Sharing OOI’s Cyberinfrastructure with NSF COMPASS Fellows

On Thursday March 7, 2024, Senior Manager of Cyberinfrastructure and OOI Data Lead Jeffrey Glatstein introduced a group of 18 students and seven instructors in the National Science Foundation’s CI Compass Fellowship Program (CICF) for Undergraduates to the challenges of collecting, distributing, and keeping safe OOI’s vast amount of data.  Students Fellows in CICF learn about real-world cyberinfrastructure challenges, and how to begin solving them for NSF Major Facilities

Glatstein first gave the group an overview of the type, amount, and diversity of data OOI collects from more than 900 instruments. The collected data consists of 135 billion rows of numerical data, 1.2 petabytes of raw data and nearly 10,000 hours of high-definition video, 327,000 hours of audio recordings, and 1.28 million digital still images.

He then shared OOI’s data delivery track record. Since 2016, OOI has responded to 987 million requests for calculated data, providing 333 terabytes of data.

[media-caption path="https://oceanobservatories.org/wp-content/uploads/2024/03/240307_OOI-Jeff-Glatstein_3.png" link="#"]Senior Manager of Cyberinfrastructure and OOI Data Lead Jeffrey Glatstein (green highlighted screen) discussed OOI’s cyberinfrastructure with 18 COMPASS Fellows and their instructors. Credit: CICF.[/media-caption]

Glatstein then went into detail about OOI’s extensive cybersecurity measures, which includes multiple storage sites with duplicate data to ensure that if the primary system went down, it could be quickly restored.  This is particularly important for OOI because its stores data for posterity for future use in long-term time-series.

The students were amazed and engaged, as demonstrated by multiple questions after the presentation.  Said Glatstein, “I enjoy sharing our work with students. It helps open their eyes to career opportunities in unexpected areas, like the ocean sciences, and their questions provides another way into looking at the work that we do.”

 

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NSF Announces Solicitation for OOIFB Support Office

On March 12, 2024, the U.S. National Science Foundation (NSF)  announced a solicitation (NSF 24-557) for proposals for an administrative support office to assist the NSF OOI Facility Board (OOIFB) in fulfilling its responsibilities. Details are available here.

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Bio-acoustic Sonar Echograms

The U.S. National Science Foundation Ocean Observatories Initiative (OOI) deploys bio-acoustic sonar instruments at all Arrays. Modified Kongsberg EK-60 instruments (ZPLSC-B) are deployed at the OOI Regional Cabled Array (RCA) on the seafloor at the OOI Endurance Array Oregon Shelf site (80 m depth) and at 200 m depth on the cabled mooring at the OOI Endurance Array Oregon Offshore site (Fig. 1). The EK-60s are being replaced with the newer EK-80 instruments, which came online during Summer 2023. ASL Environmental Sciences AZFP instruments (ZPLSC-C) are mounted on Surface Mooring Multi-Function Nodes (MFNs) at the Endurance Array Oregon and Washington Inshore sites and the Washington Shelf and Offshore sites, and formerly at the Pioneer NES Array Inshore, Central and Offshore sites (Fig. 2).  At the Global Arrays (Irminger Sea, Station Papa, and formerly Argentine Basin and Southern Ocean), upward and downward looking AZFP instruments (ZPLSG-A) are mounted in the top spheres of the Hybrid Profiler Moorings (~150 m depth).

[media-caption path="https://oceanobservatories.org/wp-content/uploads/2024/03/ROPOS.jpg" link="#"]Figure 1. Upper: The ROPOS ROV releasing the tungsten carbide calibration sphere on the Oregon Shelf (80 m) bioacoustic sonar platform. The EK60 transducer heads are orange. Credit: UW/NSF-OOI/CSSF; Dive R1792; V14. [/media-caption] [media-caption path="https://oceanobservatories.org/wp-content/uploads/2024/03/Jason.jpg" link="#"]Figure 1. Lower: The Jason ROV hovers above the Oregon Offshore Shallow Profiler platform in 200 m water depth, amid a swarm of krill. The neon orange EK80 sonar transducer heads are visible on the far left. Credit: UW/NSF-OOI/WHOI, Dive J2-1516, V23.[/media-caption]

The bio-acoustic sonar data are best visualized using echograms, which require processing the data then plotting the data products. In order to provide more accessible data products to the science community, OOI is generating echograms using the Python package Echopype. The Python code used and developed by OOI to generate the echograms via Echopype is freely available on GitHub. Data from the Endurance, Pioneer, and Global ASL AZFP instruments are processed from recovered instrument data, post-deployment. (Data Explorer refers to this as “Recovered Host” data.) The processing generates daily and weekly NetCDF files of the processed data as well as weekly echograms (Fig. 3), all available in the OOI Raw Data Archive (see the above-referenced GitHub README for file paths). Comparable processing will occur with data from the RCA Kongsberg EK-60 and EK-80 instruments; however, the processing will occur daily as new data are delivered to shore. In addition, the converted raw data files, formatted following the ICES SONAR-netCDF4 convention and produced by Echopype, are also in the Raw Data Archive.

