Two Decades of Mooring and Ship-Based Observations from the Newport Hydrographic Line

[media-caption path="/wp-content/uploads/2022/08/Screen-Shot-2022-08-18-at-3.36.36-PM.png" link="#"](left)Time series of a) temperature b) salinity and c) meridional velocity from the Oregon shelf site.  Time series exist at this site starting in 1997.  The OOI time series begin in summer 2014 for the Regional Cabled Array and spring 2015 for the uncabled Endurance Array.  For clarity, only 2012-2022 are shown.  Prior to OOI, the site was named NH-10.  Adapted from Figures 6, 7, and 8 Risien et al. (2022)Risien et al. (2022), Making Available More Than Two Decades of Mooring and Ship-Based Observations from the Newport Hydrographic Line, OT06-01, presented at Ocean Sciences Meeting 2022, Honolulu, HI (virtual), 4 Mar.[/media-caption]

C.M. Risien, M.R. Fewings, J.L. Fisher, B.T. Cervantes, C.A. Morgan, J.A. Barth, P.M. Kosro, J.O. Peterson, W.T. Peterson, and M.D. Levine

In the Northern California Current System (NCCS), during spring and summer months, equatorward winds drive the upwelling of cold, nutrient-rich, and oxygen-poor waters from depth onto the shelf, fueling a highly productive marine ecosystem that supports valuable commercial fisheries. Oceanographic conditions in the NCCS vary on temporal scales from hours to decades. In contrast, grant-funded research typically consists of shorter-term studies (3-5 years). While such studies resolve intra-annual and perhaps inter-annual variability, they do not capture decadal scale variability that is critical for climate studies.

Risien et al. (2022), present two new decadal-scale data products. The first is ~550 gridded, cross-shelf hydrographic sections of temperature, salinity, potential density, spiciness, and dissolved oxygen from data collected biweekly to monthly from March 1997 to present along the Newport Hydrographic Line (NHL; 44.6°N, 124.1–124.65°W) off Newport, Oregon, USA, mostly by NOAA programs. They also present monthly climatologies derived from these observations.

The second data product is 23 years (1999–2021) of mooring temperature, salinity and velocity data — collected by five programs (OSU-NOPP, GLOBEC, OrCOOS, NANOOS/CMOP, OOI) at NH-10 (44.6°N, 124.3°W), 10 nautical miles west of Newport, Oregon along the NHL — that they stitched together into one coherent, quality-controlled data set (see figure above).

Making available such multi-decadal data sets, which they plan to release via public repositories, is essential to enable scientists to characterize natural and anthropogenically-forced variability; resolve cause-and-effect relationships in Earth’s climate and marine ecosystems at intra-seasonal, seasonal, inter-annual and decadal time scales; and verify climate models. These new gridded and concatenated data products show that long-term ocean observing efforts require multi-generational teams with a wide range of skills and a shared vision that is motivated by science and ocean monitoring needs.

Read More

R/V Oceanus Decommissioned and Celebrated

The R/V Oceanus was decommissioned last year, but its 45 years of service to the oceanographic community were celebrated at Oregon State University (OSU) at an event Friday May 6, 2022. The Coastal Endurance Array team used the Oceanus for many recovery and deployment expeditions before her retirement in 2021.

[media-caption path="/wp-content/uploads/2022/05/Picture1-copy.jpg" link="#"]The Oceanus was originally built in 1975 and began its work as a research vessel in 1976. Photo: OSU.[/media-caption]

[media-caption path="/wp-content/uploads/2022/05/graphics-OOI_AST2-DSC_5970.jpg" link="#"]R/V Oceanus departing WHOI on the deployment leg of OOI At-Sea Test 2 (AST-2) on September 22, 2011. Photo: Ken Kostel ©WHOI.[/media-caption]

Prior to its tenure at OSU, the Oceanus was in service at the Woods Hole Oceanographic Institution (WHOI) from 1976-2012.  WHOI retired the ship and it was transferred to OSU in 2012.  While at WHOI, the ship was used in early test deployments of equipment being evaluated for use in OOI arrays.

