News
Pioneer Array Design: Building on the known to explore the unknown
The location of the Ocean Observatories Initiative Pioneer Array has been ideal for understanding recent, unprecedented changes in temperature and ocean properties on the continental shelf and slope off the coast of New England, coincident with an increase in warm core rings at a time when the Gulf Stream has grown increasingly unstable. That’s the conclusion of a review paper published last month in the Journal of Operational Oceanography.
The paper, written by Glen Gawarkiewicz and Al Plueddemann of Woods Hole Oceanographic Institution, details how the components and location of the array were determined and how the data gathered there has changed scientific questions being asked in this critical region. The array also provides a unique observatory model that can be applied in other shelf break regions across the world.
“We already knew a fair bit about what was happening in the region, but what we’re seeing now isn’t what we expected,” said Plueddemann. “Fortunately, the array was designed and constructed in such a way that we were ready for just about anything.”
The shelf break front stretches along the U.S. Northeast Coast from Georges Bank to Cape Hatteras, dividing cooler, fresher waters of the coast and continental shelf from warm, saltier waters of the slope. It is a complex, productive, and constantly changing area, driven by the interaction of winds, currents, and offshore rings.
Prior to the Pioneer Array, data from the shelf break came primarily from stationary moored instruments or from short-term, mobile observations provided by ocean gliders and towed shipboard systems. In designing the Pioneer Array, scientists and engineers working with the NSF-funded Ocean Observatories Initiative integrated moorings, gliders and propeller-driven AUVs to provide a long-term, multi-dimensional data set that blends the advantages of multiple observing technologies. This is particularly important as ocean processes occurring at the shelf break occur on a variety of space and time scales.
Gawarkiewicz and Plueddemann point out that in addition to enabling new scientific discovery, data from the Pioneer Array has the potential for real-time applications to help track and forecast hurricanes and winter storms, improve search-and-rescue operations, and the siting and operation of off-shore wind installations.
Since becoming operational in 2016, the Pioneer Array has gathered near-continuous data across a 24,000 square-kilometer swath of the shelf break region. By combining moorings, gliders, and AUVs, the array has provided the scientific community with high-resolution observations across space and time, which are unprecedented in their scope and detail and are also freely available on the Ocean Observatories Initiative data portal.
“We haven’t even scratched the surface yet,” said Plueddemann. “There’s still lots of potential to mine in the Pioneer Array data.”
The Ocean Observatories Initiative (OOI) is a long-term infrastructure project funded by the National Science Foundation to gather physical, chemical, and biological data from the ocean, atmosphere, and seafloor and to deliver that data on demand and in near real-time online. The program includes fixed instruments and autonomous underwater vehicles deployed at key locations off in U.S. coastal waters and in the open ocean. The OOI currently maintains arrays off the Northeast and Northwest coasts of the U.S., the Irminger Sea southeast of Greenland, and at Station Papa in the Gulf of Alaska, as well as a seafloor cabled array off the coast of Oregon. Data from the arrays help researchers address questions ranging from rapidly changing weather events to long-term climate change and from air-sea interaction to sea floor processes. OOI is managed by the Woods Hole Oceanographic Institution (WHOI) and implemented by WHOI, the University of Washington, Oregon State University, and Rutgers, the State University of New Jersey.
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ANNOUNCEMENT – OOI Facilities Board Town Hall at AGU – Call for Lightning Talks
ANNOUNCEMENT – OOI Facilities Board Town Hall at AGU – Call for Lightning Talks
The Ocean Observatories Initiative Facilities Board (OOIFB) will host a Town Hall at the 2019 Fall AGU meeting in San Francisco, CA. The Town Hall is scheduled for Monday, December 9th from 6:15 pm to 7:15 pm at Moscone West, Room 2007, L2. The community will have the opportunity to hear the latest information about the OOI facility, meet the OOIFB members, and learn about research using OOI data.
The Town Hall will include a series of lightning presentations where scientists are invited to present one slide in one minute explaining how s/he has used (or plans to use) freely available observatory data in their respective research. In this Town Hall we will expand beyond OOI, and encourage users of other observatories to also share their experiences in applying observatory data in their respective research. We hope you will consider presenting a slide in the lightning session.
Sign-up now to present a lightning talk – If you are using observatory data (OOI, NCAR, NEON, etc.) and wish to present a lightning talk during the Town Hall, please sign up at <https://forms.gle/VxiHDQvEq6Se5uxi8> by December 1st.