[media-caption path="https://oceanobservatories.org/wp-content/uploads/2024/03/Transducers.jpg" link="#"]Figure 2.  Picture of the ZPLSC-C transducers mounted on the Pioneer Central Surface Mooring MFN.  The transducers are angled at 15 degrees away from the mooring riser to reduce interference.  © WHOI.[/media-caption]

The Echopype-generated NetCDF files from the Raw Data Archive are compiled into the longer time-series visualizations and are available in Data Explorer. More data have been added since our online July 2023 Town Hall, with a recorded version  here.

For more information about research using bio-acoustic sonar data, and using the Echopype software, see this excerpt from the OOI Science Plan, 2021. Another example using raw data can be foundhere.

[media-caption path="https://oceanobservatories.org/wp-content/uploads/2024/03/Eclipse.png" link="#"]Figure 3. Example echogram from the RCA managed, Coastal Endurance, Oregon Offshore Cabled Shallow Profiler Mooring (CE04OSPS). Data were collected from 2017-08-20 through 2017-08-27. Of special note is the total solar eclipse that occurred on 2017-08-21. The path of totality passed directly over this site on the morning of 2017-08-21. The response of the zooplankton to the changing light levels can be seen in a brief reversal of the diel vertical migration as the eclipse reached totality at 18:16 UCT (as shown in area with dotted white lines).[/media-caption]

 

 

 

 

 

 

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Pioneer MAB Array Workshop Applications

~ OOIFB Workshop Announcement ~
Coastal Pioneer MAB Array Community Workshop
September 10-12, 2024
Old Dominion University, Norfolk, VA
Application Deadline:  March 26, 2024

The Ocean Observatories Initiative Facility Board (OOIFB) will host a community workshop focusing on current and future initiatives that can be addressed using data from the National Science Foundation’s (NSF) OOI Coastal Pioneer Array, which is planned to be relocated to the Southern Mid-Atlantic Bight. The workshop will be held at the Webb University Center, Old Dominion University, in Norfolk, VA, on September 10-12, 2024.

The event will bring together a diversity of scientists, resource managers, educators, and other stakeholders to learn about the capabilities of the Coastal Pioneer MAB Array and the cutting-edge research that can be done in this new location. The workshop also will provide a forum to facilitate cross-network collaborations, identify strategies for better engaging current and future users of the NSF’s OOI, and foster the research and proposal development process. NSF OOI Program team members and NSF representatives will be on hand to answer questions and provide information on NSF OOI operations.

Researchers who are using or are considering using NSF OOI data; resource managers from national, state, and tribal agencies; and educators at all levels interested in using data from the NSF OOI Coastal Pioneer MAB Array are encouraged to participate in this community workshop. To apply for the workshop, please complete the online application form that is available on the workshop web page. Travel support is available, but limited. Broad representation from institutional, geographic, and disciplinary groups is desired and will be considered in participant selection. The deadline for applications is March 26, 2024.

Additional details about the workshop and agenda are available here. If you have any questions, please be in touch.

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Is Axial Seamount Napping?

Oregon State University Researcher Bill Chadwick attempted to answer this question in a poster he presented at AGU in December 2023. Chadwick has been watching the “ups and downs” of Axial Seamount for more than 30 years, including its last eruption in 2015. He and other observers monitor the seamount’s activity using bottom pressure recorders (BPR) connected to the US National Science Foundation Ocean Observatories Initiative (NSF OOI) Regional Cabled Array (RCA), operated by the University of Washington, along with additional uncabled BPRs and Mobile Pressure Recorder surveys at an array of seafloor benchmarks every two years using a remotely operated vehicle.

[media-caption path="https://oceanobservatories.org/wp-content/uploads/2024/03/BPR-scaled.jpg" link="#"]A repeatable inflation-deflation cycle has been documented at Axial Seamount over the last 30 years, using autonomous, battery-powered Bottom Pressure Recorders (BPRs), and later cabled-BPRs like this one connected to the OOI-RCA. Credit: UW/NSF-OOI/CSSF, 2014.[/media-caption]

“Axial Seamount has erupted three times in the last 25 years. As of March 2024, the seamount is 90-95% reinflated to the level it reached before the 2015 eruption, so we’re getting close to the eruption triggering point,” said Chadwick. “But on the other hand, the rate of inflation, which started high right after the 2015 eruption, has been decreasing and decreasing since then.”

The inflation rate reached nearly zero last summer (just slightly positive at ~1 cm/year, the lowest rate seen at Axial).   “At that very low rate, it was hard to tell how long it would take to reach the 2015 inflation threshold,” Chadwick added.

Since October 2023, however, the rate of uplift has been slowly increasing. University of Washington Researcher William Wilcock’s Axial Seamount Earthquake Catalog page also indicates the seismicity has been on the rise since October 2023, with a large swarm of >600 events on 10 February.

“Since October 2023, the rate of inflation has increased a bit to 5-6 cm/yr, which is still quite low compared to rates we’ve seen over the last 25 years but seems to indicate that Axial may be coming out of its slumber of last summer,” Chadwick explained.  “And the earthquake swarm on Feb 10 also seems to support that notion.”

Longer-term eruptive history documented by mapping and dating lava flows at the summit shows that Axial has produced at least 50 eruptions in the last 800 years, (Clague et al., 2013), an average of one every 15-18 years, suggesting that the current lull at Axial might not be long.

