Tackling Sea Surface Sampling Issues

The sea surface is the hardest place to work, according to Jonathan Fram, Project Manager of the Coastal Endurance Array. That’s because at the surface, waves are constantly sloshing around. At any time, a large wave can tug on mooring winch lines, creating sudden tension, which can wear down cables and even cause them to break.

Scuba divers know that surface waters are rough, but below a certain depth—about one wave orbital below the surface—the waters calm significantly. Unfortunately, a lot of great science takes place at the surface, so it’s important for sampling instruments like the Coastal Surface Piercing Profiler (CSPP) to be able to withstand the waves at and near the surface.  Fortunately, OOI engineers have found ways to meet the many challenges of working in this rough environment.

“The Coastal Endurance Array Team has made changes to the CSPP to make it more robust, so that we can get the kind of continuous time series that are so valuable to scientists,” said Fram.

A CSPP spends most of its time near the sea floor, but either two or four times a day, the profiler winches itself up to the surface, taking samples as it ascends. Once it reaches the surface, the profiler sends its data back to shore and then quickly returns to the safety of the seafloor. Profilers are important ocean observatory tools because they can help capture what is happening at certain depths where stationary instruments aren’t present. “We’ve had times where you get a persistent chlorophyll bloom at a certain depth where there is zero mooring data,” explained Fram. “So the CSPP sampling is needed to make sense of what’s happening. It’s impossible to have all the instruments at all depths. The CSPP fills in this gap.”

Last year, the Coastal Endurance Array team reviewed their activities looking for ways to reduce lost time at sea. One thing they discovered was that the anchor systems of the CSPPs were unreliable. To deal with this problem, the team created a new kind of anchor. The old profiler anchors had a chain between the profiler and anchor that helped dampen the waves so that the device was not tugged on when resting in between profiles. The chain, however, made it difficult to deploy the anchor in an upright position. Anchors need to be deployed upright so their recovery floats can be acoustically released. The team redesigned the anchors so they now behave like a weeble wobble toy that is weighted so it always rights itself. This new design makes it hard to deploy an anchor upside down, making the anchors more reliable.

The team also made updates to the modems that send data to shore. When the CSPP is at the surface, the winch must stay on because it keeps the antenna vertical. This time-on takes up about a quarter of the battery power. To reduce the power demand, the team switched out some of the iridium modems for cellular modems, which has allowed the CSPPs to send data more quickly. A faster modem means that the profiler spends less time at the surface, not only saving power, but reducing the risk of being damaged by a large wave. The team is currently working on upgrading to faster cellular modems that can connect further from shore.

“At the same time we are making these updates on the Oregon Shelf Mooring, we’re also implementing them on the Washington Shelf Mooring,” said Fram. “So an improvement on one platform is also leading to an improvement on another platform.”

A third innovation involves improvements to the batteries.

“When waves tug on the winch, it goes from being a power sink to a power source. That sometimes creates power spikes that can fry the connectors. So we’ve rewired the batteries to make them more robust,” explained Fram. The rewiring is expected to reduce the number of power failures and keep the CSPPs running continuously. “Since April when we first started using the rewiring scheme, we’ve had four profilers in the water with no problems for six weeks,” said Fram.

The team also is in the process of replacing batteries that power the profiler with their own design of rechargeable batteries. While OOI engineers prefer to use commercially available parts for easier repair and replacement, when parts on the market don’t fit their needs, they design their own. The new batteries will be more reliable than those they are replacing. The newly designed batteries will also be deployed on the wire-following profilers on the Coastal Pioneer Array.

“My focus is on making all of the Coastal Endurance instrumentation work,” said Fram. “When we’re able to get a full three months’ deployment through the winter, through super rough seas, that makes my day. Making improvements is what I look forward to the most.”

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Applications for the Pioneer Array Innovations Lab 2 due May 31st

Applications to apply for the Pioneer Array Innovations Lab 2 are due on May 31st. The Lab will be held each day during the week of June 21-25 (about 5-6 hours each day). During this Lab, participants will work to identify the observatory opportunities that can be offered by the Pioneer Array at its new location at the Mid-Atlantic Bight. Details are provided below.