“The R/V Oceanus and its sister ship R/V Wecoma remain my favorite research vessels for air-sea interaction research due to their moderate size, uncluttered bows, and streamlined shapes,” said Jim Edson, Principal Investigator of the Ocean Observatories Initiative (OOI). “Research cruises on these vessels led to the development of the direct covariance systems we are using on the OOI surface moorings today.”

The Oceanus will be replaced with a new modern research vessel, the R/V Taani, which is expected to be delivered next year.

The Oceanus’ service in the Pacific is celebrated in this video produced by OSU:


Video remembrance of Oceanus:


Video of departure:



Read More

pH and pCO2 Time Series from the Endurance Array

Adapted and condensed by OOI from Dever et al., 2022, and Fassbender et al., 2018 doi://10.5194/essd-10-1367-2018.

The Ocean Observatories Initiative (OOI) Endurance Array makes extensive measurements of collocated physical and biogeochemical parameters throughout the water column. At the recent Ocean Sciences meeting, we reported on moored measurements from 2015 to the present off Washington and Oregon. We focused on spatial and temporal variability of pH and pCO2 and compared the measurements to published values in the region. This information was also presented in a seminar at UC, Santa Cruz on 14 Jan 2022.

[media-caption path="/wp-content/uploads/2022/04/Endurance-highlight.png" link="#"]OOI (blue, orange) mooring seasonal cycles and monthly averages (gray) for pCO2. For context, OOI mooring cycles are plotted together with Fassbender et al. (2018) (black) regional seasonal cycles.  WA moorings are compared with the Fassbender et al. Outer Coast (OC) region. OR moorings are compared with the Fassbender et al. North Pacific (NP) region.[/media-caption]

The quality-controlled biogeochemical time series are self-consistent and in line with other regional measurements. For example, pH and pCO2 have significant onshore-offshore variation and along-shelf differences north and south of the Columbia River. This variability is related to the Columbia River plume, the strength of local upwelling, and mixing with offshore waters. On a seasonal scale, pH and pCO2 is also driven by summer upwelling and winter river inputs. Variability is highest in spring and summer. pCO2 values greatly exceed atmospheric values (~400 μatm) at times in the summer (Figure above). The highest monthly pCO2 averages are seen at the Oregon shelf site.

Dever et al. (2022), pH and pC02 Time Series from the Ocean Observatories Initiative Endurance Array, CBP05, presented at Ocean Sciences Meeting 2022, Honolulu, HI (virtual), 01 Mar 2022.

Fassbender et al. (2018), Earth Syst. Sci. Data, 10, 1367–1401, 2018


Read More

In Spite of Weather, Endurance 16 Delivers

Weather did not deter the Endurance 16 cruise to recover and deploy ocean observing equipment to ensure the continuance of data to shore for the next six months.  When heavy weather closed in at the end of the second leg, the science party and crew aboard the R/V Sikuliaq met the challenge, accelerated their schedule, and arrived back in Newport on April 2, several days early.

“In spite of the less-than-ideal weather conditions, we successfully accomplished all activities with the exception of the Oregon Coastal Surface Profiler (CSPP) deployments and the Oregon offshore anchor recovery,” said Ed Dever, Chief Scientist for Endurance 16 and Principal Investigator of the Coastal Endurance Array team at Oregon State University. “When the weather cooperates, we will use a smaller vessel to deploy the remaining CSPP’s.  The anchor recovery will be done during Endurance 17.”

He added, “Early spring weather in the Northeast Pacific can be unpredictable and sometimes pretty nasty for shipboard operations.  We carefully monitored the weather conditions and adjusted our recovery and deployment schedule accordingly to maximize work that could be accomplished during safe weather conditions.

[media-caption path="" link="#"]Working to the weather. Spring in the North Pacific can bring pretty high winds and seas. When the Endurance 16 team had good weather, they pressed on through long days. Here Alex Wick and Kristin Politano get a subsurface float into position on the R/V Sikuliaq during an evening mooring deployment on the OOI Spring Endurance cruise. Credit: Ed Dever, OSU[/media-caption]

In spite of the abbreviated time at sea, in addition to the mooring deployments, the Endurance 16 team also successfully deployed four gliders and recovered another.  And, during the second leg of the cruise, a scientific party of five that had joined the expedition succeeded in collecting and recovering sediment trap samples for an ongoing experiment led by Dr. Jennifer Fehrenbacher of Oregon State University.

