Deep Water Horizon

**This project is complete. The page serves as an archive for work completed by AOML during the event.**

Monitoring the Gulf of America During the Deepwater Horizon Oil Spill

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What We Did

As part of NOAA’s mission to study the role of the ocean in climate and ecosystems, scientists at AOML have been devising methods and tools to allow for the real-time monitoring of ocean conditions. Following the Deepwater Horizon explosion in April 2010, AOML organized a scientific response effort building upon these capabilities. This webpage was designed to provide data and graphical products about ocean currents, sea surface temperature, sea level, ocean color, and particle displacement, during and after the event. These data were obtained using direct ocean measurements, remote observations collected via satellite, and outputs from numerical models.

Scientists at AOML participated in spill related research panels, published scientific manuscript related to the ocean conditions during the oil spill, and led research cruises focused on assessing the extent of the spill in the greater Gulf of America and the potential for entrainment via the Loop Current to downstream ecosystems. AOML and NOAA’s Southeast Fisheries Science Center (SEFSC) also organized an oceanography workshop in Miami on July 1-2, 2010, where observations, methods, and strategies were discussed.

Satellite image of the Gulf of America, showing the location of the Deepwater Horizon spill site and the extent of the oil spill on April 20, 2010.

Satellite image of the Gulf of America, showing the location of the Deepwater Horizon spill site and the extent of the oil spill on April 20, 2010.

Ocean Conditions in the Gulf of America

These maps of ocean surface currents determined from satellite measurements provide information to scientists, decision makers, and emergency response personnel about the present oceanic flows and how they are changing with time.

The map to the right shows an estimate of the surface currents in the Gulf of America in August of 2010. The red star indicates the location of the Deepwater Horizon explosion. The solid red line indicates the location of the Loop Current and anticyclonic rings and eddies (red) and cyclonic eddies (blue).

SHA data source: US Global Ocean Data Assimilation Experiment (GODAE)

Currents produced by NOAA/AOML and NOAA/CoastWatch.

Gulf of America current map in August 2010 after the Deepwater Horizon oil spill.

Surface Current Fields

To see an animation of the surface currents field during the Deepwater Horizon event, please select one of the months below:

Deepwater Horizon Oil Spill Monitoring

These instruments were used to monitor the Deepwater horizon oil spill during the summer of 2010. Click on the icons below to learn more.

eXpendable BathyThermograph

An Expendable BathyThermograph (XBT) is a probe that is dropped from a ship and measures the temperature as it falls through the water. A very thin wire transmits the temperature data to the ship where it is recorded for later analysis. The probe is designed to fall at a known rate, so that the depth of the probe can be inferred from the time since it was launched.

During several research missions in the Gulf of America, AOML and CIMAS scientists, onboard the NOAA Ship Gordon Gunter, the R/V F.G. Walton Smith, and the NOAA ship Nancy Foster deployed XBT instruments near the location of the Deepwater Horizon oil rig.

Jump to Observations

Why are these observations helpful?

XBT data provide information about the large scale circulation in the Gulf of America. They describe the surface temperature as well as the structure of oceanic thermal features at different depths. They also provide information about ocean heat content and can be used in the validation of numerical models currently being utilized in the Gulf of America monitoring.

Conductivity Temperature Depth

Conductivity Temperature Depth (CTD) is an electronic device used by oceanographers to measure temperature, salinity (via conductivity), depth (via pressure), and density as the instrument is deployed in the water from a ship. The sensors for conductivity, temperature and pressure are attached to a frame along with optional auxiliary sensors, such as those for measuring oxygen concentration and fluorescence. As the CTD package is lowered into the water via a hydrowire, scientists are able to determine the distribution of these sea water properties as a function of depth.

During several research missions in the Gulf of America, AOML and CIMAS scientists, onboard the NOAA Ship Gordon Gunter, the R/V F.G. Walton Smith, and the NOAA ship Nancy Foster deployed CTD instruments near the location of the Deepwater Horizon oil rig.