The Town Hall is aimed at researchers who are now using or are considering using OOI data, researchers interested in adding instrumentation to the OOI infrastructure, and educators at all levels interested in the OOI. Thank you and we hope to see you at the OOIFB Town Hall!
Event: OOI Facility Board Town Hall
When: Monday, December 9th from 6:15 pm to 7:15 pm
Where: Moscone West, Room 2007, L2 – San Francisco, CA
Read MoreOOI achieves milestone with Irminger Sea deployment
The recently completed OOI mooring service cruise on the R/V Neil Armstrong (2-25 Aug 2019) established a significant milestone – the Irminger Sea Global Surface Mooring was sustained for over a year and returned high quality data. To our knowledge, this is the first surface mooring with instrumentation to compute bulk air-sea fluxes of heat, moisture and momentum that has operated through a full annual cycle in this region.
It is now recognized (e.g. de Jong and de Steur, 2016, Geophys. Res. Lett., 43, 7106–7113, DOI: 10.1002/2016GL069596) that extreme heat loss in the Irminger Sea results in deep water formation, which ultimately influences the strength of the Atlantic Meriodonal Overturning Circulation and has important climate implications. The strong heat loss in the region is largely driven by episodic cold-air outbreaks from the southern tip of Greenland (Josey et al., 2019, Geophys. Res. Lett., 46. DOI: 10.1029/2018GL080956).
[media-caption type="image" path="https://oceanobservatories.org/wp-content/uploads/2019/09/Winds1-300x212.jpg" link="#"]Fig. 2. Satellite scatterometer winds (QuikSCAT) during a cold-air outbreak (right; from Vage et al., 2008))[/media-caption]Cold-air outbreaks are associated with high winds, sub-freezing temperatures, and large, steep waves (Vage et al., 2008, J. Phys. Oceanogr., 38(3), DOI: 10.1175/2007JPO3678.1), which create very difficult conditions for sustained observations at the air-sea interface. The situation is further complicated by the occasional passage of icebergs, which could impact the buoy. The lack of continuous time series data through the winter season capable of identifying episodic events has hindered understanding of air-sea interaction in the Irminger Sea.
The biggest risks to sustained operation of the OOI Irminger Sea mooring were determined to be icing on the buoy tower & freezing of sensitive instrument components. Icing could not be controlled, but potential impacts could be mitigated, for example by shutting down the wind turbines to reduce the likelihood of broken blades. However, a turbine shut-down also meant reduced power generation. Freezing of the precipitation sensor was controllable using a built-in heater, but at the cost of additional power.
[media-caption type="image" path="https://oceanobservatories.org/wp-content/uploads/2019/09/Buoy-300x169.jpg" link="#"]Fig. 3a. Buoy cam pictures showing tower icing.[/media-caption]The CGSN operations team took on the challenge by monitoring weather forecasts for conditions conducive to icing, adding cameras to the buoy tower to detect icing, and implementing a power management strategy during storms. When icing conditions were forecast, the wind turbines were shut down to reduce the likelihood of damage, while some mooring components were simultaneously shut down to save power. Power to high priority instruments (including the bulk meteorology system) and the precipitation sensor heaters was maintained. The strategy was effective, but the difficulty of sustained observations was still evident: The direct-covariance flux package was damaged upon deployment and did not return useful data. The buoy sustained damage to the wind vane, a solar panel and a wind turbine during the winter storms. This compromised power generation capability eventually led to an eight-day data gap in June 2019 due to sustained low wind and overcast skies.
[media-caption type="image" path="https://oceanobservatories.org/wp-content/uploads/2019/09/Winds-2-300x225.png" link="#"]Fig. 4. Time series of METBK meteorological parameters spanning the full deployment period. Left panel: Air (red) and sea surface (blue) temperature, relative humidity and barometric pressure. Right panel: East (red) and north (blue) wind, shortwave (red) and longwave radiation, and precipitation.[/media-caption] [media type="image" path="https://oceanobservatories.org/wp-content/uploads/2019/09/Winds-3-300x225.png" link="#"][/media]Despite the challenges, the buoy bulk meteorology system operated for 420 days of the 428-day deployment (8 June 2018 – 9 Aug 2019) and returned a wealth of scientific data. One-minute records from the bulk meteorology sensors show wind speeds up to 25 m/s and air temperatures as low as -5 C associated with cold -air outbreaks that likely dominate the cumulative wintertime heat loss, as described by Josey et al. (2019). The availability of the first annual cycle of surface meteorology, in conjunction with subsurface data from the OOI Irminger Sea array and the Overturning in the Subpolar North Atlantic Program (OSNAP) array, provide the potential for new insights into the nature of deep mixing, carbon sequestration and deep-water formation in the region.