“I’m hoping that the rate of inflation will continue to increase, but it’s too early to tell.  Anything could happen,“ Chadwick added.  “I’m more hopeful than I was a year ago that the next eruption may not be too far off but only time will tell!”

[media-caption path="https://oceanobservatories.org/wp-content/uploads/2024/03/Chadwick-dots.jpg" link="#"]Map showing the locations of Mobile Pressure Recorder (MPR) benchmarks, as well as the autonomous and cabled Bottom Pressure Recorders (BPR). The red dots are the BPRs connected to OOI Regional Cabled Array.[/media-caption]

 

Reference: Clague, D.A., et al., (2013) Geologic history of the summit of Axial Seamount, Juan de Fuca Ridge, Geochem Geophys, Geosystems, doi: 10.1002/ggge.20240.

 

 

 

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Communicating with Colleagues Teaching with OOI Data

The Ocean Observatories Initiative (OOI) and the OOI Ocean Data Labs are serious collaborators.  While two different NSF-funded initiatives share portions of their names, their roles are different, but complementary.  The OOI provides data that the OOI Ocean Data Labs Project uses to prepare instructional materials for undergraduate classrooms. It’s a collaboration that helps to expand the use of OOI data into classrooms and into the hands of potential future researchers.

To honor this collaboration, the OOI has launched a new Discourse forum OOI in the Classroom where educators can share their experiences teaching with OOI data and establish dialogues with their colleagues. This forum is designed to offer an online area to share ideas, tell tales, and work to develop supportive, instructive, and challenging classroom experiences.

The OOI Ocean Data Labs also hosted an in-person workshop at the recent Ocean Sciences Meeting to introduce faculty to the community-developed collection of OOI Data Explorations and the online OOI Lab Manual. The workshop invited participants to integrate OOI data into undergraduate courses (Greengrove et al., 2020), to not only teach concepts in oceanography but to build transferable skills.

The Ocean Data Labs is holding a workshop (June 2-5, 2024 at the Marine Science Center, University of North Carolina Wilmington) that will focus on the relocation of the Pioneer Array to the Mid-Atlantic Bight, and the potential this move will provide for future educational lessons and student research activities. Learn more and apply to attend. Participants will be selected and notified by mid-April.

Another way to get involved  is to join the Ocean Data Labs mailing list to learn of the latest innovations and lesson plans developed by this network of educators.  Also, be sure to sign on to Discourse to continue the ongoing conversation within the education network of OOI data users.

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Live Data Demos at OOI Booth#210

Join OOI data expert Stace Beaulieu at the Ocean Sciences Meeting as she demonstrates how to use Data Explorer to find, compare, and share OOI data. During each session, Stace will use data from a different OOI array to demonstrate the breadth and depth of data available and how easy it is to access, download, and use.  She will demo Data Explorer, followed by plenty of time to answer your questions and use this tool to explore data relevant to your research. On Wednesday morning, she’ll demo JupyterHub so you will have another tool to use OOI data in your research.

Mark your calendar, as follows, and come visit Stace at OOI’s booth #210 at the Ocean Sciences Meeting February 19-22, 2024.

Find, compare, and share OOI data

  • Monday Feb 19
    3:30-4:00 pm
    Global Irminger Sea Array
  • Tuesday Feb 20
    10:00-10:30 am
    Coastal Endurance Array
    3:30-4:00 pm 
    Coastal Pioneer New England Shelf Array
  • Wednesday Feb 21
    10:00-10:30 am 
    JupyterHub demo for AUV data from Coastal Pioneer New England Shelf Array
    3:30-4:00 pm 
    Global Southern Ocean Array
  • Thursday Feb 22
    10:00-10:30 am
    Regional Cabled Array

A complete list of OOI-related events at the Ocean Sciences Meeting 2024 can be found here.

 

 

 

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OOI at Ocean Sciences Meeting 24

OOI will be at booth #210 at the Ocean Sciences Meeting in New Orleans from 18-23 February 2024. Please visit our booth.  Daily we have an OOI data expert giving in-person demonstrations on how to use Data Explorer in your research.  Times and topics will be announced soon, so stay tuned.

The following is a compilation of OOI-related presentations at this year’s Ocean Sciences Meetinh. If we’ve missed any OOI-related sessions, please contact dtrewcrist@whoi.edu and we will be happy to add them.  Hope to see you in person this year! Share your OSM news at #OSM24. 