The sediment traps had been collecting material in place for the past six months and were recovered during the Endurance 16 team’s recovery and deployment work. Once the traps were back onboard, the collecting cups were taken off, emptied, replaced, and the traps redeployed for another six-month period. The researchers packaged the collected materials for analysis at OSU and her collaborators at the University of South Carolina.

The team also analyzed live specimens from night-time plankton tows,  which took advantage of the quiet night-time hours when the Endurance team was unable to safely move large, bulky, equipment in the dark.

Added Dever, “Success at sea is about teamwork, and I really appreciate  the science party and the captain and crew of the R/V Sikuliaq. Everyone was flexible and willing to work long, arduous hours to get the job done.”    

[media-caption path="" link="#"]At the end of an expedition everyone’s eager to get home. Here the R/V Sikuliaq approached NOAA’s pier in Newport, OR, but there was one more chore to do – get that recovered equipment off the deck.  The motivated crew and science party cleared the deck within 2 and half hours of docking! Photo: Ed Dever, OSU[/media-caption]


Read More

Summer 2021 Low Oxygen Event on the West Coast of North America

Adapted and condensed by OOI from Tetjana et al., 2022. 

A team of researchers using OOI Coastal Endurance data reported a low oxygen event on the west coast of America. They found that while hypoxic events are known to occur seasonally in coastal bottom waters along the west coast of North America, 2021 was more severely hypoxic. The onset of low oxygen water was the earliest in 35 years (NOAA, 2021), lasted longer (Lundeberg, 2021), was anomalously low, and covered a larger extent, reaching north into Canadian waters where hypoxia is rare (Crawford and Pe.a, 2013).

[media-caption path="/wp-content/uploads/2022/04/Screen-Shot-2022-04-12-at-3.44.04-PM.png" link="#"]Dissolved oxygen measured from an underwater vehicle glider operated by Oregon State University on a cross-shore transect off Grays Harbor, Washington, USA (plots available at and data available at the U.S. Integrated Ocean Observing System Glider Data Acquisition Center, ). Hypoxic water occupies the lower three-quarters of the water column near the mid-shelf mooring location (~80 m isobath) and stretches from the outer continental shelf, shoreward to at least the 50-m isobath.[/media-caption]

The paper was published in the Winter 2022 edition of Pices Press and can be reviewed here.



Read More

Uncovering Changing Life in the Water Column

Oregon State University Assistant Professor Jennifer Fehrenbacher needed a ship to carry out her National Science Foundation-funded research investigating the lives of foraminifera (single-celled organisms about the size of a grain of sand and smaller) in the northern Pacific. Her work, in collaboration with Dr. Claudia Benitez-Nelson at the University of South Carolina (UofSC), involves deploying bottom-moored sediment traps and collecting plankton tows while at sea, giving researchers the opportunity to explore foraminifera that live in lighted surface waters, and how these communities have changed over time in response to the surrounding ecosystem.

Fehrenbacher found her ship. She will be joining forces with the Endurance Array Team aboard the R/V Sikuliaq during its bi-yearly expedition to recover and deploy ocean observing equipment at its array in the northeast pacific off the coast of Oregon. Fehrenbacher and her team of four researchers will join the Endurance Array 16 team in early April for the second of its two-leg expedition. This will be a continuation of her research project that began in September 2021.

Last September, Fehrenbacher’s team put in place two tandem sediment traps that are located close to the OOI Slope base node. One was deployed at about 600 meters water depth, the other slightly above the sea floor. The last sediment trap study in this region was conducted around 30 years ago, and the foraminiferal species have likely changed since then, as have ocean conditions.

