Underwater Acoustics
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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. -
Ocean Acoustic Tomography: a Missing Element of the Ocean Observing System
UACE2017 - 4th Underwater Acoustics Conference and Exhibition OCEAN ACOUSTIC TOMOGRAPHY: A MISSING ELEMENT OF THE OCEAN OBSERVING SYSTEM Brian Dushawa, John Colosib, Timothy Dudac, Matthew Dzieciuchd, Bruce Howee, Arata Kanekof, Hanne Sagena, Emmanuel Skarsoulisg, Xiaohua Zhuh aNansen Environmental and Remote Sensing Center, Thormøhlens gate 47, 5006 Bergen, NORWAY bNaval Postgraduate School, 833 Dyer Road, Monterey, CA 93943 USA cApplied Ocean Physics and Engineering, MS 11, Woods Hole Oceanographic Institution, Woods Hole, MA 02543 USA dScripps Institution of Oceanography, University of California, San Diego 92093-0225 USA eOcean and Resources Engineering, University of Hawaii at Manoa, Honolulu HI 96822 USA fInstitute of Engineering, Hiroshima University, 1-3-2 Kagamiyama, Higashi-Hiroshima City, Hiroshima, JAPAN 739-8511 gFoundation for Research and Technology Hellas, Institute of Applied and Computational Mathematics, P.O. Box 1385, GR-71110 Heraklion, GREECE hSecond Institute of Oceanography, State Oceanic Administration, 36 Baochubei Road, Hangzhou, CHINA 310012 Brian Dushaw, Nansen Environmental and Remote Sensing Center, Thormøhlens gate 47, 5006 Bergen, NORWAY fax: (+47) 55 20 58 01, e-mail: [email protected] Abstract: Ocean acoustic tomography now has a long history with many observations and experiments that highlight the unique capabilities of this approach to detecting and understanding ocean variability. Examples include observations of deep mixing in the Greenland Sea, mode-1 internal tides radiating far into the ocean interior (coherent in time and space), relative vorticity on multiple scales, basin-wide and antipodal measures of temperature, barotropic currents, coastal processes in shallow water, and Arctic climate change. Despite the capabilities, tomography, and its simplified form thermometry, are not yet core observations within the Ocean Observing Systems (OOS). -
The 10Th EAA International Symposium on Hydroacoustics Jastrzębia Góra, Poland, May 17 – 20, 2016
ARCHIVES OF ACOUSTICS Copyright c 2016 by PAN – IPPT Vol. 41, No. 2, pp. 355–373 (2016) DOI: 10.1515/aoa-2016-0038 The 10th EAA International Symposium on Hydroacoustics Jastrzębia Góra, Poland, May 17 – 20, 2016 The 10th EAA International Symposium on Hy- Dr. Christopher Jenkins: Backscatter from In- droacoustics, which is also the 33rd Symposium on • tensely Biological Seabeds – Benthos Simulation Hydroacoustics in memory of Prof. Leif Børnø orga- Approaches; nized in Poland, will take place from May 17 to 20, Prof. Eugeniusz Kozaczka: Technical Support for 2016, in Jastrzębia Góra. It will be a forum for re- • National Border Protection on Vistula Lagoon and searchers, who are developing hydroacoustics and re- Vistula Spit; lated issues. The Symposium is organized by the Prof. Andrzej Nowicki et al.: Estimation of Ra- Gdańsk University of Technology and the Polish Naval • dial Artery Reactive Response using 20 MHz Ul- Academy. trasound; The Scientific Committee comprises of the world – Prof. Jerzy Wiciak: Advances in Structural Noise class experts in this field, coming from, among others, • Germany, UK, USA, Taiwan, Norway, Greece, Russia, Reduction in Fluid. Turkey and Poland. The chairman of Scientific Com- All accepted papers will be published in the periodical mittee is Prof. Eugeniusz Kozaczka, who is the Pres- “Hydroacoustics”. ident of Committee on Acoustics Polish Academy of Sciences and Chairman of Technical Committee Hy- droacoustics of European Acoustics Association. Abstracts The Symposium will include invited lectures, struc- -
Acoustic Seabed and Target Classification Using Fractional