[media-caption type="image" path="https://oceanobservatories.org/wp-content/uploads/2019/09/team-640x360.jpg" link="#"]Fig. 5. Photo of the Irminger-5 buoy about to be recovered from the R/V/ Armstrong in August 2019. A close look shows damage to the wind turbine and solar panel on the left side.[/media-caption] Read MoreRegional Cabled Array 2019 Expedition Sets Records
This summer’s Regional Cabled Array (RCA) 44-day expedition (May 30-July 12, 2019) onboard the R/V Atlantis was highly successful with the completion of all tasks scheduled for this annual maintenance and operations cruise. One hundred forty-nine out of 151 RCA Core and PI instruments are operational, all three instrumented Deep Profiler vehicles and instrumented Science Pods on the Shallow Profiler Moorings are conducting daily traverses through the water column, and 113 RCA instruments were installed. It was wonderful to once again see the beautiful life inhabiting the hydrothermal vents at Axial Seamount, amazing aggregations of cod curious about our work at the Oregon Offshore site, and to witness the profound changes that have taken place again at the methane seeps at Southern Hydrate Ridge.
During the 53 days of staging and demobing for the cruise over the four legs 166 tons of RCA equipment were transported to/from Seattle, WA and Newport, OR. Onboard staffing included 52 personnel with 13 students, six non-OOI PI’s-technicians from four institutions and one member from industry. In addition, Susan Casey, a New York Times bestselling author (i.e. The WAVE, the Devils Teeth, and Voices of the Ocean) participated on Leg 4. As part of the NSF Oceans Month, a 1-hour “Science in the Deep” Facebook live interactive broadcast was conducted, including live streaming of imagery from Jason working at Southern Hydrate Ridge and a period for questions and answers. There were 58 Jason Dives, with a record setting 20 dives in five days including deep dives to 2600 m and 2900 m water depths. The vehicle worked extremely well with turn-arounds commonly less than one hour.
Another big success for this summer occurred during nine days of at-sea operations dedicated to turning and installation of cabled and uncabled instrumentation and field work provided to externally-funded researchers. This work included the:
- Installation of an NSF-funded new high resolution, self-calibrating pressures sensor at Central Caldera, Axial Seamount (W. Wilcock, University of Washington).
- The recovery, repair and reinstallation of the NSF-funded COVIS multibeam sonar for hydrothermal plume imaging at the ASHES hydrothermal field, as well as installation of a thermistor array (K. Bemis, Rutgers University); Bemis also conducted a several hour thermal and video survey of the field.
- The turning of an NSF-funded CTD at the ASHES hydrothermal field, Axial Seamount (W. Chadwick, Oregon State University). Note Chadwick received a new NSF award to expand the CTD network to monitor the release of subsurface brines associated with eruptions at Axial as observed during the 2015 eruption (see Xu et al., 2018).
- The recovery of an ONR-funded uncabled Benthic Observatory Platform (BOP) from the Oregon Offshore site and installation of another BOP at a seep site at Southern Hydrate Ridge (C. Reimers-Oregon State University and P. Girguis-Harvard University) and associated sediment sampling; and
- The recovery, repair, and reinstallation of a University of Bremen-Germany-funded cabled overview multibeam sonar for imaging of all methane plumes at Southern Hydrate Ridge (G. Bohrmann and Y. Marcon -University of Bremen) – the range of this sonar is now extended from 200 m to 700 m. A new 4K video-still camera was also installed near Einsteins’ Grotto.
The RCA engineering and science team is enjoying being on land after conducting round the clock operations to insure that the facility work was completed on schedule. Folks are enjoying the Seattle sun and the Cascades and Olympic mountains during the summer blue-skied days. Soon however, our thoughts, will be turning to refurbishment and planning for next years cruise. The team is looking forward to working with the VISIONS19 students on their projects this upcoming academic year; we are excited to see the stories they tell with new eyes focusing on the oceans, the RCA, and OOI.