Jump to Observations

Why are these observations helpful?

CTD data provide information about the large scale circulation in the Gulf of America. They describe the surface temperature as well as the structure of oceanic thermal features at different depths. They also provide information about ocean heat content and can be used in the validation of numerical models currently being utilized in the Gulf of America monitoring.

eXpendable Current Profiler

An eXpendable Current Profiler (XCP) is a probe that is dropped from a ship or an aircraft and measures the temperature and velocity as it falls through the water. A very thin wire transmits the measurements to the ship where it is recorded for later analysis. The probe is designed to fall at a known rate, so that the depth of the probe can be inferred from the time since it was launched. XCPs allow for rapid surveying from an aircraft or ship underway obtaining snapshots of oceanic vertical and horizontal structure on horizontal scales of 10’s of kilometers. This instrument allows dynamical studies of internal gravity waves (including near-inertial waves and internal tides), fronts, and vortices (including rings and eddies).

Jump to Observations

Why are these observations helpful?

XCP data provide information about the vertical structure of the large scale circulation in the Gulf of America. They describe the ocean current and temperature as a function of depth. Their information of surface currents can be used in the validation of numerical models currently being utilized in the Gulf of America monitoring.

 

Airborne EXpendable BathyThermograph

The Airborne EXpendable BathyThermograph (AXBT) measures ocean temperature as a function of depth. The temperature profiles produced are from the surface to 350 m, at 1.5 m vertical intervals. During several joint missions by the University of Miami and NOAA in the Gulf of America, these probes were deployed from a NOAA WP-3D aircraft .

Jump to Observations

Why are these observations helpful?

AXBT data provide information about the large scale circulation in the Gulf of America. They describe the surface temperature as well as the structure of oceanic thermal features at different depths. They also provide information about ocean heat content and can be used in the validation of numerical models currently being utilized in the Gulf of America monitoring.

 

Surface Drifters

Satellite-tracked drifting buoys, or “drifters”, measure sea surface temperature, but most are also equipped to measure other variables. As the drifter moves around, guided by ocean currents, measurements of atmospheric pressure, winds, wave height, and salinity can be taken. This data is collected by sensors in the drifter and transmitted to overhead satellites. A drifter’s drogue, also known as a sea anchor, extends 20 meters (or 65 feet) deep and is designed to move with the near-surface ocean currents. The drogue and surface float move together, connected by a long tether.

Tracking the location of drifters over time allows scientists to build a profile of ocean currents. Many are deployed by NOAA as part of the Global Drifter Program (GDP).

Jump to Observations

Why are these observations helpful?

Satellite-tracked drifting buoys travel with ocean surface currents. These instruments provide scientists with a direct measure of upper-ocean circulation.

XBTCTDobs

XBT and CTD Observations

Temperature and Salinity Sections: July 1-18, 2010 (NOAA ship Nancy Foster)

The map to the right shows the location of  eXpendable BathyThermograph (XBT) (circles) and Conductivity Temperature Depth (CTD) (triangles) observations carried out by AOML scientists onboard the NOAA ship Nancy Foster between July 1-18, 2010. The map also shows the mean sea surface temperature (SST, °C) for the previously mentioned dates, superimposed on the regional bathymetry (in meters). The location of the Deepwater Horizon rig is denoted by a star.

Nine temperature sections and six salinity sections were produced using the XBT and CTD profiles obtained by the scientists during their cruise in the Gulf of America. These sections can be viewed by clicking on the sections below. In all sections, the deployment locations of XBT and CTD are indicated by green and blue inverted triangles, respectively.