[media-caption path="/wp-content/uploads/2022/03/IMG_5185-copy.jpg" link="#"]Fehrenbacher’s team will be retrieving two tandem sediment traps that are located close to the OOI Regional Cabled Array slope base node. Credit: Jennifer Fehrenbacher, OSU.[/media-caption]

The sediment traps have been collecting material in place for the past six months and will be recovered along with the Endurance 16 team’s recovery and deployment work. Once the traps are back onboard, the collecting cups will be taken off, emptied, replaced, and the traps redeployed for another six-month period. The researchers will package the collected materials for analysis at OSU and UofSC.

The team also will be examining live specimens from night-time plankton tows, taking advantage of quiet night-time hours to conduct the plankton tows when the Endurance team is unable to work safely moving large, bulky, and unwieldy equipment in and out of the ocean.  “This arrangement is a win-win for everyone,” said Endurance Array Chief Scientist Ed Dever. “It maximizes the use of ship time, while helping to provide data to answer some questions about how ocean conditions are changing.”

Fehrenbacher’s team will be conducting a series of discrete new tows from the surface to about 500 meters. “While I don’t anticipate a ton of critters in the really deep water, net tows haven’t been done extensively in these waters at these depths. The last one was 30 years ago by oceanographer Alan Mix and his graduate student Joseph Ortiz, so this new work will give us insight into how life in the water column may have changed over time, “ said Fehrenbacher.

Fehrenbacher’s team will be conducting experiments with live foraminifera in a portable travel lab they will bring onboard.  A number of different experiments are planned:

PhD candidate Kelsey Lane will be collecting foraminifera (shortened version “forams”) to study their genetics and their microbial communities, other species living with forams.

Graduate student Grace Meyer will be striving to measure carbon and oxygen isotopes in individual forams. She will be collecting empty shells from both the water column and sediment trap material and compare what is found in both, providing information about water column processes that could alter shells’ composition.

Postdoctoral researcher Brittany Hupp will be collecting both live forams and empty shells to study the chemistry of different types of forams, looking  at their isotopes and trace metals content.

Researcher Eric Tappa, a sediment trap expert from the UofSC, will be deploying and recovering the sediment trap equipment. Tappa has been working with sediment trap moorings for decades and have proven critical in providing longer time-series records of processes occurring in overlying waters.

As lead scientist Fehrenbacher will be participating in these onboard experiments. She also will be growing forams under controlled conditions and watching them to learn how temperature modulates their shells or their behaviors during the day-night cycle, and will continue her work with recovered forams once she returns to her home lab. There she will be measuring the trace element concentrations in foram shells so results can help inform the Paleo record. . She explained, “Foram shells are used basically as proxies for environmental conditions. So when we measure trace elements in their shells, this gives us information about the pH,  temperature, nutrient content,  and even the salinity of the ocean in the past.”  The onboard experiments help scientists under how forams incorporate these elements into their shells when they are alive, which they can use in assessing past records.

[media-caption path="/wp-content/uploads/2022/03/IMG_5196-copy.jpg" link="#"]An anchor weighing ~2500 pounds is deployed to keep a sediment trap in place for six months until it is recovered with a treasure trove of marine life and particulates for investigation. Credit: Jennifer Fehrenbacher, OSU.[/media-caption]

Challenges of studying small living things

Studying single-celled organisms is difficult on dry land, but is compounded by a moving ship in rolling seas.  Fehrenbacher’s team will be taking onboard multiple microscopes, including an inverted microscope to see their subjects, water circulators to keep them at constant conditions while they are alive, and a pH meter. High-powered microscopes are critical for the work because forams range in size from smaller than a grain of sand—about 100 microns— to up to about a millimeter.

“We look at forams in a petri dish under the microscope,” explained Fehrenbacher.  “This is challenging as the ship moves back and forth so does the water in the petri dish so you’re looking back and forth as the ship moves.”  The researchers have come up with the solution of holding the petri dish at an angle so the water and foram stay in one place and helps prevent researchers’ sea sickness.

Fehrenbacher predicts that the amount of material collected on the Endurance Array 16 cruise will keep she and her graduate students busy for at least the next two years and beyond.  She added, “There’s really just nothing quite like the type of information you can get from sediment trap studies.  While going out to sea for two weeks a year and doing plankton tows are helpful, we only get information about what’s in the water column at the exact moment of collection. But sediment traps provide months’ worth of data at really high resolution that we can compare with other OOI data and get a detailed picture of ocean conditions and how those conditions affect marine life.