University of New Orleans ScholarWorks@UNO University of New Orleans Theses and Dissertations Dissertations and Theses 12-15-2006 Acoustic Seabed and Target Classification using rF actional Fourier Transform and Time-Frequency Transform Techniques Madalina Barbu University of New Orleans Follow this and additional works at: https://scholarworks.uno.edu/td Recommended Citation Barbu, Madalina, "Acoustic Seabed and Target Classification using rF actional Fourier Transform and Time-Frequency Transform Techniques" (2006). University of New Orleans Theses and Dissertations. 480. https://scholarworks.uno.edu/td/480 This Dissertation is protected by copyright and/or related rights. It has been brought to you by ScholarWorks@UNO with permission from the rights-holder(s). You are free to use this Dissertation in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Dissertation has been accepted for inclusion in University of New Orleans Theses and Dissertations by an authorized administrator of ScholarWorks@UNO. For more information, please contact [email protected]. Acoustic Seabed and Target Classication using Fractional Fourier Transform and Time-Frequency Transform Techniques A Dissertation Submitted to the Graduate Faculty of the University of New Orleans in partial fulllment of the requirements for the degree of Doctor of Philosophy in Engineering and Applied Sciences by Madalina Barbu B.S./MS, Physics, University of Bucharest, Romania, 1993 MS, Electrical Engineering, University of New Orleans, 2001 December, 2006 c 2006, Madalina Barbu ii To my family iii Acknowledgments I would like to express my appreciation to Dr. -
OCEANS ´09 IEEE Bremen
11-14 May Bremen Germany Final Program OCEANS ´09 IEEE Bremen Balancing technology with future needs May 11th – 14th 2009 in Bremen, Germany Contents Welcome from the General Chair 2 Welcome 3 Useful Adresses & Phone Numbers 4 Conference Information 6 Social Events 9 Tourism Information 10 Plenary Session 12 Tutorials 15 Technical Program 24 Student Poster Program 54 Exhibitor Booth List 57 Exhibitor Profiles 63 Exhibit Floor Plan 94 Congress Center Bremen 96 OCEANS ´09 IEEE Bremen 1 Welcome from the General Chair WELCOME FROM THE GENERAL CHAIR In the Earth system the ocean plays an important role through its intensive interactions with the atmosphere, cryo- sphere, lithosphere, and biosphere. Energy and material are continually exchanged at the interfaces between water and air, ice, rocks, and sediments. In addition to the physical and chemical processes, biological processes play a significant role. Vast areas of the ocean remain unexplored. Investigation of the surface ocean is carried out by satellites. All other observations and measurements have to be carried out in-situ using research vessels and spe- cial instruments. Ocean observation requires the use of special technologies such as remotely operated vehicles (ROVs), autonomous underwater vehicles (AUVs), towed camera systems etc. Seismic methods provide the foundation for mapping the bottom topography and sedimentary structures. We cordially welcome you to the international OCEANS ’09 conference and exhibition, to the world’s leading conference and exhibition in ocean science, engineering, technology and management. OCEANS conferences have become one of the largest professional meetings and expositions devoted to ocean sciences, technology, policy, engineering and education. -
On Ocean Waveguide Acoustics
BOOKREVIEW ___________________________________________________ GEORGE V. FRISK ON OCEAN WAVEGUIDE ACOUSTICS acoustic waves with multilayered media is also an ac ACOUSTIC WAVEGUIDES: APPLICATIONS TO OCEANIC SCIENCE tive area of research in underwater acoustics. By C. Allen Boyles, Principal Professional Staff, In recent years, the inverse problem of determining The Johns Hopkins University Applied Physics Laboratory oceanographic properties from acoustic measurements Published by John Wiley & Son, New York, 1984. 