The application form for the Pioneer Array Innovations Lab 2 is available here.

To learn more or to apply, please visit here.

 

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Innovative Instruments on the RCA

The Regional Cabled Array (RCA) provides power and bandwidth to a set of core OOI pressure sensor and tiltmeter instruments, developed by Dr. W. Chadwick, which measure subsidence or uplift of the seafloor, an important indicator of activity at Axial Seamount.  But these instruments undergo slow instrumental drift, which can be misinterpreted as seafloor height changes. To increase measurement accuracy, three novel instruments have been added to the RCA – the self-calibrating pressure recorder, flipping tilt meter, and A-0-A pressure sensor – to account and correct for instrument drift.

Researchers are field testing these new drift-and pressure-measuring instruments and comparing results with the conventional instruments onsite, with the intent of identifying which might be the most reliable over the long-term and under specific conditions. The pressure and tilt data being collected and served by these instruments are being incorporated into models that are increasing understanding of volcanic activity at isolated and hard-to-measure sites such as Axial Seamount. The instrument placements and ongoing research is supported by the National Science Foundation.

Flipping Tilt Meter and A-0-A

Dr. William Wilcock, of the University of Washington, oversees the flipping (or rotating) tilt meter and the A-0-A (A zero A) sensor deployed on the RCA for three years at Axial: it will be recovered this summer.  The A-0-A is currently deployed within Axial’s Caldera at the Central Caldera site.

Tilt meters are widely used on volcanoes because when volcanoes inflate the tilt of the ground changes. Because conventional tilt meters drift a lot, they are only useful in environments where there are big signals, or where changes happen quite quickly. The flipping tilt meter corrects for this drift and allows it to be used in areas with smaller, more subtle changes.

Wilcock explains the corrective principle, “I have an old-fashioned kitchen scale with a rotating needle.  Every time I put the tray on top of the scale, I have to zero it out by turning a dial.  All three instruments are based on resonant quartz crystal sensors which drift, so our calibrations are similar to the principle in a kitchen scale with a dial adjustment. “

A flipping tilt meter is a three-component accelerometer, which measures the acceleration of the Earth, in the vertical and in two horizontal directions. In the vertical, it measures the acceleration of gravity, 9.8 meters per second squared. In the horizontal, there’s no acceleration of gravity, so it measures nothing. But if the instrument tilts, a small component of gravity pulls the horizontals in the downward direction because the instruments are no longer completely level.

“Every month we rotate one of the horizontal channels into the vertical to measure the acceleration of gravity, which doesn’t change. So we compare the rate of acceleration of gravity from the prior measurement and calculate how much the instrument had drifted and correct for that drift,” added Wilcock.  Wilcock and his team have tested the flipping tilt meter on land at Piñon Flat in California and now on the seafloor at Axial Seamount.

At Axial, the flipping tilt meter has been proven to measure tilt within about one part in 106—a very small tilt signal. Wilcock hosts data collected by the flipping tilt meter through IRIS, the Incorporated Research Institutions for Seismology. Wilcock and his team are currently writing a paper where the calibration data from the instrument will be shared.

Wilcock hopes the next test site for the flipping tiltmeter is placement in a borehole, where it can be secured so as to not experience drift nor temperature changes.  Because the flipping tiltmeter doesn’t need recalibration, it holds promise for being a simple sort of “plug and play type” of tiltmeter.

[caption id="attachment_20232" align="alignright" width="400"] The Self-Calibrating Pressure Recorder (left) sits adjacent to the A-O-A instrument allowing cross comparison of data focused on seafloor deformation. Credit: UW/NSF-OOI/WHOI; V19.[/caption]

Wilcock also has an A-0-A  (Ambient – zero for atmospheric pressure- Ambient) instrument co-located with the Self-calibrating Pressure Recorder at Central Caldera.  The A-0-A instrument compares ocean pressure to atmospheric pressure, calculated by a barometer within the instrument to determine drift.

The A-0-A is equipped with two redundant pressure sensors and a valve that switches from measuring the pressure at the seafloor to measuring the pressure internal to the instrument.

