OCEA 5250 – Acoustical Oceanography David R. Barclay

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OCEA 5250 – Acoustical Oceanography David R. Barclay

OCEA 5250 – Acoustical Oceanography Term Assignment Selection of five key publications: October 4th Presentation due date: November 22nd Description: The objective of this project is to write a review and explanation of a method or application of in acoustical oceanographic. The presentation should aim to be clear and informative, suitable for the class audience or a conference of experts. The presentation must cite at least five key publications on the topic, although the widest read possible is encouraged. The current state-of-the-art of the research topic should be presented. Presentations will be 15 minutes, ~12 minutes of discussion, with ~3 minutes for questions at the end. Resources: Journal subscriptions are available when connected to the Dalhousie Network. VPN access is available through the library website. Topics: The following topics are suggested, although you may choose an unlisted topic with approval of Dr. Barclay or Dr. Hay. Noise tomography in the deep ocean Acoustical tomography in deep and shallow water Broadband scattering: acoustic colour Time reversal ocean acoustics Underwater acoustic communications The effect of internal waves on propagation Passive geoacoustic inversion Surface processes using active sonar Seabed processes using active sonar Sediment generated noise Acoustic identification of fish species Non-linear methods for geoacoustic inversion and acoustic localization Range estimation and tracking of marine mammals with a single hydrophone Quantifying rainfall at sea with passive acoustics Acoustic signature of snowfall in open and ice covered seas Effect of ice cover on propagation Surface wave effects on propagation Acoustic vector sensor performance Passive estimates of air-sea gas exchange Acoustic gravity waves Seismic oceanography Grading: A grade out of 30 will be awarded. Equal weight will be given in the categories of 1) Scientific accuracy – Demonstrate a complete physical and mathematical grasp of the topic. 2) Instructional clarity – How clearly does the presentation explain the questions that arise from the topic? Are the explanations at the appropriate level? David R. Barclay Fall 2016 .

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Barotropic Tide in the Northeast South China Sea
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Calhoun, Institutional Archive of the Naval Postgraduate School Calhoun: The NPS Institutional Archive Faculty and Researcher Publications Faculty and Researcher Publications 2004-10 Barotropic Tide in the Northeast South China Sea Beardsley, Robert C. Monterey, California. Naval Postgraduate School Vol.29, no.4, October 2004 http://hdl.handle.net/10945/35040 IEEE JOURNAL OF OCEANIC ENGINEERING, VOL. 29, NO. 4, OCTOBER 2004 1075 Barotropic Tide in the Northeast South China Sea Robert C. Beardsley, Timothy F. Duda, James F. Lynch, Senior Member, IEEE, James D. Irish, Steven R. Ramp, Ching-Sang Chiu, Tswen Yung Tang, Ying-Jang Yang, and Guohong Fang Abstract—A moored array deployed across the shelf break in data using satellite advanced very high-resolution radiometer, the northeast South China Sea during April–May 2001 collected altimeter, and other microwave sensors [8]. sufficient current and pressure data to allow estimation of the The SCS study area was centered over the shelf break near barotropic tidal currents and energy fluxes at five sites ranging in depth from 350 to 71 m. The tidal currents in this area were 21 55 N, 117 20 E, approximately 370 km west of the mixed, with the diurnal O1 and K1 currents dominant over the southern tip of Taiwan (Fig. 1). This area was chosen in part upper slope and the semidiurnal M2 current dominant over the for three reasons: 1) large-amplitude high-frequency internal shelf. The semidiurnal S2 current also increased onshelf (north- waves generated near the Luzon Strait propagate through the ward), but was always weaker than O1 and K1.
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