Monday, 19 February 2024

09:40 – 09:50 Eastern (08:40 – 08:50 CST) 203-205, Second Floor (Convention Center)

AI11A-02 Air-Sea Flux Impacts Over Misaligned Waves During Atmospheric Cold Fronts 
Cesar Sauvage1, Hyodae Seo2, James B Edson1 and Carol Anne Clayson3, (1)Woods Hole Oceanographic Institution, Woods Hole, MA, United States, (2)WHOI, Woods Hole, United States, (3)Woods Hole Oceanographic Institution, Physical Oceanography, Woods Hole, MA, United States

10:03 – 10:14 Eastern (09:03 – 09:14 CST) 215-216, Second Floor (Convention Center)

OT11A-04 Expanding surface wave observations at the OOI Pioneer Array – New England Shelf using buoy motion sensors
Andrew C Reed and James B Edson, Woods Hole Oceanographic Institution, Woods Hole, MA, United States

10:47 – 10:58 Eastern (09:47 – 09:58 CST) 208-209, Second Floor (Convention Center)

ED11A-08 Accessible Oceans: Using Data Sonification to Engage Diverse Audiences in Ocean Science 
Amy S Bower, Woods Hole Oceanographic Institution, Woods Hole, United States, Leslie M Smith, Your Ocean Consulting, Knoxville, United States, Jon Bellona, University of Oregon, School of Music and Dance, Eugene, United States, Jessica Roberts, Georgia Institute of Technology, College of Computing, Atlanta, United States and Huaigu Li, Georgia Institute of Technology Main Campus, Atlanta, United States

11:45 – 11:55 Eastern (10:45 – 10:55 CST) R06-R07, Second Floor (Convention Center)

OB12C-02 The seasonality of chlorophyll and cloudiness from high-latitude ocean moorings 

Katherine Shrader, James Madison University, Geology and Environmental Science, Harrisonburg, VA, United States, Nicole S Lovenduski, University of Colorado, Department of Atmospheric and Oceanic Sciences, Boulder, CO, United States and Genevieve Clow, University of Colorado at Boulder, Atmospheric and Oceanic Sciences, Boulder, United States

15:30-16:00 CST Exhibit Hall, Booth #210
Data Demo on Global Irminger Sea Array

15:49 – 15:58 Eastern (14:49 – 14:58 CST) 229-230, Second Floor (Convention Center)

PI13A-06 Inner Shelf Nitrate Response to Wind Forcing on the Newport Hydrographic Line, Oregon, USA

Andrew Scherer, Oregon State University, College of Earth, Ocean, and Atmospheric Sciences, Corvallis, United States, Melanie R Fewings, Oregon State University, College of Earth, Ocean, and Atmospheric Sciences, Corvallis, OR, United States and Thomas Connolly, Moss Landing Marine Laboratories, Moss Landing, CA, United States

16:06 – 16:17 Eastern (15:06 – 15:17 CST) 225-227, Second Floor (Convention Center)

PL13A-07 Biological and physical drivers of interannual variability in long-term carbon sequestration by the subpolar North Atlantic biological pump
Kristen E Fogaren1, Hilary I Palevsky1, Meg F. Yoder1, Femke de Jong2, Isabela Le Bras3 and David P Nicholson4, (1)Boston College, Earth and Environmental Sciences, Chestnut Hill, United States, (2)Royal Netherlands Institute for Sea Research, Texel, Netherlands, (3)Woods Hole Oceanographic Institution, Woods Hole, United States, (4)Woods Hole Oceanographic Institution, Marine Chemistry and Geochemistry, Woods Hole, MA, United States

17:00 – 19:00 Eastern (16:00 – 18:00 CST) Poster Hall, First Floor (Convention Center)

DS14A-0359 Distribution of microbial eukaryotes living as epibiota on tubeworms (Ridgeia piscesae) in hydrothermal fluid flow and vent plumes at Axial Seamount
Han Weinrich, University of Washington Seattle Campus, School of Oceanography, Seattle, United States
PL14B-2221 Drivers of inorganic carbon cycling in the central Irminger Sea
Meg F. Yoder1, Hilary I Palevsky2 and Kristen E Fogaren1, (1)Boston College, Earth and Environmental Sciences, Chestnut Hill, United States, (2)Boston College, Earth and Environmental Sciences, Chestnut Hill, MA, United States

15:00-18:00 CST Exhibit Hall – Visit OOI’s Booth #210

18:00 CST OOI Meet up at The Rusty Nail, 1100 Constance Street, New Orleans

Tuesday, 20 February 2024

09:30 – 11:00 Eastern (08:30 – 10:00 CST) eLightning Theater, First Floor (Convention Center)

ED21B-05 Patterns at the Edge: Ocean Biogeochemistry at the Edge of the Northeast U.S. Shelf Revealed by Autonomous Underwater Vehicles (AUVs)
Taina Sanchez1,2, Stace Beaulieu3, Heidi M Sosik4 and Bofu Zheng2, (1)University of Miami, Miami, United States, (2)Woods Hole Oceanographic Institution, Woods Hole, United States, (3)Woods Hole Oceanographic Institution, Biology, Woods Hole, MA, United States, (4)Woods Hole Oceanographic Institution, Woods Hole, MA, United States

1o:00-10:30 CST Exhibit Hall, Booth #210
Data Demo on Coastal Endurance Array

13:45 – 14:45 Eastern (12:45 – 13:45 CST) 220-222, Second Floor (Convention Center)

TH23LOcean Observatories Initiative Facility Board (OOIFB) Town Hall
Holly Morin, University of Rhode Island, Graduate School of Oceanography, Narragansett, RI, United States, Kendra L Daly, University of South Florida, College of Marine Science, St. Petersburg, United States and Dax Christian Soule, CUNY Queens College, School of Earth and Environmental Sciences, Flushing, NY, United States