When the valve switches to the internal pressure of the instrument, the drift of the two pressure sensors can be measured by comparing their reading to a barometer inside the instrument.  If the calibration is working, then the two calibrated readings of the two sensors should give the same reading when the valve switches back and they measure the pressure at seafloor.  Early results show that they agree within a few millimeters per year in 1500 meters of water.

University of Washington graduate student Erik Fredrickson is using data from the Flipping Tilt and A-0-A meters to help refine models of the inflation occurring at Axial Seamount. “With pressure data, you can see the pressure increasing and decreasing in minutes. Pressure measurements work opposite of what you might expect for we are basically measuring the weight of the water. So as a volcano inflates, it lowers pressure on a seafloor instrument, and when it erupts, we get a higher-pressure signal. It’s really helpful to have accurate pressure measurements so we can understand how the volcano is behaving.”

Self-calibrating Pressure Recorder

Drs. Glen Sasagawa and Mark Zumberge of the Institute of Geophysics and Planetary Physics at Scripps Institution of Oceanography, University of California, San Diego conceived of and built a self-calibrating pressure recorder (SCPR) in 2013. They initially tested their battery-operated prototype off the coast of California. All data were stored on the instrument, which had to be retrieved by boat and uplinked data back to shore.

The SCPR, installed at Axial Seamount in 2018, was a much more sophisticated version consisting of many mechanical elements, including a deadweight tester, an instrument whose history dates back to the 19th century.  The deadweight tester consists of a piston that fits inside a closely spaced cylinder, over which a mass is placed. Oil and hydraulic fluid are pumped in until the tester floats up in the middle of the cylinder, causing the piston to rise up. (see diagram below). When that occurs, the weight of the piston (mass x gravity) is balanced by the pressure acting on the surface area of the piston on the bottom. A mathematical formula is applied to calculate pressure (mass x gravity divided by the area).

[caption id="attachment_21228" align="alignleft" width="375"] The key components of the SCPR. A 41.6-cm diameter sphere contains two recording pressure gauges which record ambient seawater pressure. Once every ten days for a period of 20 min the two gauges are hydraulically connected to a piston gauge that provides a reference pressure used to determine their drift rates.[/caption]

One key change since the SCPR prototype is that it is no longer battery-powered. “RCA provided us with a slot on the cable and took care of getting the instrument placed and plugged into the network, and then getting the data onshore to Seattle,” explained Sasagawa. “From an investigator’s perspective, all I have to do to access our data is log onto an FTP site, grab some data, and I’m good to go.”

Every three months or so, Sasagawa logs onto a computer terminal in his office to gain access to the control panel of the SCPR calibrate and operate the SCPR.  “I have direct communication with an instrument that is some 1500 meters under the sea, hundreds of miles off the Oregon coast. It’s definitely very cool and an amazing capability,” he added.

The goal is to keep this SCPR onsite at Axial for five-years, during which time data are consistently transmitted and available for researchers here. Sasagawa hopes to next test the efficacy of the SCPR at the Cascadia subduction zone, which runs from Vancouver Island in Canada to northern California, with smaller signals than at Axial.

“I would just add that we can’t overemphasize the importance of having power and communications on the seafloor. With the cable right there, we have the really critical things that we take for granted in our daily lives… Just plugging something into the wall socket, and turning on Wi-Fi.  And certainly in the oceans, we just cannot take that for granted. This is key infrastructure. And having data come back in real or near real time is critical,” concluded Sasagawa.

 

 

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NOAA Ocean Exploration FY22 Funding Opportunity

We are sharing this notice on behalf of the NOAA Office of Exploration in case it is of interest to OOI data users:

NOAA Ocean Exploration (formally the NOAA Office of Ocean Exploration and Research, OER), is soliciting proposals to conduct or support ocean exploration resulting in outcomes that provide or enable initial assessments about unknown or poorly understood regions of U.S. waters. This funding opportunity will focus on the outcomes of the Workshop to Identify National Ocean Exploration Priorities in the Pacific hosted by the Consortium for Ocean Leadership (COL) in 2020 in partnership with OER. Proposals should support the ocean exploration topical priorities or spatial priorities in the U.S. Exclusive Economic Zone (EEZ) identified in the “Report on the Workshop to Identify National Ocean Exploration Priorities in the Pacific.”