Read More

Sixteenth Turn of the Coastal Endurance Array

A team of ten scientists and engineers will depart aboard the R/V Sikuliaq in late March for a two-week expedition to recover and redeploy ocean observing equipment at the Coastal Endurance Array. Located in the northeast Pacific off the coasts of Oregon and Washington, the Coastal Endurance Array consists of two cross-shelf moored array lines, designed to observe cross-shelf and along-shelf variability in the region.

The team will recover and deploy seven moorings. Four of the moorings are located on the Washington Shelf, with the remaining three on the Oregon Shelf. The team also will be recovering a surface piercing profiler at the Washington Shelf site and deploying four surface piercing profilers on the Washington and Oregon lines. Another goal of the team is to deploy and recover gliders so that five are in the water and continue to sample and report back data over the next three months. The gliders collect data across the shelf in shallow water down to 200 meters and also collect data offshore down to depths of 1000 meters.

[media-caption path="/wp-content/uploads/2022/03/sea-lions.png" link="#"]The Endurance Array team has to contend with occasional visits of sea lions, which can weigh up to 1000 pounds, and who like to explore the components of the array. This expedition will be testing a re-enforce solar platform to see if can better bear the weight of these hefty and curious visitors. Credit: Endurance Array team.[/media-caption]

When not recovering and deployment equipment, members of the onboard team will be taking CTD (connectivity, temperature, and depth) casts to verify and calibrate instrumentation. Because of the quantity of the equipment to be recovered and deployed, the cruise will take place in two separate legs.

Measurements collected by this array capture the variability of ocean properties across a broad range of temporal and spatial scales. Scientists are using these data to examine ocean health issues such as hypoxia, ocean acidification, and harmful algal blooms, and changing ocean conditions such as intermittent marine heat waves.

“Every time we head out to turn the Endurance Array, the OSU team works together with folks at WHOI to improve the resilience of the gear we put out there and to improve the quality of the data collected,” said Ed Dever, Principal Investigator for the Coastal Endurance Array, serving as Chief Scientist for the Endurance 16 expedition. “It’s a tough environment. The equipment spends six months at sea, getting jostled by high waves and strong winds and serving as habitat for marine life big and small.  Yet over the last eight years, we’ve continuously made improvements  to the instruments and infrastructure to improve data return. It’s a real testament to the creativity and skills of the whole team. They never stop thinking about ways to make things even better.”

During the second leg of the cruise, a scientific party of five will join the expedition to collect sediment samples for an ongoing experiment led by Dr. Jennifer Fehrenbacher from Oregon State University. This specific scientific inquiry is an example of how the OOI was designed to add instrumentation and adapt sampling approaches to meet the needs of the scientific community it serves.  

[media-caption path="/wp-content/uploads/2022/03/Sediment-trap.jpeg" link="#"]Dr. Jennifer Fehrenbacher’s team will be deployin this   McLane Mark VII 13 cup Sediment Trap, which is used to collect a time-series of material falling through the water column. The stack of three railroad wheels (on right) are the anchor. Credit: University of South Carolina.[/media-caption]

To help answer other specific science questions, the Endurance 16 team also will be conducting sampling for researchers with instruments on the Endurance Array moorings. The team will test deployment of fish acoustic monitors on the near shore instrument frames (see picture below) of both inshore moorings and the Washington Shelf surface mooring for Taylor Chappel a researcher at Oregon State University.  The team will also collect settling organisms on devices attached to multi-function nodes on the Oregon Offshore and Surface moorings for Oklahoma State researcher Ashley Burkett.