15:30-16:00 CST Exhibit Hall, Booth #210
Data Demo on Coastal Pioneer New England Shelf Array

15:44 – 15:55 Eastern (14:44 – 14:55 CST) 211-213, Second Floor (Convention Center)

DO23A-05A Model for Community-driven Development of Best Practices: The Ocean Observatories Initiative Biogeochemical Sensor Data Best Practices and User Guide
Hilary I Palevsky, Boston College, Earth and Environmental Sciences, Chestnut Hill, United States, Sophie Clayton, National Oceanography Centre, Southampton, United Kingdom, Heather M Benway, Woods Hole Oceanographic Inst., Woods Hole, United States, Mai Maheigan, Woods Hole Oceanographic Institution, Marine Chemistry and Geochemistry, Woods Hole, MA, United States and The OOI Biogeochemical Sensor Data Working Group

17:00 – 19:00 Eastern (16:00 – 18:00 CST) Poster Hall, First Floor (Convention Center)

OT24B-1524 Assessment and Improvement of Dissolved Oxygen Measurements from NSF Ocean Observatories Initiative Gliders
Stuart Pearce1, Peter J Brickley2, Jonathan Whitefield3, Diana Wickman2, Collin Dobson2, Russell Desiderio3, Albert J Plueddemann2 and Edward Paul Dever4, (1)Oregon State University, College of Earth, Ocean, and Atmospheric Sciences, Corvallis, OR, United States, (2)Woods Hole Oceanographic Institution, Woods Hole, United States, (3)Oregon State University, College of Earth, Ocean, and Atmospheric Sciences, Corvallis, United States, (4)Oregon State University, Corvallis, OR, United States

OT24B-1523Application of Automated Quality Control Flags to OOI Data: Identification of Storm Events at Coastal Pioneer Array
Kylene Cooley, Woods Hole Oceanographic Institution, Ocean Observatories Initiative, Woods Hole, United States and Andrew C Reed, Woods Hole Oceanographic Institution, Woods Hole, MA, United States

OT24D-1537 Comparison of Vertical Temperature and Salinity Structures in the Northeast Pacific Ocean from Nested Regional Ocean Models 
Caitlin Amos, US Naval Research Laboratory, Stennis Space Center, United States, John J Osborne, U.S. Naval Research Laboratory, Ocean Sciences Division, Stennis Space Center, MS, United States and Gregg A. Jacobs, Naval Research Lab, Stennis Space Center, MS, United States

PI24B-1683Bloom Compression By Marine Heatwaves Contemporary With the Oregon Upwelling Season  
Ian Black1, Maria T Kavanaugh1 and Clare E Reimers2, (1)Oregon State University, College of Earth, Ocean, and Atmospheric Sciences, Corvallis, United States, (2)Oregon State University, College of Earth, Ocean, and Atmospheric Sciences, Corvallis, OR, United States

10:00-18:00 CST Exhibit Hall – Visit OOI’s Booth #210

Wednesday, 21 February 2024

09:50-10:00 Eastern (08:50 – 09:00 CST) 210, Second Floor (Convention Center)

DO31A-03 Building Training Datasets through the Documentation of Species Diversity and Abundance at ASHES vent field, Axial Seamount, for Future Machine Learning Applications
Julia Sandke1, Danilo Seskar2, Hikari Oshiro2, Karen G Bemis3 and Dax Christian Soule4, (1)CUNY Queens College, School of Earth and Environmental Sciences, Flushing, United States, (2)Rutgers University New Brunswick, Marine and Coastal Sciences, New Brunswick, United States, (3)Rutgers, The State University of New Jersey – New Brunswick, Marine and Coastal Sciences, New Brunswick, United States, (4)CUNY Queens College, School of Earth and Environmental Sciences, Flushing, NY, United States

1o:00-10:30 CST Exhibit Hall, Booth #210
JupyterHub demo for AUV data from Coastal Pioneer New England Shelf Array

15:30-16:00 CST Exhibit Hall, Booth #210
Data Demo on Global Southern Ocean Array

17:00-19:00 Eastern (16:00 – 18:00 CST) Poster Hall, First Floor (Convention Center)

OT34B-1585 A Glider Study of Seasonal Changes in Bio-Optical Properties and Phytoplankton Biomass at the New England Shelf Break Front
Robert D Vaillancourt, Millersville University of Pennsylvania, Millersville, PA, United States and Michael A. Miller, Millersville University of Pennsylvania, Earth Sciences, Millersville, United States

ED34B-0145 Correlation of Diffuse Venting with Geophysical Time Series at Axial Seamount   
Cal Mills1, Melissa Celik1, Fabio Dos Santos1, Karen G Bemis2 and Dax Christian Soule3, (1)CUNY Queens College, Flushing, United States, (2)Rutgers, The State University of New Jersey – New Brunswick, Marine and Coastal Sciences, New Brunswick, United States, (3)CUNY Queens College, School of Earth and Environmental Sciences, Flushing, NY, United States

PS34B-2105 What makes the seasonal stratification breakdown at the US Northeast shelfbreak front so rapid? – Comparing contributions from surface forcing, local mixing, and lateral advection 
Lukas Lobert1,2, Ke Chen2, Albert J Plueddemann2 and Glen Gawarkiewicz2, (1)Massachusetts Institute of Technology, Cambridge, United States, (2)Woods Hole Oceanographic Institution, Woods Hole, United States