Proposals should also support the National Strategy for Mapping, Exploring, and Characterizing the United States Exclusive Economic Zone (national strategy). Proposals for the ocean exploration and marine archaeology themes must be for projects in unknown or poorly understood areas as referenced in the national strategy’s implementation plan and within the U.S. EEZ in the Pacific Ocean.

The Pacific priorities workshop report stresses the active awareness of the cultural context in which ocean exploration is often conducted. Recognizing the unique and numerous Pacific communities as partners and stakeholders enhances the overall impact of the ocean exploration enterprise through wider public support, a more diverse workforce and community of practitioners, and incorporation of traditional knowledge systems throughout the process. Applicants should consider including the interests of tribal nations and Indigenous peoples within targeted exploration areas and engaging these communities in a meaningful way.

OER is soliciting proposals focused on any one of the following three themes:

1. OCEAN EXPLORATION: Exploration of the biological, chemical, and physical ocean environments and areas to inform future characterization, research, and responsible ocean stewardship in unknown or poorly explored U.S. deepwater areas (see the definition of ocean exploration in the national strategy). Areas proposed for exploration must be at water depths of 200 m or more. OER is particularly interested in themes and/or geographic priorities identified by the COL Pacific workshop report, including proposals on deep-ocean acoustics, the water column, seafloor habitat, biology, and marine resources. The use of autonomous and other innovative technologies is an OER priority.
2. MARINE ARCHAEOLOGY. Exploration and discovery of underwater cultural heritage sites and objects to enrich U.S. maritime history and inform decisions concerning site, feature, or object preservation and potential seafloor use. Marine archaeology projects can be conducted in any water depth. OER is particularly interested in proposals focused on themes and/or geographic priorities identified by the COL Pacific workshop report, including submerged evidence of early human migration and occupation on the continental shelf and places significant to U.S. history. The use of autonomous and other innovative technologies is an OER priority.

3. TECHNOLOGY. Application of new or novel use of existing ocean technologies or innovative methods that could increase the scope and efficiency of acquiring ocean exploration data and expanding exploration data availability and use. Proposed ocean technologies must be applicable to water depths of 200 m or greater, preferably full-ocean depth (testing in shallower water or lab-based testing is acceptable). OER is particularly interested in proposals focused on innovative sensors and technologies that could increase the capabilities of autonomous seagoing systems and artificial intelligence (AI) and machine learning (ML) applications that could improve ocean exploration data usability and accessibility. Consult the NOAA Artificial Intelligence Strategic Plan for information on NOAA defined AI/ML.

The deadline for the pre-proposal submission is June 21, 2021 at 11:59 p.m. EDT. The full proposal is due on October 8, 2021.

Please see the attached document for the notice of funding opportunity published on May 17, 2021. The notice is also on the NOAA Ocean Exploration website.

A webinar about the funding opportunity will be held on May 26, 2021, at 1 p.m. EDT. Registration is required. A recording of the webinar will be posted on the Federal Funding Opportunity web page on the NOAA Ocean Exploration website after the event. Additional questions may be directed to oer.ffo2022@noaa.gov.

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Easing Sharing of Glider Data

The OOI’s Coastal and Global Array teams regularly use Teledyne-Webb Slocum Gliders to collect ocean observations within and around the array moorings. The gliders fly up and down the water column from the surface down to a maximum depth of 1000 meters, collecting data such as dissolved oxygen concentrations, temperature, salinity, and other physical parameters to measure ocean conditions.

OOI shares its glider data with the Integrated Ocean Observing System (IOOS) Glider Data Assembly Center (DAC). IOOS serves as a national repository for glider data sets, serving as a centralized location for wide distribution and use. It allows researchers to access and analyze glider data sets using common tools regardless of the glider type or organization that deployed the glider.

OOI serves data to these repositories in two ways.  When the gliders are in the water, data are telemetered, providing near real-time data to these platforms.  Once the gliders are recovered, data are downloaded, metadata provided, and data are resubmitted to the Glider DAC as a permanent record.

