Acoustic Data from Vessels of Opportunity

Total Page:16

File Type:pdf, Size:1020Kb

Acoustic Data from Vessels of Opportunity MESOPP Acoustic data from vessels of opportunity Deliverable Lead: CSIRO Reference: MESOPP-18-0009 Dissemination Level: Public Issue: 1. 0 Date: 2018, Dec. 03 Horizon 2020. Grant agreement No 692173 Public Acoustic data from vessels of opportunity MESOPP-18-0009 Public V1.0 2018,Dec.03 Chronology Issues Issue Date Reason for change Author 1.0 21/11/2018 First version of the document K. Haris R. Kloser 23/11/2018 Second version of the document P. Lehodey (comments on first version) 27/11/2018 Third version of the document S. Fielding (comments on first version) 30/11/2018 Fourth version of the document P. Lehodey (comments on second version) 30/11/2018 Finalized issue 1.0 K. Haris R. Kloser Distribution Company Means of distribution Names CLS Notification Citation This report can be cited as follow: Haris K., Kloser R. (2018). Acoustic data from vessels of opportunity. Report from the EU-H2020 MESOPP project, MESOPP-18-0009: 39 pp. www.mesopp.eu/documents/ 1 - 10 - GB - NT - www.mesopp.eu Copyright © MESOPP Project Consortium i.1 FORM Acoustic data from vessels of opportunity MESOPP-18-0009 Public V1.0 2018,Dec.03 List of Contents 1. Introduction ........................................................................................................................... 1 1.1. Acoustic data to biomass .......................................................................................................... 2 1.2. Ecosystem models .................................................................................................................... 3 1.3. This report................................................................................................................................. 4 2. Processed acoustic data portals .............................................................................................. 4 3. Processed acoustic data description and quality flags .............................................................. 5 4. Overview of bioacoustic metrics ............................................................................................. 9 5. Effects of data processing routines and quality checking methods ......................................... 12 5.1. Calibration............................................................................................................................... 12 5.2. Effect of motion correction .................................................................................................... 13 5.3. Data quality and effect of filters ............................................................................................. 14 5.4. Effect of secondary corrections .............................................................................................. 17 6. Limitation of single frequency data ....................................................................................... 21 7. Existing resolution of the NetCDF and limitations .................................................................. 24 8. Conclusions .......................................................................................................................... 25 9. References ........................................................................................................................... 26 Appendix A - Importance of calibration parameters .................................................................. 29 Appendix B - Secondary corrections for sound speed and absorption ........................................ 30 Appendix C - Matlab function for visualisation .......................................................................... 32 1 - 10 - GB - NT - www.mesopp.eu Copyright © MESOPP Project Consortium i.2 FORM Acoustic data from vessels of opportunity MESOPP-18-0009 Public V1.0 2018,Dec.03 List of tables and figures List of tables: Table 1. Description of variables present in a NetCDF file. ..................................................................... 8 Table 2. A brief overview of bioacoustic metrics used in the literature. .............................................. 11 List of figures: Figure 1. Example of how bioacoustics data is collected by transmitting a pulse of sound in the water that reflects off the species to produce an echogram, www.imos.org.au. .................................... 1 Figure 2. Visualisation of 38 kHz acoustic data (푆푣) collected by FV Rehua during a 4 day transit from New Zealand to Australia in August 2010. Image courtesy: Tim Ryan, CSIRO. ............................... 2 Figure 3. Flowchart showing how acoustic data is normally converted to fish biomass. ....................... 3 Figure 4. Map showing spatial coverage of processed bioacoustic transects as of 13 November 2018. (a) MESOPP project. (b) IMOS. ....................................................................................................... 5 Figure 5. Generic overview of the data processing sequence in the context of data variables present in a NetCDF file. Reproduced from Ryan et al. (2015). ................................................................... 6 Figure 6. Resolution of a NetCDF file containing processed acoustic data. ............................................. 6 Figure 7. Organization of variables present in a NetCDF file. .................................................................. 7 Figure 8. A broad classification of DSL studies. ....................................................................................... 