321 pp. $46.95 has become increasingly important and has given rise to the term "acoustical oceanography," a variant of "ocean acoustics" that emphasizes the oceanograph ic implications of acoustic experiments. A major de The field of ocean acoustics is an active area of the velopment in this area is time-of-flight acoustic oretical and experimental research, with a continual tomography in which front and eddy intensity and ly expanding body of literature in research journals variability over hundreds of kilometers are measured and textbooks. Boyles' book is a welcome addition to acoustically. In ocean-bottom acoustics, direct inverse the literature and provides a useful text for both stu methods are being developed that utilize some mea dents and practitioners in the field. surement of the acoustic field, such as the plane wave Although electromagnetic waves are strongly ab reflection coefficient of the bottom, as direct input to sorbed by water, acoustic waves can, under the prop algorithms for determining the acoustic properties of er conditions, propagate over hundreds, even thou the bottom. This approach is to be contrasted with sands, of miles through the ocean. As a result, sound conventional techniques in which forward models for waves and sonar assume the major role in the ocean computing the acoustic field are run for different bot that electromagnetic waves and radar play in the at tom properties until best fits to the data are obtained. -
Christopher Bassett Dept
Christopher Bassett Dept. of Applied Ocean Physics and Engineering Phone: (508) 289-3891 Woods Hole Oceanographic Institution Email: [email protected] Woods Hole, Massachusetts Education 2013 Ph.D. Mechanical Engineering, University of Washington 2010 M.S. Mechanical Engineering, University of Washington 2007 B.S. Mechanical Engineering, University of Minnesota Professional Experience 2013-pres. Postdoctoral Scholar, Department of Applied Ocean Physics & Engineering, Woods Hole Oceanographic Institution 2009-2013 Graduate Research Assistant, Mechanical Engineering/Applied Physics Laboratory, University of Washington 2008-2009 Teaching Assistant, Department of Physics, University of Minnesota Research Interests Passive acoustics - Measurements and modeling of vessel noise - Mapping and modeling course-grained sediment transport Broadband acoustic scattering - Scattering from rough surfaces - Discrimination and quantification of targets near interfaces - Acoustic remote sensing of sea ice and oil spills in/under sea ice - Scattering from marine organisms - Broadband scattering from suspended sediment Marine hydrokinetic energy (MHK) - Radiated noise measurements and acoustic impacts modeling of MHK devices - Instrumentation for environmental impacts monitoring around MHK devices Peer-Reviewed Publications J.1 Polayge, B., C. Bassett, M. Holt, J. Wood, and S. Barr (under revision). Estimated detection of tidal turbine operating noise in Admiralty Inlet, Puget Sound, Washington, Journal of Oceanic Engineering. J.2 Bassett, C., A.C. Lavery, T. Maksym, and J. Wilkinson (2015). Laboratory measurements of high-frequency, acoustic broadband backscattering from sea ice and crude oil, Journal of the Acoustical Society of America, 137(1), EL32-EL38. J.3 Bassett, C., J. Thomson, P. Dahl and B. Polagye (2014). Flow-noise and turbulence in two tidal channels, Journal of the Acoustical Society of America, 135(4), 1764-1774. -
THE OCEANOGRAPHY SOCIETY BIENNIAL SCIENTIFIC MEETING 2-5 April 2001 Miami Beach, Florida USA
THE OCEANOGRAPHY SOCIETY BIENNIAL SCIENTIFIC MEETING 2-5 April 2001 Miami Beach, Florida USA Listed alphabetically by first author. Asterisk(*) indicates invited speaker. ALLARD, Richard ~, John Christiansen 2, Steve *APEL, John R.' Williams ~ and Larry Jendro ~ From Pictures to Measurements: Four Decades of The Distributed Integrated Ocean Prediction System Ocean Remote Sensing (DIOPS) With the arrival of more-or-less continuous satellite The Distributed Integrated Ocean Prediction System data streams and fully vetted measurement capabilities, (DIOPS) is a wave, tide and surf prediction system ocean remote measurement has gone from being con- designed