The behind-the-scene process transmitting this huge amount of data is quite complex. OOI Data Team members, Collin Dobson of the Coastal and Global Scale Nodes at Woods Hole Oceanographic Institution (WHOI) and Stuart Pearce of the Coastal Endurance Array at Oregon State University (OSU) teamed up to streamline the process and catch up on a backlog of submission of recovered data.

Pearce took the lead in getting the OOI data into the DAC. In 2018, he began writing code for a system to transmit near real-time and recovered data. Once the scripts (processing code) were operational by about mid-2019, Pearce implemented them to streamline the flow of Endurance Array glider data into the DAC. Dobson then adopted the code and applied it to the transmission of glider data from the Pioneer, Station Papa, and Irminger Sea Arrays into the repository.

As it turned out, timing was optimum. “ I finished my code at the same time that the Glider DAC allowed higher resolution recovered datasets to be uploaded,” said Pearce. “So I was able to adjust my code to accommodate the upload of any scientific variable as long as it had a CF compliant standard name to go with it.”  This opened up a whole range of data that could be transmitted in a consistent fashion to the DAC. CF refers to the “Climate and Forecast” metadata conventions that provide community accepted guidance for metadata variables and sets standards for designating time ranges and locations of data collection.  Dobson gave an example of the name convention for density:  Sea_water_density.

“Being CF compliant ensures your data have the required metadata and makes the data so much more usable across the board,” added Dobson.  “If I wanted to include oxygen as a variable, for example, I have to make sure to use the CF standard name for dissolved oxygen and report the results in CF standard units.”

The Endurance Array team was the first group to add any of the non-CTD variables into the Glider DAC. This important step forward was recognized by the glider community, and was announced at a May 2019 workshop at Rutgers with 150 conveyors of glider data in attendance.  One of Pearce’s gliders was used as the example of how and what could be achieved with the new code.

To help expedite the transfer of all gliders into the DAC, Pearce made his code open access. The additional metadata will help advance the work of storm forecasters, researchers, and others interested in improving understanding ocean processes.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

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Data Explorer v1.1. Launches

Since its inaugural launch in October 2020, OOI has been working with users of Data Explorer to learn what features worked for them, which could be improved, and what could be added to optimize users’ experiences.  This input has been put into practice and is now available for further testing on Data Explorer v1.1.

Improvements made to this version include the addition of five new instrument data types: Wire-following, Surface-piercing, Cabled Deep and Shallow Profilers, and Cabled Single Point Velocity Meters. Changes were made to improve the display and use of ERDDAP data.  Now it is possible to print custom configuration of time-series and data comparison charts.

A global search capability was added to allow users to use search terms to discover data sets in the Data Explorer. The search and navigation functions were tweaked to also find the data sets across all instruments and times.  Other behind-the-scenes fixes were implemented to improve the site’s overall operability and functionality for users. The release notes can be viewed here.

“This version of Data Explorer incorporates suggestions from its growing community of users.  We’re pleased to have received feedback that is serving to make Data Explorer a tool that meets users’ needs, which is our ultimate goal.” said Jeffrey Glatstein, OOI Data Delivery Lead and Senior Manager of Cyberinfrastructure.

A preview of the new features of Data Explorer v1.1 was held on 9 April 2021 and can be viewed below

[embed]https://youtu.be/WhXgQ5qe78E[/embed]

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OOI Pioneer Array to Relocate to MAB

It’s official, the next location of the OOI (Ocean Observatories Initiative) Coastal Pioneer Array is the Mid-Atlantic Bight (MAB) and the move will take place in 2024.  The geographic footprint championed during the NSF-sponsored Innovations Lab #1 is the region of the MAB between Cape Hatteras and Norfolk Canyon. This region offers opportunities to collect data on a wide variety of cross-disciplinary science topics including cross-shelf exchange, land-sea interactions associated with large estuarine systems, a highly productive ecosystem with major fisheries, and carbon cycle processes. This location also offers opportunities to improve our understanding of hurricane development, tracking and prediction, and offshore wind partnerships.

As background, the OOI has been in full operations since 2016. The OOI Pioneer Array was designed to be relocatable, and in 2020 the Ocean Observatories Initiative Facilities Board (OOIFB) and the National Science Foundation (NSF) launched a process to select the next OOI Pioneer Array location. A Phase 1 Innovations Lab was held in March 2021 to explore possible locations based on scientific questions of interest. The inputs received helped NSF make its decision to select the MAB.

