters, which were found using an autoregressive spectral estimator. This work investigates the differences between a "channel" region and a "no channel" region based on an inferred stratigraphic model. Inversions were performed on data from a single buoy both at individual frequencies and multiple frequencies simultaneously. Since the use of multiple frequencies and a certain set of constraints proved to be an effective method of inversion, the method was applied to data from the other three buoys as well. It is shown that the "channel" and "no channel" regions have significantly different sound speed profiles. / by Rebecca Weeks. / Thesis (M.S.C.S.)--Florida Atlantic University, 2010. / Includes bibliography. / Electronic reproduction. Boca Raton, Fla., 2010. Mode of access: World Wide Web.

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