Read MoreOOI moorings provide sustained observations of the Irminger Sea Deep Western Boundary Current
Data from the Ocean Observatories Initiative (OOI) Global Irminger Sea Array contributed to the longest continuous record of total volume transport of water in the Deep Western Boundary Current. This current, in the subpolar North Atlantic, travels southwest along the continental slope off of Greenland and is considered a significant part of the global climate system.
In a recent Journal of Geophysical Research Letters: Oceans paper, Dr. Joanne Hopkins at the National Oceanography Center in Southampton, U.K., and collaborators used data from two U.S. OOI flanking moorings, along with three U.S. Overturning in the Subpolar North Atlantic Program (OSNAP) East Greenland Current array moorings, and five U.K. OSNAP moorings to study the total amount of water moved by the current over a period of two years, as well as its daily and seasonal variability.
The data used for this paper was gathered over 22 months between 2014 and 2016, while all 10 of the moorings were in the water for the same period. Previous research to determine transport estimates at this latitude have been limited by a sparse number of direct and sustained measurements, relying instead on measurements over 9.5 months, 60 days, and “snapshot” or repeated summertime hydrographic sections.
Hopkins et al estimate that the Deep Western Boundary Current transports an average of 10.8 × 106 m3 of water per second with variation in time. In addition, the transport variability shifts from high to low frequencies with distance down slope. While the results did suggest an increase in transport since 2005-2006, they did not conclude that there was a significant long-term trend, given the limitations of previous data sets.
The location of the OOI Global Irminger Sea array was selected as part of an effort by the scientific community to place moorings in areas that have been historically under-sampled and subject to high winds and sea states that make frequent ship-based measurements difficult. The OOI Data Portal provides access to data from the Irminger Sea Array dating back to the initial installation in September 2014.
Read MoreNSF Science in the Deep with ROV Jason
NOTE: Video of this event available here. Fast forward to about 52:00 to get past the distorted audio.
The National Science Foundation will host “Science in the Deep,” a Facebook Live event with researchers aboard R/V Atlantis on Wednesday, June 26, from 1:00-2:00 p.m. Eastern. The Atlantis team will be off the coast of Oregon servicing parts of the Ocean Observatories Initiative Regional Cabled Array using the remotely operated vehicle (ROV) Jason, which is expected to be 800 meters deep at Southern Hydrate Ridge, where methane bubbles from the seafloor and life flourishes.
Join NSF host Deena Headley as she speaks with OOI Research Scientist Michael Vardaro and Research Scientist/Eng2 Katie Bigham, both from the University of Washington, about their work on the recent cruises off the U.S. Northwest Coast, live views from Jason on the seafloor, and life at sea.
Read MoreStreaming Live From the Deep: The 2019 OOI Regional Cabled Array expedition
This summer’s exciting sea-going expedition in the Northeast Pacific to maintain the National Science Foundation’s Ocean Observatories Initiative Regional Cabled Observatory is underway, and you can join us at InteractiveOceans.
Over the next several weeks, the University of Washington Cabled Array team will be adding novel sensors that allow a global audience to watch live the daily deformation and seismic activity at the largest underwater volcano off our coast, Axial Seamount. Axial erupted in 2015 and is poised to do so again. In addition, we will be adding new instruments, including a 4K video camera aimed at a highly dynamic methane seep site off Newport, Oregon, called Southern Hydrate Ridge, where streams of bubbles issue from the seafloor daily.
[media-caption type="image" path="https://oceanobservatories.org/wp-content/uploads/2019/06/AtlantisBackdeck_1_small-1080.jpg" link="#"]R/V Atlantis steams back to shore after Leg 1 of the 2019 Regional Cabled Array cruise, following the successful installation of the Shallow Profiler Mooring at Axial Base. Photo by J. Tilley, University of Washington[/media-caption]The cruise, which departed June 2 and continues until July 12, is using the remotely operated vehicle (ROV) Jason onboard the R/V Atlantis operated by Woods Hole Oceanographic Institution. Nineteen U.S. and international undergraduate students are working side-by-side scientists, engineers, ROV team, and ship’s crew on the expedition as part of the UW experiential at-sea VISIONS program.
This expedition is highly complex with a diverse array of more than100 instruments, junction boxes, and instrumented pods on the Shallow Profiler Moorings that will be recovered, installed, and tested. R/V Atlantis will be “packed to the gills” on each of the four legs that make up this expedition, carrying everything from state-of-the-art mooring components to sharpies.