9 Figure 9. Example of the fishing vessel (Antarctic Discovery) 38 kHz acoustic data covering the Pacific Ocean. The Longhurst oceanic biogeographical provinces are superimposed as white lines. The center part of the south Pacific highlight oligotrophic regions with low predicted productivity (blue), which is observed in general by the low mesopelagic (400–800 m depth) backscatter strength (small magenta circles) (Haris and Kloser, 2017). .......................................................... 10 Figure 10. Calibrated 퐺0 (blue) and 푆푎 corr (red) values for (a) FV Rehua and (b) Austral Leader between 2005–2015. Reproduced from Downie et al. (2018). .................................................... 12 Figure 11. Effect of motion correction on raw 38 kHz 푆푣 data collected by RV Southern Surveyor on 15 October 2013. Note the strong non-linear range dependent effect. ...................................... 13 Figure 12. Voyage track of the data presented in Figure 13. Map generated using Ocean Data View (Schlitzer, 2018). ........................................................................................................................... 14 Figure 13. Combined effects of data processing filters on raw 38 kHz 푆푣 data collected by FV San Tongariro. (a) Calibrated raw data. (b) Final processed data including secondary corrections described in the following section. ............................................................................................... 15 Figure 14. Data quality flags associated with the data presented in Figure 13. ................................... 16 Figure 15. Voyage track of the data presented in Figure 16. ................................................................ 17 Figure 16. Examples of calculated sound speed and absorption coefficient values along the 38 kHz transect from SW Indian Ocean to Mauritius. The absorption coefficients were calculated using two equations as shown in the figure. .......................................................................................... 18 1 - 7 - GB - NT - www.mesopp.eu Copyright © MESOPP Project Consortium i.3 FORM Acoustic data from vessels of opportunity MESOPP-18-0009 Public V1.0 2018,Dec.03 Figure 17. Boxplots of calculated sound speed and absorption coefficient values presented in Figure 16. .................................................................................................................................................. 19 Figure 18. The difference in 38 kHz 푆푣 before and after secondary corrections. Related percentage corrections are shown in the boxplots. Note the increasing correction with range. ................... 20 Figure 19. Voyage track of the data presented in Figure 20. Map generated using Ocean Data View (Schlitzer, 2018). ........................................................................................................................... 21 Figure 20. Multi-frequency echograms highlighting different scattering layers and functional groups. .......................................................................................................................................... 22 Figure 21. Example of multi-frequency metrics (green = 120 kHz; black = 70 kHz; red = 38 kHz; blue = 18 kHz). Average backscatter data in epipelagic (20–200 m), upper mesopelagic (200–400 m), and lower mesopelagic (400–800 m) zone. .................................................................................. 23 Figure 22. Sampling range limitation of high-frequency (120 kHz) data. .............................................. 23 Figure 23. Example echogram showing fish schools at a fine resolution. The grid lines represent existing resolution of the NetCDF file. .......................................................................................... 24 1 - 7 - GB - NT - www.mesopp.eu Copyright © MESOPP Project Consortium i.4 FORM Acoustic data from vessels of opportunity MESOPP-18-0009 Public V1.0 2018,Dec.03 Overview The underlying concept of MESOPP is the creation of a collaborative network and associated
Recommended publications
  • Single Particle Analysis of Particulate Pollutants in Yellowstone National Park During the Winter Snowmobile Season
    SINGLE PARTICLE ANALYSIS OF PARTICULATE POLLUTANTS IN YELLOWSTONE NATIONAL PARK DURING THE WINTER SNOWMOBILE SEASON. Richard E. Peterson* and Bonnie J. Tyler** * Dept. of Chemistry and Biochemistry **Dept. of Chemical Engineering Montana State University, Bozeman, MT 59717, USA [email protected] Introduction: Particulate, or aerosol, pollution is a complex mixture of organic and inorganic compounds which includes a wide range of sizes and whose composition can vary widely depending on the time of year, geographical location, and both local and long range sources. Aerosol are important because of participation in atmospheric electricity, absorption and scattering of radiation (i.e. sunlight and thus affecting climate and visibility), their role as condensation nuclei for water vapor (and thus affecting precipitation chemistry and pH), and health effects. Particles greater than 2 micrometers in diameter (coarse) are generally formed by mechanical processes while smaller particles (fine) are formed by gas to particle conversion and accumulation/coagulation of these smallest aerosol. Because particles smaller than 2.5 micrometers (USEPA PM2.5) can become trapped deep in the lungs, it is of particular interest to identify toxic substances, such as heavy metals and polyaromatic hydrocarbons, that may be present in particles of this size range. Epidemiological studies have typically used particle size as the metric for identifying adverse health effects of particulate matter (PM), largely because data on PM size is available. Data on particle composition or other characteristics are less well known, if known at all in many cases. We are evaluating the potential for using Time of Flight Secondary Ion Mass Spectroscopy (TOF-SIMS) to study the composition of single particles from atmospheric aerosol.