A second (Phase 2) Innovations Lab is scheduled for the week of June 21-25.  During this Lab, participants will work to further identify and refine the opportunities afforded by the new Pioneer Array location. Selected participants will be exploring how the Pioneer Array sensors and platforms can be optimized to achieve science and education goals at the new site, based on environmental, logistical, and infrastructural considerations. Partnership and collaboration potentials at the new location will also be discussed.  The OOIFB, in partnership with Know Innovations, will again be facilitating the second Innovation Lab.

There is also an open to all Microlab scheduled for May 12th  if you are intrigued and want to learn more: (https://ooifb.org/meetings/pioneer-array-phase2/).

The ocean community is invited to help identify new design considerations that can enable exciting research endeavors at the chosen location.  Scientists, educators, and other stakeholders are encouraged to apply for the Phase 2 Innovations Lab. Please visit the OOIFB  website for more information.

 

 

 

 

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Expanding Reach of OOI Data

[caption id="attachment_21045" align="alignnone" width="640"] Pioneer Array data is now available on NERACOOS’ new Mariner’s Dashboard. This is but one example of how OOI data are integrated into other data repositories to maximize their benefit and use.[/caption]

OOI shares data with partner repositories and institutions that host similar data but have different user bases. These partnerships expand the data available for forecasting models, help provide insight into current ocean conditions, and serve as important resources for many ranging from fishers and other maritime users to land-based researchers and students.

With the exception of the Station Papa Array, the OOI Coastal and Global Arrays maintain surface buoys. Instruments deployed on these buoys measure meteorological variables such as air temperature, barometric pressure, northward and eastward wind velocities, precipitation, solar radiation, and surface water properties of sea surface temperature and salinity. Other instruments on the moorings collect wave data, such as significant wave height, period, and direction. These data are then consumed by national and regional networks to improve accuracy of weather forecasting models.

The Regional Cabled Array (RCA) consists of fiber-optic cables off the Oregon coast that provide power, bandwidth, and communication to seafloor instrumentation and moorings with instrumented profiling capabilities. A diverse array of geophysical, chemical, and biological sensors, a high-definition camera, and digital still cameras on the seafloor and mooring platforms, provide real-time information on processes operating on and below the seafloor and throughout the water column, including recording of seafloor eruptions, methane plume emissions and climate change. These data are available for community use. Since 2015, the RCA has fed data into Incorporated Research Institutions for Seismology (IRIS), the primary source for data related to earthquakes and other seismic activity. In addition, data including zooplankton sonar data, are being utilized within the Pangeo ecosystem for community visualization and access and pressure data are incorporated into NOAA’s operational tsunami forecasting system.

Helping Improve Models and Forecasting

One of the recipients of OOI data is the National Data Buoy Center (NDBC), part of the National Oceanic and Atmospheric Administration’s (NOAA) National Weather Service. NDBC maintains a data repository and website, offering a range of standardized real-time and near real-time meteorological data. Data such as wind speed and direction, air and surface water temperature, and wave height and direction are made available to the broader oceanographic and meteorological community.

“Many researchers go to NDBC for their data, “said Craig Risien, a research associate with OOI’s Endurance Array and Cyberinfrastructure Teams, who helps researchers gain access to and use OOI data. “NBDC is a huge repository of data and it’s easy to access. So there’s a low barrier for researchers and students who are looking for information about wind speed, water temperature and a slew of other data. OOI contributing to this national repository significantly increases its data reach, allowing OOI data to be used by as many people as possible. “

OOI sea surface temperature data also make their way into the operational Global Real-Time Ocean Forecast System (RTOFS) at the National Centers for Environmental Prediction (NCEP), another part of NOAA’s National Weather Service. RTOFS ingests sea surface temperature and salinity data from all available buoys into the Global Telecommunications System (GTS). OOI glider data also are pushed in near real-time to the US Integrated Ocean Observing System Glider Data Assembly Center (DAC). From there, the data goes to the GTS where it can be used by the operational modeling centers such as NCEP and the European Centre for Medium-Range Weather Forecasts.