10:00-18:00 CST Exhibit Hall – Visit OOI’s Booth #210

Thursday, 22 February 2024

10:14-10:25 Eastern (09:14- 09:25 CST) 225-227, Second Floor (Convention Center)

PI41A-05 Interannual variability in the physical and biological drivers of carbon sequestration in the southeast Pacific Subantarctic Mode Water Formation region
Peter Brown1, Pablo Trucco-Pignata2, Maribel García-Ibáñez3, Dorothee C E Bakker4, Sophy Oliver1, Paula C. Pardo5 and Adrian Martin1, (1)National Oceanography Centre, Southampton, United Kingdom, (2)University of Southampton, Southampton, United Kingdom, (3)Institut de Ciències del Mar – CSIC, Barcelona, Spain, (4)University of East Anglia, Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, Norwich, United Kingdom, (5)Instituto de Investigacións Mariñas (IIM-CSIC), Vigo, Spain Peter Brown1, Pablo Trucco-Pignata2, Maribel García-Ibáñez3, Dorothee C E Bakker4, Sophy Oliver1, Paula C. Pardo5 and Adrian Martin1, (1)National Oceanography Centre, Southampton, United Kingdom, (2)University of Southampton, Southampton, United Kingdom, (3)Institut de Ciències del Mar – CSIC, Barcelona, Spain, (4)University of East Anglia, Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, Norwich, United Kingdom, (5)Instituto de Investigacións Mariñas (IIM-CSIC), Vigo, Spain

1o:00-10:30 CST Exhibit Hall, Booth #210
Data Demo on Regional Cabled Array

12:10-12:200 Eastern (11:10- 11:20 CST) 217-219, Second Floor (Convention Center)

OT42A-05 Adding a wave energy converter to the Pioneer Array Coastal Surface Mooring 
Ryan Coe, PhD1, Albert J Plueddemann2, Giorgio Bacelli3, Derek Buffitt4, J. Andrew Hamilton5, Kevin Dullea6, Scott Jenne7, Frederick Driscoll8, Umesh A Korde9, Salman Husain8, Mike Muglia10, Jantzen Lee6, Johannes Spinneken11, Sahand Sabet8, Carrie Schmaus12, John Reine13, Patterson Taylor14, Donald Peters13, Amanda M Vieillard15 and Eric Wade16, (1)Sandia National Laboratories, Water Power Technologies, Albuquerque, United States, (2)Woods Hole Oceanographic Institution, Woods Hole, United States, (3)Sandia National Laboratories, Albuquerque, United States, (4)Woods Hole Oceanographic Institution, Applied Ocean Physics and Engineering, Woods Hole, United States, (5)Monterey Bay Aquarium Research Institute, Moss Landing, CA, United States, (6)Sandia National Laboratories, United States, (7)National Renewable Energy Laboratory Golden, Golden, United States, (8)National Renewable Energy Laboratory, United States, (9)Johns Hopkins University, Baltimore, MD, United States, (10)Coastal Studies Institute, United States, (11)Evergreen Innovations, United States, (12)Department of Energy, Water Power Technologies Office, Washington DC, United States, (13)Woods Hole Oceanographic Institution, United States, (14)University of North Carolina Coastal Studies Insitute, Wanchese, NC, United States, (15)US Department of Energy, Water Power Technologies Office, Washington, DC, United States, (16)East Carolina University, Greenville, United States

17:00-19:00 Eastern (16:00 – 18:00 CST) Poster Hall, First Floor (Convention Center)

OT44A-1627Towards acoustic observations of ocean basin temperatures using the Kauai beacon and Ocean Observatories Initiative Hydrophones
John Ragland1, Nicholas Durofchalk2, Shima Abadi1, David Dall’Osto3 and Kay Gemba2, (1)University of Washington, Seattle, United States, (2)Naval Postgraduate School, Monterey, United States, (3)Applied Physics Laboratory University of Washington, Seattle, United States

ED44C-0222An Introductory Oceanography lab sequence implementing a combination of OOI Data Labs and basic lab science experiments
Alexander Wurm, Western New England University

OB44F-1014 Fall-Winter Seasonal Dynamics in the In Situ Bio-Optics for the Mid-Atlantic Bight 
Teemer Barry, Rutgers University New Brunswick, Marine & Coastal Sciences, New Brunswick, United States, Oscar Schofield, Rutgers University, Center of Ocean Observing Leadership, School of Environmental and Biological Sciences, New Brunswick, United States and Grace Saba, Rutgers University, Department of Marine and Coastal Sciences, New Brunswick, United States

ED44C-0218 The OOI Data Lab Manual: Using large ocean observatory data to improve data literacy in multi-modal undergraduate courses
Anna Pfeiffer-Herbert, Stockton University, Galloway, United States, Denise Bristol, Hillsborough Community College – SouthShore, Biological and GeoSciences, Ruskin, United States, Charles Sage Lichtenwalner, Rutgers University, Marine and Coastal Sciences, New Brunswick, United States and Janice McDonnell, Rutgers University New Brunswick, Marine & Coastal Sciences, New Brunswick, United States