    [Show full text]
  • Linking Mesopelagic Prey Abundance and Distribution to the Foraging
    Deep–Sea Research Part II 140 (2017) 163–170 Contents lists available at ScienceDirect Deep–Sea Research II journal homepage: www.elsevier.com/locate/dsr2 Linking mesopelagic prey abundance and distribution to the foraging MARK behavior of a deep-diving predator, the northern elephant seal ⁎ Daisuke Saijoa,1, Yoko Mitanib,1, , Takuzo Abec,2, Hiroko Sasakid, Chandra Goetsche, Daniel P. Costae, Kazushi Miyashitab a Graduate School of Environmental Science, Hokkaido University, 20-5 Bentencho, Hakodate, Hokkaido 040-0051, Japan b Field Science Center for Northern Biosphere, Hokkaido University, 20-5 Bentencho, Hakodate, Hokkaido 040-0051, Japan c School of Fisheries Science, Hokkaido University, 3-1-1 Minato cho, Hakodate, Hokkaido 041-8611, Japan d Arctic Environment Research Center, National Institute of Polar Research, 10-3, Midori-cho, Tachikawa, Tokyo 190-8518, Japan e Department of Ecology & Evolutionary Biology, University of California, Santa Cruz, CA 95060, United States ARTICLE INFO ABSTRACT Keywords: The Transition Zone in the eastern North Pacific is important foraging habitat for many marine predators. Deep-scattering layer Further, the mesopelagic depths (200–1000 m) host an abundant prey resource known as the deep scattering Transition Zone layer that supports deep diving predators, such as northern elephant seals, beaked whales, and sperm whales. fi mesopelagic sh Female northern elephant seals (Mirounga angustirostris) undertake biannual foraging migrations to this myctophid region where they feed on mesopelagic fish and squid; however, in situ measurements of prey distribution and subsurface chlorophyll abundance, as well as the subsurface oceanographic features in the mesopelagic Transition Zone are limited. While concurrently tracking female elephant seals during their post-molt migration, we conducted a ship-based oceanographic and hydroacoustic survey and used mesopelagic mid-water trawls to sample the deep scattering layer.
    [Show full text]
  • Censusing Non-Fish Nekton
    WORKSHOP SYNOPSIS Censusing Non-Fish Nekton Carohln Levi, Gregory Stone and Jerry R. Schubel New England Aquarium ° Boston, Massachusetts USA his is a brief summary of a "Non-Fish SUMMARIES OF WORKING GROUPS Nekton" workshop held on 10-11 December 1997 at the New England Aquarium. The overall goals Cephalopods were: (1) to assess the feasibility of conducting a census New higher-level taxa are yet to be discovered, of life in the sea, (2) to identify the strategies and especially among coleoid cephalopods, which are components of such a census, (3) to assess whether a undergoing rapid evolutionary radiation. There are periodic census would generate scientifically worth- great gaps in natural history and ecosystem function- while results, and (4) to determine the level of interest ing, with even major commercial species largely of the scientific community in participating in the unknown. This is particularly, complex, since these design and conduct of a census of life in the sea. short-lived, rapidly growing animals move up through This workshop focused on "non-fish nekton," which trophic levels in a single season. were defined to include: marine mammals, marine reptiles, cephalopods and "other invertebrates." During . Early consolidation of existing cephalopod data is the course of the workshop, it was suggested that a needed, including the vast literatures in Japanese more appropriate phase for "other invertebrates" is and Russian. Access to and evaluation of historical invertebrate micronekton. Throughout the report we survey, catch, biological and video image data sets have used the latter terminology. and collections is needed. An Internet-based reposi- Birds were omitted only because of lack of time.