The GTS is like a giant vacuum sucking up near real-time observations from all sorts of different platforms deployed all over the world. On a typical day, the GTS ingests more than 7,600 data points from fixed buoys alone. As a result of this vast input, researchers can go to the GTS, pull available data, and assimilate that information into any model to improve its prediction accuracy.

Advancing Forecasting of Submarine Eruptions

As the first U.S. ocean observatory to span a tectonic plate, RCA’s data are an invaluable contributor to IRIS’s collection. Since 2015, the user community has downloaded >20 Terabytes of RCA seismometer data from the IRIS repository. Fourteen different sampling locations include key sites at Axial Seamount on the Juan de Fuca mid-ocean ridge spreading center, near the toe of the Cascadia Margin and Southern Hydrate Ridge. RCA data are catalogued and available on the IRIS site, using the identifier “OO.”

[caption id="attachment_21046" align="alignleft" width="300"] Data from short period seismometers installed at RCA’s Axial Seamount and Southern Hydrate Ridge sites are streamed live to IRIS. Credit: UW/NSF-OOI/Canadian Scientific Submersible Facility, V13.[/caption]

“RCA is a critical community resource for seismic data. Axial Seamount, for example, which erupted in 1998, April 2011, was the site of more than 8,000 earthquakes over a 24-hour period April 24, 2015 marking the start of large eruption,” explained Deb Kelley, PI of the RCA. “Being able to witness and measure seismic activity in real time is providing scientists with invaluable insights into eruption process, which along with co-registered pressure measurements is making forecasting possible of when the next eruption may occur. We are pleased to share data from this volcanically and hydrothermally active seamount so researchers the world over can use it to better understand processes happening at mid ocean ridges and advance forecasting capabilities for the first time of when a submarine eruption may occur.”

Providing Data with Regional Implications

[caption id="attachment_21047" align="alignright" width="203"] Data from Endurance Array buoy 46100 are fed into WCOFS, where they are accessible to maritime users. Credit: OSU[/caption]

OOI also provides data to regional ocean observing partners. Data from two Endurance Array buoys (46099 and 46100), for example, are fed into a four-dimensional U.S. West Coast Operational Forecast System (WCOFS), which serves the maritime user  community.  WCOFS generates water level, current, temperature and salinity nowcast and forecast fields four times per day. The Coastal Pioneer Array is within the future Northeastern Coast Operational Forecast System (NECOFS).  Once operational, Pioneer’s observations will potentially be used for WCOFS data assimilation scenario experiments.

Coastal Endurance Array data are shared with the Northwest Association of Networked Ocean Observing Systems (NANOOS), which is part of IOOS, and the Global Ocean Acidification Observing Network (GOA-ON). Endurance data are ingested by the NANOOS Visualization System, which provides easy access to observations, forecasts, and data visualizations.  Likewise, for GOA-ON, the Endurance Array provides observations useful for measuring ocean acidification.

Data from three of the Pioneer Array buoys also are part of the Mariners’ Dashboard, a new ocean information interface at the Northeastern Regional Association of Coastal Ocean Observing Systems (NERACOOS). Visitors can use the Dashboard to explore the latest conditions and forecasts from the Pioneer Inshore (44075), Central (44076), and Offshore (44077) mooring platforms, in addition to 30+ other observing platforms throughout the Northeast.

“We are working hard to distribute the OOI data widely through engagement with multiple partners, which together are helping inform science, improve weather and climate forecasts, and increase understanding of the ocean,” added Al Plueddemann, PI of the Coastal and Global Scale Nodes, which include the Pioneer, Station Papa, and Irminger Sea Arrays.

 

 

 

 

 

 

 

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Call for Applications: OOIFB Data Systems Committee

 

Application Deadline: May 20, 2021

The Data Systems Committee (DSC) of the NSF Ocean Observatories Initiative Facility Board (OOIFB) was established to help ensure timely and reliable access to high-quality Ocean Observatories Initiative (OOI) data. The Committee evaluates and recommends improvements to the data services policies and practices of the OOI Facility that will lead to more efficient and effective scientific use of OOI data.