[media-caption path="/wp-content/uploads/2022/03/Endurance-mfn.png" link="#"]This Near-Surface Instrument Frame (NSIF) is an instrumented cage that is suspended below surface moorings.  (7m for Coastal moorings, 12m for Global moorings). The NSIF contains subsurface oceanographic instruments attached to multiple data concentrator logger computers. During Endurance 16, fish acoustic monitors will be added to the standard equipment. Credit: Ed Dever, OSU.[/media-caption]

During this expedition, the team also will be deploying new equipment and other improvements. For example, a new anemometer, which sits at the top of the mooring to measure the wind speed will be deployed for the first time. A new camera made with off-the-shelf components will be put into field during for its first six-month deployment.  And, the team will be testing the rigor of its newly reinforced solar panels, which often have to withstand the weight of the occasional visit by sea lions.

The team has followed all COVID protocols and are ready to go.  They will be blogging and sharing photographs of their two-week expedition.  Bookmark this page and follow along as they share their stories.

Read More

Observations of Cross-Shelf Nitrate Fluxes over the Oregon Continental Shelf

Extracted from OOI Quarterly Report, 2022.

The US Pacific Northwest coastal ecosystems are primarily limited in growth from nitrate supply.  The nitrate supply that drives the highly productive marine growth in this region is primarily a result of wind driven coastal upwelling.  This work seeks to investigate cross-shelf nitrate fluxes over the continental shelf off the coast of Oregon following the installation of new nitrate and Acoustic Doppler current profilers (ADCPs) in the Ocean Observatories Initiative Coastal Endurance Array.

[media-caption path="/wp-content/uploads/2022/02/Endurance.png" link="#"]Figure 24.  A velocity and nitrate profile from the shelf site at the Newport line. Data used was from the 2019 summer, approximately mid-June to early October (deployments 13, 14, and 15). The net nitrate flux found at that site over this time period, found by vertically integrating the values above, is roughly 1.16 mmol Nitrate/second/meter coastline. [/media-caption]

The primary onshore flow of nitrate-rich water over the continental shelf is found to originate at the middle depths, consistent with previous research in the region. However, the upwelling and cross-shelf nitrate fluxes on the continental shelf are found to be in poor agreement with common upwelling indices, e.g., coastal upwelling transport index (CUTI) and biologically effective upwelling transport index (BEUTI).  Several factors for this disagreement are proposed, including the focus of the indices on dynamics farther offshore of the continental shelf.  Observed coastal wind stress, calculated on a weekly rolling average, is found to be a potential alternative for predicting nearshore nitrate concentrations. Farther offshore at the mid-shelf, only a weak correlation between observed wind stress and observed surface transport is found, suggesting the need for additional dynamics to fully explain the observed surface transport and nitrate fluxes. Correctly modelling the nitrate supply for coastal ecosystems is essential for predicting phytoplankton blooms that are vital to the production of fisheries on the coast.  Thus, understanding these limitations is of great importance for ocean-driven coastal economies.

Written by Andrew Scherer, California State University, Monterey Bay and Cleveland State University and Thomas Connolly, Moss Landing Marine Laboratories, San José State University

Andrew Scherer is an undergraduate physics student at Cleveland State University.  In summer 2021, he performed this research with Prof. Tom Connolly (MLML, SJSU) as part of a National Science Foundation Research Experience for Undergraduates program  and presented it at the Eastern Pacific Ocean Conference Stanford Sierra Center, Fallen Leaf Lake, California 26-29 Sep 2021.

Read More

R/V Oceanus Remembered as a Workhorse of the U.S. Academic Research Fleet

The long service of the R/V Oceanus (1976-2021) came to end on November 21, 2021 as the ship pulled into port after having successfully completed its last interdisciplinary cruise for Oregon State University (OSU). The Oceanus began its 45-year-run of scientific investigations at Woods Hole Oceanographic Institution (WHOI) in 1976.  After a major mid-life refit, the ship was transferred to OSU in 2012, and contributed to the Ocean Observatories Initiative (OOI) off both coasts.

“The Oceanus proved to be a real workhorse for the Academic Research Fleet and also played a pivotal role for the OOI during its initial launch,” said Ed Dever, PI of OOI’s Coastal Endurance Array, who sailed on the ship many times. “While at WHOI, The Oceanus performed some of OOI’s at-sea-mooring test deployments and later the ship was used for the initial deployment of the Coastal Endurance Array off the Oregon coast.”