Starting around June 12 or 13, you will be able to watch our underwater operations live through streaming video as ROV Jason works more than 300 miles offshore and 5,000 feet below the surface down at the summit of Axial Seamount, which hosts 350°C (660°F) deep-sea hot springs that support some of the most bizarre creatures on Earth. We will also be 250 miles off Newport in depths ranging from 250 feet to 10,000 feet in some of the most biologically productive waters in the world and at sedimented sites on the Cascadia margin where methane-rich plumes jet from the seafloor. There, methane seeps support dense bacterial mats and large clams that thrive in the absence of sunlight on gases pouring from the seafloor.
A 4K camera funded by the University of Bremen will provide real-time views of the methane plumes and seafloor life to document this incredibly dynamic environment marked by large explosion pits and collapse basins. This is the second year of this international collaboration that expands the capability of the Regional Cabled Array and provides new imagery of these dynamic systems for all to see.
An enhanced, high-bandwidth satellite connection from R/V Atlantis will allow you to experience our deep-sea operations through daily live video streams. It will also allow onboard engineers and scientists to see data for the first time as new instruments are connected to the seafloor submarine fiber optic cables that bring the global Internet into the oceans. So tune in and see what we see when we see it.
Read MoreOpportunity to provide feedback on OOI Data Delivery Systems
We need your help evaluating Ocean Observatories Initiative (OOI) data delivery systems and to assess the extent to which they meet the needs of the user community. The information we gather through this survey will be used to improve the current OOI data delivery systems and perhaps develop other systems that better meet the needs of users. We want to know what you think of the OOI data delivery systems and how they could be improved for users.
The survey should only take about 15 minutes to complete. Your participation is voluntary and your responses are anonymous. Click here for the OOI Data survey
Please complete the survey by April 26th. This survey is being conducted by the NSF’s OOI Facility Board’s Data Dissemination and Cyber Infrastructure (DDCI) Committee. If you have any questions, please contact Tim Crone.
Thank you very much for your time and feedback.
Regards,
Tim Crone, DDCI Committee Chair & Larry Atkinson, OOIFB Chair
Endurance Array Fall 2018 cruise data available through OOI Data Portal
Endurance Array Fall 2018 cruise data available through OOI Data Portal
[media-caption type="image" path="https://oceanobservatories.org/wp-content/uploads/2019/01/IMG_1853.jpg" link="#"]The shelf and offshore Washington buoys on the back deck of the R/V Sally Ride. Photo Credit: Zoë Philby[/media-caption]The Fall 2018 Endurance Array cruise on the R/V Sally Ride departed Seattle, Washington on September 16 and completed in Newport, Oregon on September 30. All uncabled moorings were recovered and newly refurbished moorings deployed in their place. Telemetered science data from this deployment are being ingested and are available through OOI’s Data Portal. Data from instruments deployed in spring 2018 and recovered in Fall 2018 are also available through OOI’s Data Portal. As bottle data are analyzed, they are being posted to alfresco.oceanobservatories.org. The full cruise report is available at this URL.
Read MoreA Community Welcome from The OOI 2.0 Team
A Community Welcome from The OOI 2.0 Team
The Ocean Observatories Initiative team is excited about implementation of OOI 2.0 and advancing this community facility over the next five years. Phase two of OOI began October 1, 2018 following the award by the National Science Foundation of a cooperative agreement to Woods Hole Oceanographic Institution (WHOI) to host the Program Management Office. Operations and maintenance of observatory components remains as before with WHOI operating the Global sites and the Pioneer Array, the University of Washington (UW) operating the Regional Cabled Array, Oregon State University (OSU) operating the Endurance Array, and Rutgers, the State University of New Jersey operating the cyberinfrastructure that ingests and delivers data. One important change in OOI 2.0 is that the data assessment responsibilities, formerly at Rutgers, are now distributed among the marine operating institutions to provide better integration with the science and engineering teams, as OOI 2.0 puts renewed emphasis on data QA/QC and data access.