ED44C-0220 Engaging Introductory Oceanography Students with Real Data in the Classroom and Online: OOI Data Exploration and Data Labs
Melissa Hicks, PHD, Onondaga Community College, Liberal Arts and Sciences, Syracuse, NY, United States

ED44C-0220 Engaging Introductory Oceanography Students with Real Data in the Classroom and Online: OOI Data Exploration and Data Labs
Mikelle Nuwer, University of Washington, School of Oceanography, Seattle, WA, United States

ED44C-0219 A Scaffolded Approach to Data Literacy Skills in 2YC Students using Authentic Data from OOI and other Sources 
Denise Bristol, Hillsborough Community College – SouthShore, Biological and GeoSciences, Ruskin, United States, Anna Pfeiffer-Herbert, Stockton University, Galloway, United States and Jessica Olney, Hillsborough Community College, Physical Sciences, Tampa, United States

10:00-13:00 CST Exhibit Hall – Visit OOI’s Booth #210

Friday, 23 February 2024

09:34 -09:43 Eastern (08:34- 08:43 CST) 208-209, Second Floor (Convention Center)

ED51A-01 Reflections from the OOI Data Labs Community of Practice
Janice D McDonnell, Rutgers University New Brunswick, Department of Youth Development, New Brunswick, United States, Charles Sage Lichtenwalner, Rutgers University, Marine and Coastal Sciences, New Brunswick, United States, Ellen A R Iverson, Carleton College, SERC, Northfield, MN, United States, Ellen Altermatt, University of Utah, Utah Education Policy Center, Salt Lake City, United States, Anna Pfeiffer-Herbert, Stockton University, Pomona, United States, Denise Bristol, Hillsborough Community College – SouthShore, Biological and GeoSciences, Ruskin, United States and Dax Christian Soule, CUNY Queens College, School of Earth and Environmental Sciences, Flushing, NY, United States

09:43 -09:52 Eastern (08:43- 08:52 CST) 208-209, Second Floor (Convention Center)

ED51A-02 Using interactive OOI data visualizations to improve data literacy and scientific reasoning skills in undergraduate students
Gabriela W Smalley1, Charles Sage Lichtenwalner2, Andrea Drewes1 and Kathy Browne1, (1)Rider University, United States, (2)Rutgers University, Marine and Coastal Sciences, New Brunswick, United States

 09:52 – 10:01 Eastern (08:52- 09:01 CST) 208-209, Second Floor (Convention Center)

ED51A-03 Research Shows OOI Data Lab Activities Enhance Student Success 
Claire Condie, Middlesex County College, Edison, United States

10:01-10:10 Eastern (09:01-– 09:10 CST) 208-209, Second Floor (Convention Center)

ED51A-04 Using Oceanographic Mooring and Satellite Datasets to Teach Data Analysis and Scientific Computing Skills for Undergraduate Students
Hilary I Palevsky, Boston College, Earth and Environmental Sciences, Chestnut Hill, United States

15:02-15:12 Eastern (14:02-14:12 CST) 211-213, Second Floor (Convention Center)

RH53A-01 From shelfbreak to shoreline: What is the relationship between coastal sea level and local ocean dynamics?
Carolina Camargo1, Christopher G Piecuch1 and Britt Raubenheimer2, (1)Woods Hole Oceanographic Institution, Woods Hole, United States, (2)Woods Hole Oceanographic Institution, Applied Ocean Physics & Engineering, Woods Hole, United States

 

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Battling the Corrosive Properties of Seawater

OOI engineers face the challenge of keeping ocean observing equipment operational in demanding locations for up to a year at a time. In addition to wind, waves, extreme pressure, ship traffic and trawling disruption, engineers continually battle the corrosive properties of salt water.

Senior Technician for OOI’s Coastal Endurance Array Kristin Politano provided a primer on OOI’s tactics to prevent corrosion of its equipment and instrumentation. “It’s a fun balancing act between cost versus strength versus weight versus durability. Different metals are great for certain things, so we use them in different places.”

OOI engineers try to avoid all forms of corrosion, especially galvanic corrosion, an electrochemical process where one metal corrodes preferentially in the presence of an electrolyte.  In this case, seawater serves as the electrolyte or the corrosion “enabler.” When two dissimilar metals are connected in seawater, one of them is going to corrode faster than the other.

Since zinc is very prone to corrosion and corrodes much faster than other materials used on OOI moorings, engineers use it as a “sacrificial lamb” in OOI operations. They place zinc strategically on the moorings to encourage galvanic corrosion to occur on the zinc, rather than degrading instruments, electronics, and the frames that hold the moorings and instrumentation in place.

Politano gave an example of how zinc works to protect other metals used on the moorings. Aluminum is used on the Coastal Surface Piercing Profiler frames (CSPP), the Near-Surface Instrument Frames (NSIF), a cage that contains ocean observing instruments below surface moorings, and Multi-function Nodes (MFN) frames, which are at the base of some surface moorings and act both as anchors as well as platforms to affix instruments.