    [Show full text]
  • Guidance for Using Continuous Monitors in Pm Monitoring
    United States Office of Air Quality EPA-454/R-98-012 Environmental Protection Planning and Standards May 1998 Agency Research Triangle Park, NC 27711 Air GUIDANCE FOR USING CONTINUOUS MONITORS IN PM2.5 MONITORING NETWORKS GUIDANCE FOR USING CONTINUOUS MONITORS IN PM2.5 MONITORING NETWORKS May 29, 1998 PREPARED BY John G. Watson1 Judith C. Chow1 Hans Moosmüller1 Mark Green1 Neil Frank2 Marc Pitchford3 PREPARED FOR Office of Air Quality Planning and Standards U.S. Environmental Protection Agency Research Triangle Park, NC 27711 1Desert Research Institute, University and Community College System of Nevada, PO Box 60220, Reno, NV 89506 2U.S. EPA/OAQPS, Research Triangle Park, NC, 27711 3National Oceanic and Atmospheric Administration, 755 E. Flamingo, Las Vegas, NV 89119 DISCLAIMER The development of this document has been funded by the U.S. Environmental Protection Agency, under cooperative agreement CX824291-01-1, and by the Desert Research Institute of the University and Community College System of Nevada. Mention of trade names or commercial products does not constitute endorsement or recommendation for use. This draft has not been subject to the Agency’s peer and administrative review, and does not necessarily represent Agency policy or guidance. ii ABSTRACT This guidance provides a survey of alternatives for continuous in-situ measurements of suspended particles, their chemical components, and their gaseous precursors. Recent and anticipated advances in measurement technology provide reliable and practical instruments for particle quantification over averaging times ranging from minutes to hours. These devices provide instantaneous, telemetered results and can use limited manpower more efficiently than manual, filter-based methods.
    [Show full text]
  • Meridional Patterns in the Deep Scattering Layers and Top Predator Distribution in the Central Equatorial Pacific
    University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Publications, Agencies and Staff of the U.S. Department of Commerce U.S. Department of Commerce 2010 Meridional patterns in the deep scattering layers and top predator distribution in the central equatorial Pacific Elliott L. Hazen NOAA SWFSC Pacific Fisheries Environmental Lab, [email protected] David W. Johnston Duke University Marine Lab, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/usdeptcommercepub Part of the Environmental Sciences Commons Hazen, Elliott L. and Johnston, David W., "Meridional patterns in the deep scattering layers and top predator distribution in the central equatorial Pacific" (2010). Publications, Agencies and Staff of the U.S. Department of Commerce. 275. https://digitalcommons.unl.edu/usdeptcommercepub/275 This Article is brought to you for free and open access by the U.S. Department of Commerce at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Publications, Agencies and Staff of the U.S. Department of Commerce by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. FISHERIES OCEANOGRAPHY Fish. Oceanogr. 19:6, 427–433, 2010 SHORT COMMUNICATION Meridional patterns in the deep scattering layers and top predator distribution in the central equatorial Pacific ELLIOTT L. HAZEN1,2,* AND DAVID W. component towards understanding the behavior and JOHNSTON1 distribution of highly migratory predator species. 1 Division of Marine
    [Show full text]
  • Blue-Sea Thinking
    TECHNOLOGY QUARTERLY March 10th 2018 OCEAN TECHNOLOGY Blue-sea thinking 20180310_TQOceanTechnology.indd 1 28/02/2018 14:26 TECHNOLOGY QUARTERLY Ocean technology Listening underwater Sing a song of sonar Technology is transforming the relationship between people and the oceans, says Hal Hodson N THE summer of 1942, as America’s Pacific has always been. The subsurface ocean is inhospitable fleet was sluggingit out at the battle ofMidway, to humans and their machines. Salt water corrodes ex- the USS Jasper, a coastal patrol boat, was float- posed mechanisms and absorbs both visible light and ALSO IN THIS TQ ing 130 nautical miles (240km) off the west radio waves—thus ruling out radar and long-distance UNDERSEA MINING coast of Mexico, listening to the sea below. It communication. The lack of breathable oxygen se- Race to the bottom was alive with sound: “Some fish grunt, others verely curtails human visits. The brutal pressure Iwhistle or sing, and some just grind their teeth,” reads makes its depths hard to access at all. FISH FARMING the ship’s log. The discovery of the deep scattering layer was a Net gains The Jasper did not just listen. She sang her own landmark in the use of technology to get around these song to the sea—a song of sonar. Experimental equip- problems. It was also a by-blow. The Jasperwas not out MILITARY ment on board beamed chirrups of sound into the there looking for deepwater plankton; it was working APPLICATIONS depths and listened for their return. When they came out how to use sonar (which stands forSound Naviga- Mutually assured back, they gave those on board a shock.
