Award Abstract # 1536851
Collaborative Research: The Oleander Project: High-resolution observations of the dynamic ocean between New Jersey and Bermuda

NSF Org: OCE
Division Of Ocean Sciences
Recipient: UNIVERSITY OF RHODE ISLAND
Initial Amendment Date: September 14, 2015
Latest Amendment Date: March 8, 2022
Award Number: 1536851
Award Instrument: Continuing Grant
Program Manager: Baris Uz
bmuz@nsf.gov
 (703)292-4557
OCE
 Division Of Ocean Sciences
GEO
 Directorate for Geosciences
Start Date: September 15, 2015
End Date: March 31, 2023 (Estimated)
Total Intended Award Amount: $391,520.00
Total Awarded Amount to Date: $391,520.00
Funds Obligated to Date: FY 2015 = $80,927.00
FY 2016 = $68,886.00

FY 2017 = $75,666.00

FY 2018 = $85,856.00

FY 2019 = $80,185.00
History of Investigator:
  • H. Thomas Rossby (Principal Investigator)
    trossby@uri.edu
  • Kathleen Donohue (Co-Principal Investigator)
Recipient Sponsored Research Office: University of Rhode Island
75 LOWER COLLEGE RD RM 103
KINGSTON
RI  US  02881-1974
(401)874-2635
Sponsor Congressional District: 02
Primary Place of Performance: University of Rhode Island
215 South Ferry Road
Narragansett
RI  US  02882-1197
Primary Place of Performance
Congressional District:
02
Unique Entity Identifier (UEI): CJDNG9D14MW7
Parent UEI: NSA8T7PLC9K3
NSF Program(s): PHYSICAL OCEANOGRAPHY
Primary Program Source: 01001516DB NSF RESEARCH & RELATED ACTIVIT
01001617DB NSF RESEARCH & RELATED ACTIVIT

01001718DB NSF RESEARCH & RELATED ACTIVIT

01001819DB NSF RESEARCH & RELATED ACTIVIT

01001920DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 1324, 9150, EGCH
Program Element Code(s): 161000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

This project will extend for five years and enhance the multi-decadal oceanographic observations from the MV Oleander, a container vessel that on a weekly schedule crosses four distinct regions, namely the continental shelf, Slope Sea, Gulf Stream and Sargasso Sea on its route between New Jersey and Bermuda. The enhancements include an acoustic Doppler current profiler (ADCP) pair that will provide direct measurement of the currents through the base of the thermocline to about 1200 m depth in the open ocean on the one hand, and high vertical resolution profiling of the upper ocean on the other. The former will enable research into the full upper ocean structure of the Gulf Stream, the mesoscale eddy field, and the highly variable Sargasso Sea, all of which are important components in the large scale ocean circulation including the climatically important meridional overturning circulation (MOC). The latter will greatly improve coverage on the continental shelf, shelfbreak front and resolution of the mixed layer seasonal thermocline structure.

The Oleander track is uniquely situated as it enables in situ measurements across the shelf and slope, through the southernmost extension of the North Atlantic subpolar gyre, and into the subtropical gyre. The beauty of these ADCP snapshots is that they tell us what the ocean is doing over a wide range of scales. Ensemble averaging these leads to robust data sets that will contribute to continued and deeper investigations into (1) seasonal, and interannual to decadal variability on the mid-Atlantic Bight shelf, (2) dynamics controlling the communication between the shelf and open ocean, (3) connectivity along western boundaries in the MOC at different latitudes, and (4) interannual to decadal variability in the Gulf Stream position, strength and the structure of the subpolar gyre, and the recirculation in the Sargasso Sea. In addition, the high horizontal resolution of surface salinity, temperature and velocity afforded by individual tracks will enable continued investigation into sub-mesoscale processes. A replacement ship is expected to enter service in the second or third year of the project. With the installation of two new ADCPs on the new hull, one for improved shelf-slope operation and one to profile to 1200 m depths, the Oleander project will greatly increase its observational footprint in the northwest Atlantic. All data will be available to the public as soon as they are processed and quality-controlled. The expansion of the University of Hawaii UNOLS-wide ADCP data acquisition system, UHDAS to include volunteer observing ships will allow for real time data streams from not only the Oleander, but also other such ADCP-equipped vessels in operation in the North Atlantic.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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(Showing: 1 - 10 of 11)
Andres, M., K. A. Donohue, and J. M. Toole "The Gulf Stream's Path and Time-averaged Velocity Structure and Transport at 68.5W and 70.3W" Deep-Sea Research , 2019
Bisagni, J.J., A. Gangopadhyay, and A. Sanchez-Franks "Secular change and inter-annual variability of the Gulf Stream position, 1993?2013, 70°?55°W" Deep-Sea Rsearch, I , v.125 , 2017 http://dx.doi.org/10.1016/j.dsr.2017.04.001
Callies, J. "Submesoscale dynamics inferred from Oleander data." Oceanography , v.32 , 2019 , p.106 https://doi.org/10.5670/oceanog.2019.3xx.
Fratantoni, D. F., J. K. O?Brien, C. Flagg, and T. Rossby "AXIS?An Autonomous Expendable Instrument System" J. Atmospheric and Oceanic Technology , v.34 , 2017 , p.2673 10.1175/JTECH-D-17-0054.1
Palter, J., L. Cook, A. M. G. Neto, S.Nickford, and D. Bianchi "Acoustic backscatter patterns." Oceanography , v.32 , 2019 , p.108 https://doi.org/10.5670/ oceanog.2019.3xx.
Rossby, T., C. Flagg, K. Donohue, S. Fontana, R. Curry, M. Andres, and J. Forsyth "The Oleander is more than a flower: Twenty-five years of Oceanography aboard amerchant vessel." Oceanography , v.32 , 2019 , p.1 https://doi.org/10.5670/ oceanog.2019.3xx.
Rossby, T., R. Curry, and J. Palter "Packing science into a shipping vessel," Eos , 2017 https://doi.org/10.1029/2017EO071319
Sanchez-Franks, A., S. Hameed and R.E. Wilson "The Icelandic Low as a predictor of the position of the Gulf Stream north wall position" J. Physical Oceanography , v.44 , 2016 , p.817
Schloesser, F., P. Cornillon, K. Donohue, B. Boussidi and E. Iskin. "Evaluation of thermosalinograph and VIIRS data for the characterization of near-surface temperature fields." J. Atmospheric and Oceanic Technology , v.33 , 2016 , p.1843 https://doi.org/10.1175/JTECH-D-15-0180.1
Smith, S.R., K. Briggs, N. Lopez, N. and V. Kourafalou "Applying Automated Underway Ship Observations to Numerical Model Evaluation." J. Atmospheric and Oceanic Technology , v.33 , 2016 , p.409
Tom Rossby, K. Donohue, J. Palter "What can Hydrography between the New England Slope, Bermuda and Africa tell us about the strength of the AMOC?" Geophysical Research Letters , v.49 , 2022 , p.e2022GL09 10.1029/2022GL099173
(Showing: 1 - 10 of 11)

