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Evidence of gulf stream bimodality on a several month timescaleLee, Dana K. 05 1900 (has links)
No description available.
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A comparison of cross-stream velocities and Gulf Stream translations utilizing in-situ and remotely-sense dataFreise, Carl Bruce. January 1988 (has links)
Thesis (M.S.)--Massachusetts Institute of Technology, 1988. / "October 1988." "Funding was provided by the Office of Naval Research through contract Numbers N00014-86-K-0751 and N00014-87-K-0007, and by the United States Navy." Includes bibliographical references (leaves 46-48).
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Responses of benthic macrofauna to the dynamics of a Gulf Stream front on the continental shelf near Cape Hatteras, North CarolinaHarrington, Cynthia Lucile, January 1981 (has links)
Thesis (Ph. D.)--University of Wisconsin--Madison, 1981. / Typescript. Vita. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references.
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Analysis of the Gulf Stream path and Rossby waves in the North Atlantic based on satellite data /Osychny, Vladimir. January 2006 (has links)
Thesis (Ph. D.)--University of Rhode Island, 2006. / Typescript. Includes bibliographical references (leaves 246-250).
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Acoustical identification of the characteristics of ocean frontsRadcliffe, Stewart Alexander January 1997 (has links)
No description available.
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Topographic influences on the path of the Gulf StreamWarren, Bruce A. January 1962 (has links)
Thesis--Massachusetts Institute of Technology (Ph. D. Geology). / Photocopy of typescript, Microfilm -- 1 reel ; 35 mm.
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Mesoscale forcing on ocean waves during Gulf Stream North Wall eventsOkon, John A. 03 1900 (has links)
Approved for public release; distribution is unlimited / Under meteorological conditions associated with extreme cold air outbreaks (CAO) off the U.S. East Coast, large ocean waves sometimes develop along the North Wall of the Gulf Stream. These wave events produce wave heights above those expected given the short fetch and moderate winds. The highest waves are often very localized, which suggests localized forcing by the atmosphere. In this study, results from four cases are examined to characterize the role of high resolution, mesoscale wind forcing in generating localized regions of large ocean waves during events with large air-sea temperature differences. A known "true" atmosphere is simulated through the use of the Navy's Coupled Oceanographic and Atmospheric Mesoscale Prediction System (COAMPS). Model surface wind output from COAMPS is used to generate a wave field using Wavewatch Three (WW3), which is then compared to buoy observations and ship reports. Results of these cases show the mesoscale wind forcing of ocean waves during CAO and the importance of mesoscale atmospheric modeling in localized generation of ocean wind waves. Additionally, empirical wave forecast techniques are compared to WW3 model output for these cases to further reinforce the mesoscale atmospheric forcing during rapid growth of wind wave events in fetch limited environments. / Lieutenant Commander, United States Navy
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Atmospheric interactions with Gulf Stream rings /Dewar, William K. January 1983 (has links)
Thesis (Ph. D.)--Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1983. / Includes bibliographical references (p. 226-229).
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On the midwater fish faunas of Gulf Stream rings with respect to habitat differences between slope water and northern Sargasso Sea.Jahn, Andrew E. January 1900 (has links)
Thesis (Ph. D.)--Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1976.
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Equipping a selected group of pastors in the Gulf Stream Baptist Association, Fort Lauderdale, Florida, in strategic planning skillsBoone, John C., January 1900 (has links)
Thesis (D. Min.)--New Orleans Baptist Theological Seminary, 2007. / Abstract and vita. Includes final project proposal. Includes bibliographical references (leaves 190-196, 74-78).
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