    [Show full text]
  • The Development of SONAR As a Tool in Marine Biological Research in the Twentieth Century
    Hindawi Publishing Corporation International Journal of Oceanography Volume 2013, Article ID 678621, 9 pages http://dx.doi.org/10.1155/2013/678621 Review Article The Development of SONAR as a Tool in Marine Biological Research in the Twentieth Century John A. Fornshell1 and Alessandra Tesei2 1 National Museum of Natural History, Department of Invertebrate Zoology, Smithsonian Institution, Washington, DC, USA 2 AGUAtech, Via delle Pianazze 74, 19136 La Spezia, Italy Correspondence should be addressed to John A. Fornshell; [email protected] Received 3 June 2013; Revised 16 September 2013; Accepted 25 September 2013 Academic Editor: Emilio Fernandez´ Copyright © 2013 J. A. Fornshell and A. Tesei. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. The development of acoustic methods for measuring depths and ranges in the ocean environment began in the second decade of the twentieth century. The two world wars and the “Cold War” produced three eras of rapid technological development in the field of acoustic oceanography. By the mid-1920s, researchers had identified echoes from fish, Gadus morhua, in the traces from their echo sounders. The first tank experiments establishing the basics for detection of fish were performed in 1928. Through the 1930s, the use of SONAR as a means of locating schools of fish was developed. The end of World War II was quickly followed by the advent of using SONAR to track and hunt whales in the Southern Ocean and the marketing of commercial fish finding SONARs for use by commercial fisherman.
    [Show full text]
  • Acoustics Today, July 2012 V8i3p5 ECHOES Fall 04 Final 8/14/12 11:17 AM Page 27
    v8i3p5_ECHOES fall 04 final 8/14/12 11:17 AM Page 25 COUNTING CRITTERS IN THE SEA USING ACTIVE ACOUSTICS Joseph D. Warren Stony Brook University, School of Marine and Atmospheric Sciences Southampton, New York 11968 Introduction “Alex Trebek asked me a “fancy fish-finder.” While this is true in few years after I finished gradu- a very broad sense, there are significant ate school, I was a contestant on simple question. How many differences between scientific Athe TV game show “Jeopardy,” echosounders and the fish-finders on where my performance could gener- krill does a whale eat when it most fishing boats. ously be described as terrible. During The first recorded incident (that I the between-rounds Question and opens its mouth and takes a am aware of) of active acoustic detec- Answer (Q&A) segment with host Alex tion of biological organisms was in the Trebek, we talked about my research on gulp? I froze and realized I “deep scattering layer” (DSL) (Dietz, Antarctic krill and he asked me a sim- 1948; Johnson, 1948). Early depth- ple question. “How many krill does a had no idea what the answer measuring systems used paper-charts to whale eat when it opens its mouth and record the strength of the echoes that takes a gulp?” I froze and realized I had was to his question.” were detected. The seafloor produced a no idea what the answer was to his very strong echo, however the chart- question. Having attended a few scientific conferences at recorder also showed weaker reflections occurring several this point in my career, I knew how to respond to a question hundred meters deep in the ocean that were definitely not the like this: sound knowledgeable, speak confidently, and seafloor.