to provide U.S. Navy and U.S. Joint Forces a fined to the province of specialists to finding its way capability to predict wave and surf conditions at any into the toolkit of working oceanographers. While it has given location, worldwide. DIOPS contains a suite of taken well over three decades to come about, data from wave, tide and surf models (WAM, REFDIE STWAVE, a variety of sensors can currently give information of PCTIDES and SURF3.0) which can be run in a nested much interest across the spectrum of disciplines in our fashion. DIOPS is designed to operate under an object- science, even to those concerned with the sea floor if oriented framework and provides access to environ- acoustics is included as a remote sensing method. A mental inputs via the Tactical Environmental Data review is given of some sensor outputs, both historic Server (TEDS). DIOPS will be installed at the Naval and current, and examples are presented of remote Pacific Meteorology and Oceanography Center in San sensing contributions to the understanding of various Diego in Spring 2001, where a Beta-test site with an processes and phenomena taking place in the sea. -
Assessment of the Effects of Noise and Vibration from Offshore Wind Farms on Marine Wildlife
ASSESSMENT OF THE EFFECTS OF NOISE AND VIBRATION FROM OFFSHORE WIND FARMS ON MARINE WILDLIFE ETSU W/13/00566/REP DTI/Pub URN 01/1341 Contractor University of Liverpool, Centre for Marine and Coastal Studies Environmental Research and Consultancy Prepared by G Vella, I Rushforth, E Mason, A Hough, R England, P Styles, T Holt, P Thorne The work described in this report was carried out under contract as part of the DTI Sustainable Energy Programmes. The views and judgements expressed in this report are those of the contractor and do not necessarily reflect those of the DTI. First published 2001 i © Crown copyright 2001 EXECUTIVE SUMMARY Main objectives of the report Energy Technology Support Unit (ETSU), on behalf of the Department of Trade and Industry (DTI) commissioned the Centre for Marine and Coastal Studies (CMACS) in October 2000, to assess the effect of noise and vibration from offshore wind farms on marine wildlife. The key aims being to review relevant studies, reports and other available information, identify any gaps and uncertainties in the current data and make recommendations, with outline methodologies, to address these gaps. Introduction The UK has 40% of Europe ’s total potential wind resource, with mean annual offshore wind speeds, at a reference of 50m above sea level, of between 7m/s and 9m/s. Research undertaken by the British Wind Energy Association suggests that a ‘very good ’ site for development would have a mean annual wind speed of 8.5m/s. The total practicable long-term energy yield for the UK, taking limiting factors into account, would be approximately 100 TWh/year (DTI, 1999). -
Underwater Acoustics - Gee-Pinn James Too
OCEANOGRAPHY – Vol.III - Underwater Acoustics - Gee-Pinn James Too UNDERWATER ACOUSTICS Gee-Pinn James Too National Cheng Kung University, Taiwan Keywords: Underwater Acoustics, Underwater Communication, Underwater Detection, Sound Velocity Profiles, Surface Duct, Shadow Zone, SOFAR (Deep Sea) Channel, Acoustic Ray Model, Normal Mode Model, PE (Parabolic Wave Equation) Models, Temperature, Pressure, and Salinity. Contents 1. An Acoustical View of Oceanography 2. The History of Research on Ocean Acoustics 3. Measurement of Speed of Sound 3.1. The Sound Speed Profile 3.2. Propagation Theory 3.3. Applications of Underwater Acoustics 4. Other Applications Bibliography Biographical Sketch Summary Underwater acoustics is an important science with significant practical application, especially for the application in ocean. Electro-magnetic waves, which are strongly absorbed by water, have their limits in propagation range in water. Therefore, acoustic waves play an important role on the navigation, underwater communication, underwater detection, and investigation in ocean