Section #1 at 82°W (magenta triangles)

Temperature:

 

Salinity:

Section #2 at 83.7°W (red circles)

Temperature:

 

Salinity:

Section #3 at 24.7°N (brown circles)

Temperature:

 

Salinity:

Section #4 at 85.8°W (green circles)

Temperature:

 

Salinity:

Section #5 at 25.5°N (white circles)

Temperature:

Section #6 at 25.5°N (blue circles)

Temperature:

 

Salinity:

Section #8 at 26.5°N (purple circles)

Temperature:

 

Salinity:

Section #9 at 88°W (orange circles)

Temperature:

Section #10 at 88.2°W (cyan circles)

Temperature:

Temperature Sections for June 7-10, 2010 (R/V F.G. Walton Smith)

The map to the right shows the location of eXpendable BathyThermograph (XBT) observations (red, green and purple dots) deployed by AOML and University of Miami scientists onboard the R/V F.G. Walton Smith between June 7-10, 2010. The map also shows the mean sea surface temperature (SST, °C) for the previously mentioned dates, superimposed on the regional bathymetry (in meters). The location of the Deepwater Horizon rig is denoted by a star. Three temperature sections were produced using temperature profiles obtained by the scientists during their transit from Gulf Port, Mississippi to Miami, Florida, and these sections can be viewed by clicking on the observations listed here (section 1-redsection 2-green, and section 3-purple dots). 

Temperature Sections for May 28-30, 2010 (NOAA Ship Gordon Gunter)

The map to the left shows the location of eXpendable BathyThermograph (XBT) deployments (red, purple and brown dots) by AOML scientists onboard the NOAA Ship Gordon Gunter, and the mean sea surface temperature (SST, °C) for May 28-30, 2010 superimposed on the regional bathymetry (in meters). The location of the Deepwater Horizon rig is denoted by a star.

The XBT probes were deployed in concentric patterns near the location of the Deepwater Horizon oil rig. Two temperature sections were produced using the temperature profiles from the outer circle, located north (red dots), and south (purple dots) of the sunken oil rig.

Data source for SST: Remote Sensing Systems

XCPobs

EXpendable Current Profiler (XCP) Observations

Velocity and Temperature Profiles

The map to the right shows the location of  eXpendable Current Profiler (XCP) observations (blue dots) deployed by AOML and CIMAS scientists from a NOAA WP-3D aircraft between May 18-21, 2010. The map also shows the geostrophic surface velocity (vectors) and speed (colors) derived from satellite altimetry observations corresponding to the date of the survey. The location of the Deepwater Horizon rig is denoted by a red star. Nineteen profiles were collected over the Loop Current, shown by the large values of surface currents (orange and red colors).

AXBTobs

Airborne EXpendable BathyThermograph (AXBT) Observations

Velocity and Temperature Profiles

The location of Airborne EXpendable BathyThermograph (AXBT) deployments for July 9, 2010 are shown in the map to the left. The map also show the corresponding sea surface temperature (SST, °C) superimposed on the regional bathymetry (in meters). The location of the Deepwater Horizon is denoted by a star. Temperature sections for July 9, 2010 are found here: at 24°N (blue circles)25°N (green circles)25.75°N (brown circles)26.5°N (purple circles)27.2°N (yellow circles), and 28°N (red circles). Deployments denoted by white circles with crosshairs were omitted from the temperature sections.

To view all of the velocity and temperature profiles for AXBT’s deployed in response to the Deepwater Horizon spill, click the button below. Dates of each mission and the corresponding temperature sections can be viewed here. The location of AXBT deployments for each mission are shown in the maps with the corresponding sea surface temperature.

drifterobs

Surface Drifter Observations

NOAA’s Global Drifter Program arranged for 36 drifters to be deployed in the Gulf of America in 2010 following the Deepwater Horizon spill. The data from these drifters were transmitted on the Global Telecommunication System for real-time distribution, and are available in ASCII format via ftp. These drifters were deployed in pairs, so that their relative spreading rates could be quantified. The trajectories of these drifters mapped the ocean features in the Gulf, like the warm ring and the Loop Current, and helped scientists understand and forecast where these features would carry the oil.