    [Show full text]
  • METEOR-Berichte Mid-Atlantic Expedition 2003-2004 Cruise No
    METEOR-Berichte Mid-Atlantic Expedition 2003-2004 Cruise No. 60, Leg 1 – 5 November 11., 2003 – April 15., 2004 Kiel (Germany) –Funchal - Fort-de-France - Lisbon (Portugal) Autoren: D. Wallace, B. Christansen, J. Phipps-Morgan, Th. Kuhn, U. Send, Editorial Assistance: Senatskommission für Ozeanographie der Deutschen Forschungsgemeinschaft MARUM – Zentrum für Marine Umweltwissenschaften der Universität Bremen Leitstelle Deutsche Forschungsschiffe Institut für Meereskunde der Universität Hamburg 2011 The METEOR-Berichte are published at irregular intervals. They are working papers for people who are occupied with the respective expedition and are intended as reports for the funding institutions. The opinions expressed in the METEOR-Berichte are only those of the authors. The METEOR expeditions are funded by the Deutsche Forschungsgemeinschaft (DFG) and the Bundesministerium für Bildung und Forschung (BMBF). The reports are available in PDF format from http://www.dfg-ozean.de/. Editor: DFG Senatskommission für Ozeanographie c/o MARUM – Zentrum für Marine Umweltwissenschaften Universität Bremen Leobener Strasse 28359 Bremen Authors: Dr. Bernd Christiansen Universität Hamburg Telefon: +49(0)40-42838-6670 Institut für Hydrobiologie und Telefax: +49(0)40-42838-6696 Fischereiwissenschaft e-mail: [email protected] Zeiseweg 9, D-22765 Hamburg / Germany Prof. Dr. Jason Phipps Morgan GEOMAR Telefon: +49(0)431-600 2272 Forschungszentrum für Telefax: +49(0)431-600 2922 Marine Geowissenschaften e-mail: [email protected] Abt. Marine Umweltgeologie Wischhofstr. 1-3 24148 Kiel / Germany Dr. Thomas Kuhn Telefon: +49/(0)3731-393398 Department of Economic Geology and Telefax: +49/(0)3731-392610 Leibniz Lab. for Applied Marine Research e-mail: [email protected] Institute of Mineralogy Freiberg University of Mining and Technology Brennhausgasse 14 D-09596 Freiberg / Germany Prof.
    [Show full text]
  • Ocean Sciences Meeting 2020
    Thursday: Ocean Sciences Meeting 2020 Session Information Moderators: Damien Josset, US Naval Research Laboratory; David Ortiz-Suslow, Naval Postgraduate Oral Sessions School; Helen Czerski, University College London Sessions are being held in the Convention Center (CC) Poster Sessions The eLightning Theater is located in Hall C-D (Poster Hall). 0800h AI41A-01 Meridional contrasts of the Southern Ocean Posters are on display in the following venue throughout the week: Hall C-D (Poster Hall) mixed layer in response to summer forcing: M du Plessis, S Swart, A F Thompson, P M S Monteiro, L C Biddle, S Session & Paper Numbering A Nicholson Paper Numbers - A paper number designates the section, or other 0815h AI41A-02 Laboratory measurements of ocean surface sponsoring group, and chronology of the presentation. drag in extreme wind and wave conditions: B K Haus, M Example: AI21A-01 = Air-Sea Interactions, Tuesday, AM, concurrent Curcic session AI, first paper in that session. 0830h AI41A-03 Noble Gas Fluxes Reveal Links Between Air- AI 2 1 A - 01 sea Gas Exchange, Bubbles, and the Structure of the Air- sea Interface at High Wind Speeds: R H Stanley, L Kinjo, A W Smith, H R Alt, C F N Krevanko, D Aldrett, Day Time E B Kopp, B K Haus 0845h AI41A-04 Wave-generated Turbulence in the Coastal 1 = Monday 1 = AM 0800–1000 Ocean During Passage of a Tropical Cyclone: A Gargett, 2 = Tuesday 2 = AM 1030–1230 D K Savidge 0900h AI41A-05 Modeling whitecaps on global scale: A 3 = Wednesday 3 = PM 1245–1345 / 1400–1600 Raman, A Darmenov 4 = Thursday 4 = PM 1600–1800 0915h AI41A-06 A two-layer model of whitecap spectral reectance: R J Frouin, B Fougnie, J Tan 5 = Friday 5 = PM 1830–2030 0930h AI41A-07 Spectral Energy Budget Analysis in the The program is current as of 04 February 2020.