The DSC is now soliciting applications to fill one open position. The appointment will fill the remainder of an unexpired term and will be effective starting in May 2021 and run through September 2023. The selected individual will be eligible to serve a second term of 3-years.  The DSC holds at least one in-person meeting per year and one web conference each month.

Some of the objectives of the committee include:

  • Keeping abreast of the current state of the OOI cyberinfrastructure and data services with the goal of helping to promote maximum scientific use of OOI data. These efforts will be informed by the FAIR Guiding Principles for scientific data management and stewardship, such that data are: a) Findable, b) Accessible, c) Interoperable, and d) Reusable.
  • Encouraging the use of best practices, standards, and naming conventions established by the oceanographic community.
  • Engaging with the user community to gauge user needs in regard to OOI data systems, and to facilitate the promotion of a positive user experience.
  • Staying current on potential new modes of data service and access, data analysis methodologies, and related technologies that facilitate the use of OOI data.
  • Engaging with the OOI Program team regarding the priorities and plans of the OOI cyberinfrastructure groups.
  • Making recommendations for data products, usage metrics, and improving the user experience on the OOI Data Explorer, as well as other data service systems employed by the OOI.

Scientists with experience using scientific observing systems such as OOI, as well as those with experience in successfully delivering data from large-scale multi-sensor observing systems to scientific users are encouraged to apply. Applications should be submitted to Annette DeSilva, at the OOIFB Administrative Support Office (desilva@ooifb.org), and must include a letter of interest and an academic CV.

Applications are due by May 20, 2021. Applications will be reviewed by the DSC members who will give due consideration to the qualifications of applicants, as well as to maintenance of career level, disciplinary, and regional balance on the Committee. For more information about the DSC and its activities, please visit the OOIFB website or contact Tim Crone, DSC Chair (tjcrone@gmail.com).

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Sweet 16: Pioneer Array Successfully Turned

Twenty days at sea. Forty different at-sea operations.  Nine moorings recovered. Eight moorings, two coastal profiling gliders and two global test gliders deployed. Completion of more than 25 objectives during the 16th turn of the Coastal Pioneer Array.

By all counts, the Pioneer Array 16 expedition was a huge success. The scientific team was able to accomplish a full mooring service cruise in spite of COVID-imposed restrictions that restricted building occupancy for pre-cruise preparation, limited personnel onboard to accomplish the work and imposed a two-week quarantine period prior to boarding the ship.

“It’s always takes a focused effort from many people for a successful cruise, but COVID has made it harder.” said Al Plueddemann, chief scientist for Pioneer Array and principal investigator for the Ocean Observatory Initiative’s (OOI) Coastal and Global Scale Nodes. “The OOI team, the captain and crew of the Armstrong, and the shore-side support all put in a great effort to see this through to completion, while still operating at reduced efficiency under ongoing COVID-19 restrictions.”

A variety of atmospheric and oceanographic measurements are made prior to deployments and following recoveries for validation of mooring, glider, and AUV (autonomous underwater vehicle) observations. The team also conducted cross-shelf and along-shelf CTD surveys and collected water samples adjacent to all the moorings. The team also surveyed the array’s region using shipboard sensors (ADCP, EK-80, and thermosalinograph).

In addition to the successful mooring operations, the Pioneer 16 team completed several mobile platform objectives as well.  For the spring and summer time period, two coastal profiling gliders were deployed to replace winter profiler moorings.  Two global test gliders were also put through their paces to ensure safe operation and reliable data delivery prior to operations at a global array. Two AUVs were launched and traveled pre-determined paths around the array before being recovered and having their data downloaded.  While the team was following the AUVs to ensure the missions were progressing as planned, they encountered a pod of about 40 pilot whales that included both young and adult whales. The team and the pod of whales were equally fascinated by each other. Both groups stopped to observe the other’s behaviors.

[caption id="attachment_20931" align="alignleft" width="300"] Photo: Rebecca Travis©WHOI.[/caption]

“The data we collect are helping scientists better understand the ocean environment and how it is changing.  Seeing the pilot whales reminded us of the importance of these observations, and the research they enable, to the marine ecosystem.” added Plueddemann.

 

 

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