On June 7-9 2010, 6 drifter pairs were deployed from the R/V Walton Smith between the Deepwater Horizon site and the Dry Tortugas. The final two pairs were deployed close together in a convergence region where personnel aboard the Walton Smith observed oil being carried southward in a frontal jet. In July 2010, 12 drifter pairs were deployed from the R/V Nancy Foster. These deployments were concentrated in the Loop Current and the large eddies north and northwest of the current. For more deployment information please visit our Deployment Log page.

The map to the left shows the paths taken by all Global Drifter Program drifters that have ever passed through the white box in the northern Gulf of America. The color is the number of days since passing closest to the center of the box. Any time longer than two years is dark red. Data source: Drifter Data Assembly Center (DAC)

Global Drifter Program SVP-type drifters, drogued at 15 m depth, deployed to monitor ocean currents in the Gulf of America in support of NOAA’s response to the Deepwater Horizon oil spill. Data source: Drifter Data Assembly Center (DAC), and Global Telecommunication System (GTS)

Simulated Flow Trajectories

Why are they helpful?

Numerical simulations of flow trajectories show how ocean currents spread particles released from a given location. These simulations are based on satellite observations or numerical simulations of ocean surface currents. The spreading of these particles approximates how oil will act below the ocean surface, where the effect of wind and sunlight are not that important, compared with the surface where discrepancies between these simulations and the spreading of oil are possible.

Lagrangian Coherent Structures

The map to the right shows an animation of the evolution of surface water particles (in black) released daily at the Deepwater Horizon location, overlaid on the finite-time Lyapunov exponent field (FTLE) for the corresponding date. Bands of most intense red tones indicate attracting Lagrangian Coherent Structures (LCS), which act as barriers for the moving particles. Consistent with this, please note that in these animations, the distribution of the simulated particles closely follow the deformation of the LCS over time. The velocity field used for these simulations were daily outputs of the IASNFS NCOM model (Navy Coastal Ocean Model). These maps are only available for the period of the oil spill.

Fieldwork & Research Cruises

Scientists from AOML’s Ocean Chemistry & Ecosystems and Physical Oceanography Divisions participated in a number of research cruises, conferences, and provided substantial scientific support for NOAA’s response to the Deepwater Horizon oil spill.  AOML also supplied instrumentation for NOAA vessels, quality control for Winkler titrations needed to calibrate oxygen sensors, and contributed to studies of oil distribution in beach and coral reef regions of Florida.  

Working with colleagues from EPA, NOAA-ORR, the University of South Florida, Louisiana State University, Canada’s Dept. of Fisheries and Oceans, the Alliance for Coastal Technology, Dalhousie University, the Oil Spill Recovery Institute, and several corporations, former Ocean Chemistry and Ecosystems Director Michelle Wood organized a study at DFO’s Center for Offshore Oil and Gas Energy Research to evaluate the sensitivity and linearity of response for different flourometers used to detect subsurface oil during the Deepwater Horizon event. 

RV Endeavor as viewed from a small boat. Image credit: NOAA
RV Endeavor as viewed from a small boat. Image credit: NOAA

Dr. Michelle Wood, Director of AOML’s Ocean Chemistry and Ecosystems Division was Chief Scientist and Mr. Charles Featherstone of the Ocean Chemistry and Ecosystems Division provided scientific support in the R/V Walton Smith Deepwater Horizon Cruise, June 6 – June 10, 2010. [Mission Report/ Pictures]

Mr. Shailer Cummings of the Ocean Chemistry and EcosystemsDivision participated in the R/V Gordon Gunter Cruise, May 27 – June 4, 2010. [Mission Report]

Mr. Shailer Cummings of the Ocean Chemistry and Ecosystems Division participated in the R/V Nancy Foster Loop Current Cruise, June 30 – July 18, 2010. [Mission Report]