[media-caption path="https://oceanobservatories.org/wp-content/uploads/2024/01/IMG_376765-scaled.jpg" link="#"]Members of the Coastal Endurance Team deploy a Coastal Surface Piercing Profiler (CSPP) into the Pacific off the coast of Oregon. The zincs are the bare metal disks attached to the CSPP frame near loops at the top of the frame. Credit: Jon Fram, OSU.[/media-caption]

The NSIF, MFN, and CSPP have sacrificial zinc cylinders attached so that when the frames containing the instruments go into the water, the aluminum doesn’t degrade as quickly as it might otherwise. The zinc will degrade first, providing a protective layer for the important assets within the frames.  “Zinc serves as a really effective form of galvanic corrosion protection,” Politano added. “Zincs come in many different form factors, but we use ones that can be bolted directly to the mooring frames and other mechanical components,” said Politano.

Location Dictates Effectiveness

Zincs are used on both the Coastal Endurance’s inshore and offshore mooring platforms. The zincs on the inshore platforms dissolve faster and require replacement more often due to low dissolved oxygen conditions and that encourage corrosion.  Zincs on the offshore moorings last longer due to a higher oxygenated environment offshore.

Decisions about materials to use on various parts of the moorings also in part, depends on durability, conditions, and cost. Stainless steel is very durable and reacts to form a protective oxide film on its outer surface, but this reaction needs oxygen to grow and repair itself. In areas with hypoxia (lack of oxygen) particularly in the summer months, there is not enough oxygen in the water column for the stainless oxide layer to rebuild and repair itself.

[media-caption path="https://oceanobservatories.org/wp-content/uploads/2024/01/MFN.jpg" link="#"]Coastal Pioneer Array Team members get ready to deploy a 9000-pound multi-function node off the coast of Martha’s Vineyard. Credit: Rebecca Travis © WHOI.[/media-caption]

Delrin, a high-grade plastic (acetyl resin), is also used on the moorings as a corrosion preventive measure. Because of Delrin’s durability, stiffness, light weight, and water resistance, Delrin is used in instrument housings and electrical panels because it doesn’t conduct electricity, but it lacks the strength of aluminum.  “Delrin is strong, but not as strong as aluminum. So, we wouldn’t make a mooring tower or a mooring Halo out of a plastic material,” said Politano.  Components above water are made from aluminum because it is lightweight and extremely strong.  To increase strength and resilience, above water aluminum components are powder coated that prevents water from contacting the metal. The powder coating contains various pigments, polymer resins, curatives, leveling agents, and other additives, which is applied to an aluminum surface with an electrostatic spray.  “The powder coating is sprayed on, and cured in an oven that triggers a chemical reaction that hardens the coating, making a hard shell, protecting the metal beneath it,” she explained.  “A good way to imagine it is like a big M&M covering the chocolate metal inside,” she added.

The OOI team uses silicon bronze (bronze coated with a silica coating) and titanium for many underwater components. The silicon bronze has mild anti-fouling properties, which is important for OOI’s coastal arrays to help reduce biofouling. The mooring components go from a bright coppery color to a green, blue patina color. The patina acts as a durable, strong, protective layer that is highly resistant to corrosion and doesn’t fatigue.  “We use silicon bronze to bolt instrument clamps to MFN and NSIF frames and to attach instrument to the frames. The benefit of silicon bronze is that it is much cheaper than some of the other materials like titanium, so we can afford to use it many places,” said Politano.

Balancing Cost and Placement Considerations

Titanium is a fantastic material to use in the marine environment because it is highly corrosion resistance, very strong, and can remain in a marine environment for a long time. The downside is that it is very expensive, so it is used judiciously.  Titanium also has a high strength to weight ratio, which makes it ideal for floating things in the water column and  it is used to bolt together all of the critical structural mooring components. For instance, titanium bolts are used to connect surface buoys to the electromechanical chain (EM), which contains electrical components allowing power and communication with the below surface elements, to the NSIF and stretch hoses to the MFN, which anchors the mooring on the sea floor. Like stainless steel, titanium has a protective oxide layer with the ability to “heal itself.”

In addition to strength, durability, and cost the OOI team must consider the mix of materials it uses, avoiding places where two metals might touch each other. For example, copper is used as a primary anti-fouling material to mitigate the ever-present challenge of minimizing marine growth. Copper is soft so it isn’t used to attach critical mooring components. Care must be taken to avoid any dissimilar metals coming in contact with one another.  The outcome of such contact would be an extreme case of galvanic corrosion!

“It really is this sort of ballet of trying to balance the cost of the material versus the strength of the material versus the weight. We put lightweight materials above the water. The expensive materials that are really strong are used to hold the whole mooring together. And then the in-between materials that are strong, but not as expensive as the really strong materials, are used to hold all the instruments together. So, it’s a fun little balancing act,” Politano concluded.

As it turns out choosing the right materials also is a good return on investment. According to OOI Lead Systems Engineer Matthew Palanza, “While the cost of these corrosion-prevention materials is high, the loss of equipment and data due to failures caused by corrosion is much greater.  Incorporating corrosion-prevention materials into the array extends their service life much longer.  This makes it possible for some housings, connectors, and other components to be re-used every time an array is redeployed.  In fact, some housings are designed to last for the 30-year duration of the program.”

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