[media-caption type="image" path="https://oceanobservatories.org/wp-content/uploads/2019/01/PioneerSurfaceMooring-300x184.jpg" link="#"]Figure 1. The Multi-Function Node of a Pioneer Surface Mooring prepared for launch on the fantail of the R/V Armstrong. Pioneer Array moorings are recovered and replaced with refurbished components twice per year. (Photo credit: OOI CGSN)[/media-caption]The Global Array infrastructure deployments at the Irminger and Papa sites are ongoing – entering their 5th and 6th year of operation, respectively. OOI operations at the Irminger Sea Array are conducted in coordination with the NSF Overturning in the Subpolar North Atlantic Program (OSNAP), while OOI subsurface moorings and gliders at Papa are deployed in coordination with a surface mooring from NOAA’s Pacific Marine Environmental Laboratory. Deployments with reduced scope, consisting of a surface mooring only, are being conducted at the Southern Ocean Array in collaboration with the National Oceanography Centre (NOC), Southampton, UK. Operations at the Argentine Basin Array have been suspended. The Pioneer Array (Figure 1), serviced twice per year, is preparing for its 12th mooring service cruise. Several community PI projects have leveraged the Pioneer Array infrastructure, including the New England Shelf Long-Term Ecological Research (LTER) program. Observations from Pioneer, in conjunction with remote sensing and historical data, have highlighted new shelf-slope exchange mechanisms within a rapidly changing physical system with significant impacts on ecosystems.
[media-caption type="image" path="https://oceanobservatories.org/wp-content/uploads/2019/01/EnduranceArray-300x169.png" link="#"]Figure 2. The September 2018 Endurance Array cruise occurred during the transition to OOI 2.0. We recovered equipment deployed in March 2018, deployed newly refurbished equipment and continued delivering data to the OOI Data Portal. (Photo credit: OOI OSU)[/media-caption]The Endurance Array (Figure 2) includes moorings, profilers and gliders off Oregon and Washington. The infrastructure off Oregon is tied into the Regional Cabled Array at the shelf and offshore locations. The full scope of the Endurance Array was first deployed in April 2015, and we are preparing for our eleventh Endurance Array cruise in April-May 2019. Significant technical improvements have been made across the array based on system performance. Among the many improvements, we have updated sensors (Satlantic ISUS sensors replaced with SUNA) and improved bio-fouling mitigation (UV biofouling protection added to dissolved oxygen optodes). Notable successes on the Endurance Array include observations of seasonal hypoxia events at multiple locations using fixed time series, profilers, and gliders. There are also moored multi-spectral optical attenuation and absorption time series from fixed depths and from profilers. While the OOI data portal is the source of all Endurance Array data, to better serve the regional user community, some Endurance Array data is passed through other widely used access points. Near real-time Endurance buoy meteorological and surface data can be accessed through NDBC. Recent near real-time Endurance Array data can also be accessed through the regional IOOS site, nanoos.org. OOI glider data is also passed on to the IOOS Glider DAC.
[media-caption type="image" path="https://oceanobservatories.org/wp-content/uploads/2019/01/RegionalCabledArray-300x200.jpg" link="#"]Figure 3. The R/V Revelle fully loaded with the Regional Cabled Array infrastructure for installation during Leg 1 of the 2018 expedition. (Photo credit: OOI UW) [/media-caption]The Regional Cabled Array (Figure 3) is now in its 5th year of operation. As part of the OOI 2.0 transition, the UW partnered with Pacific Northwest Gigapop to operate the terrestrial west coast infrastructure, which included moving the Cabled Array and CI servers to Seattle from Portland, Oregon. In addition, the UW is now responsible for the port agent drivers and data parsers for Cabled Array Core and PI instruments. The CI Machine to Machine interface is now being routinely used by the community to access Cabled Array data, and compared to samples for verification. The OOI Cabled Array Core infrastructure is enhanced by the addition of 13 “PI” instruments with funding from the NSF, the Office of Navy Research and Germany. Newly installed PI instruments include two cabled multibeam sonars that are imaging all methane plumes issuing from the seeps at Southern Hydrate Ridge as well as a CTD-O2 sensor, two new geophysical sensors, the cabled COVIS multibeam sonar, as well as three uncabled thermistor arrays. The Shallow Profiler moorings continue to be work horses for the Cabled Array, having completed >30,000 profiles since 2015. During this next ~ six months, the Cabled Array team is working hard on platform and instrument refurbishment, and integration as testing in preparation for our 2019 cruise, which begins late May onboard the R/V Atlantis.
The OOI cyberinfrastructure (CI) is a robust CI system architecture with established processes based on community best practices that allows 24/7 connectivity and ensures sustained, reliable worldwide ocean observing data any time, any place, on any computer or mobile device. Since the operations and maintenance phase of the project started in January 2016, the OOI CI system infrastructure has provided and continues providing extremely high uptime and quality of service, has served over 150 million user requests, delivered over 100TB of data to user from over 100 distinct countries across the globe. This CI architecture is being used as model by other NSF facilities.
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