Dr.  Michelle Wood, Director of AOML’s Ocean Chemistry and Ecosystems Division was responsible for interpreting and managing a range of water column measurements during a leg of the R/V Seward Johnson Florida Shelf-Edge Expedition (FLoSEE) Cruise, July 9 – August 9, 2010. [Website]

Mr. George Berberian of the Ocean Chemistry and Ecosystems Division provided high-quality dissolved oxygen analyses during the R/V Ocean Veritas Deepwater Horizon Cruise #12, August 1 – August 2, 2010. [Report]

Mr. George Berberian of the Ocean Chemistry and Ecosystems Division provided high-quality dissolved oxygen analyses during the R/V Brooks McCall Deepwater Horizon Cruise #16 (Legs 1 & 2), August 4 – August 11, 2010. [Report]

Mr. Michael Shoemaker of the Ocean Chemistry and Ecosystems Division acted as trustee on the Natural Resource Damage Assessment (NRDA) Sediment Study Cruise aboard the R/V Gyre, September 14 – September 29, 2010.

Joint Analysis Group (JAG) 

Dr. Richard Wanninkhof, an AOML scientist in the Ocean Chemistry & Ecosytems Division, was an active member of the Joint Analysis Group (JAG) for Surface and Sub-Surface Oceanography, Oil and Dispersant Data since its founding shortly after the spill began. The JAG was a collaborative effort between the National Oceanic and Atmospheric Administration (NOAA), the U.S. Environmental Protection Agency (EPA) and the White House Office of Science and Technology Policy (OSTP). JAG was developed to ensure a comprehensive and coordinated analysis of the oceanographic data collected in the Gulf of America by private, federal, and academic scientists. Click the button below to view the final report from the group.

Survey area and month of station occupation for monitoring for subsurface dispersed oil.

Gulf of America Monitoring in Support of Oil Spill Effort

Oil Spill Response Workshop

The workshop was organized by NOAA/Atlantic Oceanographic and Meteorological Laboratory (AOML) and NOAA/Southeast Fisheries Science Center (SEFSC) in support of oil spill efforts. July 1-2, 2010. Miami, FL

Objectives of this workshop

a. Review the needs of the operational community and decision makers
b. Communicate current efforts to monitor the oil spill
c. Identify the short term and long term (operational and scientific) monitoring goals
d. Define how to best accomplish these monitoring goals

drifterdata

Data

Driving Innovative Science with Data

Access to data from several hydrographic cruises and flights carried out by NOAA and other institutions to monitor physical and chemical properties in the water column after the Deepwater Horizon oil spill event in 2010.

Publications & Reports

  • Publications

    Ryan, J.P., Y. Zhang, H. Thomas, E.V. Reinecker, R.K. Nelson, and S.R. Cummings. A High-resolution Survey of a Deep Hydrocarbon Plume in the Gulf of America during the 2010 Macondo Blowout. Monitoring and Modelling the Deepwater Horizon Oil Spill, pp. 63-67, 2011. Ed. by Y. Liu, A. MacFadyen, J-G. Ji and R.H. Weisburg. American Geophysical Union.

    Shay, L.K., B. Jaimes, J.K. Brewster, P. Meyers, E. Claire Caskill, E. Uhlhorn, F. Marks, G.R. Halliwell, O.M. Smedstad, and P. Hogan. Airborn Ocean Surveys of the Loop Current Complex from NOAA WP-3D in Support of the Deepwater Horizon Oil Spill. Monitoring and Modelling the Deepwater Horizon Oil Spill, pp. 131-152, 2011. Ed. by Y. Liu, A. MacFadyen, J-G. Ji and R.H. Weisburg. American Geophysical Union.  [PDF]

    Atwood, D. K., F. J. Burton, J. E. Corredor, G. R. Harvey, A. J. Mata-Jimenez, A. Vasquez-Botello, and B. A. Wade. Results of the CARIPOL Petroleum Pollution Monitoring Project in the Wider Caribbean. Marine Pollution Bulletin, Vol. 18 (10), 540-548, 1987.