In spring and fall 2014, after moving to OSU, Oceanus performed the initial deployments of the Oregon and Washington inshore moorings and Washington profiler mooring.  The real test for the Oceanus, however, came during 2015, when it was tasked with deploying the full scope of the Endurance Array, including the four large coastal surface moorings at the Oregon and Washington shelf and offshore sites.

Explained Dever, “Thanks to some excellent ship handling, care on the part of the deck crew and a huge assist from some very kind weather, we got the moorings safely in the water using the ship’s crane to deploy the 10,000-pound buoy off the starboard fantail and the heavy lift winch to deploy the 11,000-pound multifunction node (MFN, bottom lander) through the A-frame. The size of the buoys and MFNs meant that Oceanus could only carry one buoy out at a time and the cruise was completed in five legs with some very efficient port stops. By the end of the cruise, it was evident that we would need to move future operations to global and oceans class ships and after one more deployment in fall 2015 (with recoveries carried out on the R/V Thomas G. Thompson), we made that transition.”


After the initial Endurance Array deployments, OOI transitioned to using larger global and oceans class ships needed to recover the bulky coastal surface moorings, with one exception. In spring 2019, with tight schedules on global class ships, UNOLS (University-National Oceanographic Laboratory System charged with ship scheduling) requested that OOI Endurance split the spring mooring recovery and deployment cruise between the R/V Sikuliaq and the R/V Oceanus. The Oceanus ably performed the profiler mooring deployment, anchor recoveries, coastal surface piercing profiler deployments, and glider deployments over five days in April and May 2019.

While not directly working with the OOI, the Oceanus continued to work off Oregon at and around the OOI arrays.  Research and student cruises often sampled over the years near OOI’s  Endurance and RCA Arrays at the Oregon inshore, shelf, offshore and Hydrate Ridge sites to compare shipboard measurements and OOI time series.  This work included CTD profiles, net tows, coring, and sediment trap deployments.

The last Oceanus cruise, in fact, was one such interdisciplinary research cruise led by OSU researcher Clare Reimers, who also served as chief scientist.  During its final official outing, the team aboard the Oceanus sampled the outer shelf at the northern end of Heceta Bank, Oregon to help scientists determine any changes that may have occurred to a swath of the margin that was reopened to commercial bottom trawling in 2020 after an 18-year closure.  Reimers said, “The R/V Oceanus and crew performed flawlessly, and our science mission was fully completed.”

Added Dever, “What better way to end its long and illustrious career?  We at OOI join many others in appreciation of the R/V Oceanus, and the dedication and skills of all who sailed on her and supported ocean science throughout her many years at sea.”


Special thanks to OOI Data Center Project Manager Craig Risien for sharing the GoPro time lapse of the loading of the Oregon Offshore mooring onto the R/V Oceanus in spring 2015.

Read More

Endurance Array to Provide Hourly Meteorological Data

On 11 October 2021, the National Oceanic and Atmospheric Administration (NOAA)requested that OOI’s Coastal Endurance Array buoys provide hourly meteorological data to the National Data Buoy Center (NDBC) because a nearby NDBC buoy (46029, Columbia River bar) had gone offline. OOI buoy data are typically telemetered every two hours due to sampling schedule and bandwidth constraints (the actual sampling rate is higher).

Endurance Array team members examined sampling and telemetry schedules for the Endurance offshore coastal surface moorings to see if they could accommodate NOAA’s request. The team concluded that meteorological data from the moorings could be updated hourly while still meeting OOI sampling requirements.

“To help ensure continuity of data to the NDBC,  we plan to distribute hourly meteorological data from the Endurance Array Oregon and Washington offshore sites for the duration of the outage at NBDC 46029,” said Edward Dever, lead of the Coastal Endurance Team. “We’re pleased to respond to NOAA’s request and hope these data prove useful to operational weather forecasts and marine safety.” The Oregon and Washington offshore sites have NDBC buoys designations of 46098 and 46100, respectively.

The Endurance Array team will continue to review the performance of the buoys and ensure the updated telemetry schedule does not impact OOI sampling. If data users do experience any impacts from this change in sampling frequency, please contact Jon Fram at

Read More