research. The ocean is an inhomogeneous medium with various sound velocity profiles that vary with depth because of changes in temperature, hydrostatic pressure and salinity. Due to these sound velocity profiles, acoustic wave propagation in ocean results in several interesting phenomena such as surface duct, shadow zone, SOFAR (deep sea) channel, etc. These phenomena all have practical application in underwater communication and detection. Theoretical models and their numerical algorithms for wave propagation are developedUNESCO to describe the complicated ocean– phenomenaEOLSS of wave propagation. Some of these models, such as: acoustic ray model, normal mode model, PE (parabolic wave equation) models are described in this section. SAMPLE CHAPTERS Sonar equations comprise a group of parameters, which considers the phenomena and effects of the underwater sound. -
Matteo Bernasconi Phd Thesis
THE USE OF ACTIVE SONAR TO STUDY CETACEANS Matteo Bernasconi A Thesis Submitted for the Degree of PhD at the University of St Andrews 2012 Full metadata for this item is available in Research@StAndrews:FullText at: http://research-repository.st-andrews.ac.uk/ Please use this identifier to cite or link to this item: http://hdl.handle.net/10023/2580 This item is protected by original copyright This item is licensed under a Creative Commons Licence The use of active sonar to study cetaceans Matteo Bernasconi Submitted in partial fulfilment of the requirements for the degree of Doctor of Philosophy University of St Andrews July 2011 The use of active sonar to study cetaceans Matteo Bernasconi TABLE OF CONTENTS DECLARATIONS V ACKNOWLEDGMENTS VII ABSTRACT IX 1. INTRODUCTION 1 2. UNDERWATER ACTIVE ACOUSTIC 13 2.1 Historical notes 15 2.2 Sound: basic concepts 17 2.2.1 Sound propagation 18 2.2.2 Sound pressure and intensity 20 2.2.3 The decibel 21 2.2.4 Transmission Loss 22 2.2.5 Sound Speed 25 2.3 Transducers and beams 26 2.3.1 The beam pattern 28 2.3.2 The equivalent beam angle 29 2.3.3 Pulse and Ranging 30 2.4 Acoustic scattering 31 2.4.1 Target Strength 32 2.4.2 Target shape and orientation 33 2.4.3 Volume/area scattering coefficient 34 2.5 The sonar equation 35 3. CALIBRATION 39 3.1 The on‐axis sensitivity 41 3.2 Nearfield and Farfield 42 3.3 The TVG function 43 3.4 Standard experimental procedure 44 3.5 Calibration spheres 46 3.6 Calibration test of omnidirectional Sonar 47 3.6.1 Introduction 48 3.6.2 Method 49 3.6.3 Results & Discussion 51 3.6.4 Conclusion 57 4. -
Improved Sound Speed Control Through Remotely Detecting Strong Changes in the Thermocline
IMPROVED SOUND SPEED CONTROL THROUGH REMOTELY DETECTING STRONG CHANGES IN THE THERMOCLINE by Jose M. Cordero Ros B.S. and M.S. in Naval Sciences, Spanish Naval College, 2001 Extension Course in Hydrography (IHO Category “A”), Hydrographic Institute of the Spanish Navy, 2006 THESIS Submitted to the University of New Hampshire in partial fulfillment of the requirements for the degree of Master of Science in Ocean Engineering. Ocean Mapping September 2018 i ProQuest Number:10934448 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. ProQuest 10934448 Published by ProQuest LLC ( 2018). Copyright of the Dissertation is held by the Author. All rights reserved. This work is protected against unauthorized copying under Title 17, United States Code Microform Edition © ProQuest LLC. ProQuest LLC. 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, MI 48106 - 1346 This thesis has been examined and approved. Thesis Director, John. E. Hughes Clarke, Professor of Ocean Engineering and Earth Science Andrew Armstrong, Co-Director, Joint Hydrographic Center Affiliate Professor of Ocean Engineering and Marine Sciences and Earth Sciences Giuseppe Masetti, Research Assistant Professor of Ocean Engineering On 20th July, 2018 ii ACKNOWLEDGEMENTS I would like to thank the Hydrographic Institute of the Spanish Navy for the financial support of my studies at the Center of Coastal and Ocean Mapping (University of New Hampshire).