    Atwood, D. K., H. H. Cummings, W. J. Nodal, and R. Culbertson. The CARIPOL Petroleum Monitoring Project and the CARIPOL Petroleum Pollution Database. Caribbean Journal of Science, Vol. 23 (1), 1-3, 1987.

    Atwood, D. K. and S. Dinkel-McKay. Floating Tar and Disssolved Dispersed Petroleum Hydrocarbons in the Northern Gulf of America and the Straits of Florida. Caribbean Journal of Science, Vol. 23 (1), 73-76, 1987.

    Atwood, D. K. and R. L. Ferguson. An Example Study of the Weathering of Spilled Petroleum in a Tropical Marine Environment: Ixtoc-1. Bulletin of Marine Science, 32(1): 1-13, 1982.

    Romero, G. C., G. R. Harvey and D. K. Atwood. Stranded Tar on Florida Beaches: September 1979 – October 1980. Marine Pollution Bulletin, Vol. 12 (8), 280-284, 1981.

    Androulidakis, Y., Kourafalou, V., Le Hénaff, M., Kang, H.-S., and Ntaganou, N., 2021: The role of mesoscale dynamics over northwestern Cuba in the Loop Current evolution in 2010, during the Deepwater Horizon incident. Journal of Marine Science and Engineering, 9(2):188 (https://doi.org/10.3390/jmse9020188).

    Hole, L.R., Dagestad, K.-F., Rohrs, J., Wettre, C., Kourafalou, V.H., Androulidakis, Y., Kang, H., Le Hénaff, M., and Garcia-Pineada, O., 2019: The DeepWater horizon oil slick: High resolution model simulations of river front effects, initialized and verified by satellite observations. Journal of Marine Science and Engineering, 7(10):329 (doi:10.3390/jmse7100329).

    Goni, G., J. Trinanes, A. MacFadyen, D. Streett, M.J. Olascoaga, M.L. Imhoff, F. Muller-Karger, and M.A. Roffer, 2015: Variability of the Deepwater Horizon surface oil spill extent and its relationship to varying ocean currents and extreme weather conditions. In Mathematical Modelling and Numerical Simulation of Oil Pollution Problems , M. Ehrhardt (ed.), Springer-Verlag, New York, 1-22, (doi:10.1007/978-3-319-16459-5_1) [PDF]

    Smith, R.H., E.M. Johns, G.J. Goni, J. Trinanes, R. Lumpkin, A.M. Wood, C.R. Kelble, S.R. Cummings, J.T. Lamkin and S. Privoznik, 2014: Oceanographic conditions in the Gulf of America in July 2010, during the Deepwater Horizon oil spill. Cont. Shelf Res., 77, 118-131. [PDF]

    Smith, R ., E. Johns , G. J. Goni , J. Trinanes , R. Lumpkin , A. M. Wood, C. R. Kelble, S. R. Cummings, J. T. Lamkin and S. Privoznik, 2013: Oceanographic conditions in the Gulf of America in July 2010, during the Deepwater Horizon oil spill. Cont. Shelf Res., 77, 118-131. [PDF]

    Srinivasan A., M. LeHenaff, V.H. Kourafalou, W.C. Thacker, N.F. Tsinoremas, J. helgers, C.B. Paris, H. Kang, M. Iskandarani, J.P. zysman and O.M. Knio, 2011: Many Task Computing for Modeling the Fate of Oil Discharged from the Deep Water Horizon Well Blowout. IEEE Xplore, doi:10.1109/MTAGS.2010.5699424, pages 1-7. [PDF]

    Harvey, G. R., A. G. Requejo, P. A. McGillivary, and J. M. Tokar. Observation of a Subsurface Oil-Rich Layer in the Open Ocean. Science, Vol. 205 (4410), 999-1001, 1979.

  • Reports