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

Early in 1990 we learned that the Bermuda Container line was building a new ship, to be named MV Oleander, to operate on its Bermuda ? New Jersey route. That summer we approached the builders about installing an acoustic Doppler current profiler in its hull so we could monitor ocean currents along its route with focus on the Gulf Stream; an idea they enthusiastically endorsed. Thanks to their support we have been monitoring ocean currents from the New England slope to Bermuda almost without interruption since the fall of 1992. It has been quite a journey that continues today thanks to a new operating grant to Dr. Magdalena Andres at WHOI. 

The most recent grant focused on upgrading the operation to include two ADCPs on the new MV Oleander which arrived in early 2019. The ADCPs (38 kHz and 150 kHz) were installed during vessel construction in China. For reasons unknown the 38 was installed underneath the engine room making for serious service problems. The 150 was installed as planned but it is so far forward it was damaged twice most likely due to breaching and slamming at the surface in heavy seas. These issues are being addressed under the new grant. 

We published a comprehensive account of the first 25 years of operation in the September 2019 issue of the magazine Oceanography. In it we conclude that we cannot detect any significant trend in upper ocean transport over that time. This is not to say there isn?t any trend, but any trend is so small it is masked by the modest interannual variations in transport during that period. 

Another important finding was that the average velocity normal to the Bermuda ? NJ route goes to zero at about 1000 m depth: poleward at shallower depths, equatorward at greater depths. This is the depth of the maximum in the Atlantic meridional overturning circulation (AMOC) overturning stream function. This depth is also below the main thermocline and the subtropical wind-driven circulation. This finding allowed us to use archived hydrographic data to determine trends in the AMOC and the subtropical gyre transport over the last 70-90 years. We found that transport between the continental slope and Bermuda likely decreased about 2?0.8 Sv (1 Sv = 106 m3s-1) with most of this due to changes in the subtropical gyre transport, and an insignificant decrease in the AMOC (-0.4?0.6 Sv). While the uncertainties preclude tighter estimates of change, these geostrophic estimates are almost certainly the best ones to date of AMOC and wind-driven transport and recent trends at this latitude.  These results were reported in detail in the December 2022 issue of Geophysical Research Letters. 

The Oleander project has stimulated numerous spin-off activities. Notably, studies of the long-term warming on the northeast shelf and linkages to accelerated sea-level rise and marine heatwaves as well as seminal observationally-based studies of high-horizontal resolution dynamics.

On the technical side, two developments underway which we hope will greatly improve ADCP science on merchant marine vessels broadly. The first is the development of programmable, magnetically-attached hull camera that will be used to study the presence and character of bubble entrainment. Bubbles block the ADCP acoustics, so we need to better understand the factors that control their presence. High seas is obvious, but other factors as draft of the vessel, shape of the bow, and location of the ADCP in the hull come into play. It is high time we understand these factors better. The other development is to use computational fluid dynamics (CFD) to better understand how we can divert bubbles from under the ADCP, either by placing it in a fairing that extends below the hull or using chines to create a local upwelling of clear water. We want to evaluate the merits of fairings and chines from the point of view of maximizing clear water and minimum drag-cost to the ship. Both initiatives are underway and should help us optimize the relocation of the ADCPs in the Oleander when she is in dry dock this coming January. Developing a know-how for creating bubble-free spots or windows in the hull is an engineering effort that should have been done long ago; it has the potential to open up all kinds of possibilities for future acoustic and optical remote sensing on merchant marine vessels. 


Last Modified: 08/11/2023
Modified by: H. Thomas Rossby

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