    [Show full text]
  • Oceanography and Marine Biology an Annual Review Volume 58
    Oceanography and Marine Biology An Annual Review Volume 58 Edited by S. J. Hawkins, A. L. Allcock, A. E. Bates, A. J. Evans, L. B. Firth, C. D. McQuaid, B. D. Russell, I. P. Smith, S. E. Swearer, P. A. Todd First edition published 2021 ISBN: 978-0-367-36794-7 (hbk) ISBN: 978-0-429-35149-5 (ebk) Chapter 2 Towards an Optimal Design for Ecosystem-Level Ocean Observatories Rodney A. Rountree, Jacopo Aguzzi, Simone Marini, Emanuela Fanelli, Fabio C. De Leo, Joaquin Del Rio & Francis Juanes (CC BY-NC-ND 4.0) Oceanography and Marine Biology: An Annual Review, 2020, 58, 79–106 © S. J. Hawkins, A. L. Allcock, A. E. Bates, A. J. Evans, L. B. Firth, C. D. McQuaid, B. D. Russell, I. P. Smith, S. E. Swearer, P. A. Todd, Editors Taylor & Francis TOWARDS AN OPTIMAL DESIGN FOR ECOSYSTEM- LEVEL OCEAN OBSERVATORIES RODNEY A. ROUNTREE1,2, JACOPO AGUZZI3, SIMONE MARINI4, EMANUELA FANELLI5, FABIO C. DE LEO6,2, JOAQUIN DEL RIO7 & FRANCIS JUANES2 1The Fish Listener, 23 Joshua Lane, Waquoit, Massachusetts, USA 2Department of Biology, University of Victoria, Victoria, Canada 3Instituto de Ciencias del Mar (ICM-CSIC), Barcelona, Spain 4National Research Council of Italy (CNR), Institute of Marine Sciences, La Spezia, Italy 5Department of Life and Environmental Sciences, Polytechnic University of Marche, Ancona, Italy 6Ocean Networks Canada, University of Victoria, Victoria, Canada 7OBSEA, SARTI, Universitat Politecnica de Catalunya (UPC), Barcelona, Spain Abstract Four operational factors, together with high development cost, currently limit the use of ocean observatories in ecological and fisheries applications: 1) limited spatial coverage, 2) limited integration of multiple types of technologies, 3) limitations in the experimental design for in situ studies, and 4) potential unpredicted bias in monitoring outcomes due to the infrastructure’s presence and functioning footprint.
    [Show full text]
  • Of Animals in Deep Scattering Layers 10 July 2017, by Kim Fulton-Bennett
    Undersea robot reveals 'schools' of animals in deep scattering layers 10 July 2017, by Kim Fulton-Bennett This research suggested that the layers were sometimes made up of one dominant type of animal but more often comprised a mixture of different animals. Marine acoustician Kelly Benoit-Bird, the lead author on the recent paper, brought this research into the 21st century, using deep-diving robots to take a close look at the animals within sound- scattering layers. In Fall 2013, her research team outfitted an autonomous underwater vehicle (AUV) with an advanced sonar system that acted like a This sonar data collected by an autonomous underwater very fancy fish finder. By programming the AUV to vehicle shows animals within a sound-scattering layer. swim above and through several sound-scattering The different colors indicate sound intensity and indicate layers, the team collected sonar data that allowed two distinct aggregations or schools (likely squid to the Benoit-Bird to identify individual animals within left and fish on the right), as well as two dolphins swimming within one of the aggregations. Credit: Kelly these layers, and to track predators that dove into Benoit-Bird the layers to hunt. While the AUV conducted sonar surveys within the sound-scattering layers, Benoit-Bird and her Throughout the world ocean, animals congregate collaborators towed a net through these same at certain depths, forming layers that can be layers. After bringing the net back on deck, they hundreds of meters thick and may extend counted and identified every animal in the net horizontally for dozens or even hundreds of between 1 and 35 centimeters (0.4 to 14 inches) kilometers.
    [Show full text]