S-MODE: The Sub-Mesoscale Ocean Dynamics Experiment
Creators
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Farrar, J. Thomas1
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D'Asaro, Eric2
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Rodríguez, Ernesto3
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Shcherbina, Andrey2
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Lenain, Luc4
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Omand, Melissa5
- Wineteer, Alex3
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Bhuyan, Paban6
- Bingham, Fred7
- Villas Boas, A. B.8
- Czech, Erin9
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D'Addezio, Joseph10
- Freilich, Mara11
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Grare, Laurent4
- Hypolite, Delphine12
- Jacobs, Gregg10
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Klein, Patrice3
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Lang, Sarah5
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Leyba, Inés M.13
- Li, Zhijin12
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Mahadevan, Amala1
- McWilliams, James12
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Menemenlis, Dimitris3
- Middleton, Leo1
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Molemaker, Jeroen12
- O'Neill, Larry13
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Perkovic-Martin, Dragana3
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Pizzo, Nick5
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Rainville, Luc2
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Rocha, Cesar14
- Samelson, R. M.13
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Simoes-Sousa, Iury1
- Statom, Nick4
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Thompson, Andrew15
- Thompson, David3
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Torres, Hector3
- Uchoa, Igor16
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Wenegrat, Jacob16
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Westbrook, Elizabeth7
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1.
Woods Hole Oceanographic Institution
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2.
University of Washington Applied Physics Laboratory
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3.
Jet Propulsion Lab
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Scripps Institution of Oceanography
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5.
University of Rhode Island
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6.
University of Connecticut
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7.
University of North Carolina Wilmington
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Colorado School of Mines
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9.
Ames Research Center
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Stennis Space Center
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Brown University
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University of California, Los Angeles
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Oregon State University
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14.
Universidade de São Paulo
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California Institute of Technology
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16.
University of Maryland, College Park
Abstract
The Sub-Mesoscale Ocean Dynamics Experiment (S-MODE) is a NASA Earth Ventures Suborbital investigation designed to test the hypothesis that oceanic frontogenesis and the kilometer-scale ("submesoscale") instabilities that accompany it make important contributions to vertical exchange of climate and biological variables in the upper ocean. These processes have been difficult to resolve in observations, making model validation challenging. A necessary step toward testing the hypothesis was to make accurate measurements of upper-ocean velocity fields over a broad range of scales and to relate them to the observed variability of vertical transport and surface forcing. A further goal was to examine the relationship between surface velocity, temperature, and chlorophyll measured by remote sensing and their depth-dependent distributions, within and beneath the surface boundary layer. To achieve these goals, we used aircraft-based remote sensing, satellite remote sensing, ships, drifter deployments, and a fleet of autonomous vehicles. The observational component of S-MODE consisted of three campaigns, all conducted in the Pacific Ocean approximately 100-km west of San Francisco during 2021–23 fall and spring. S-MODE was enabled by recent developments in remote sensing technology that allowed operational airborne observation of ocean surface velocity fields and by advances in autonomous instrumentation that allowed coordinated sampling with dozens of uncrewed vehicles at sea. The coordinated use of remote sensing measurements from three aircraft with arrays of remotely operated vehicles and other in situ measurements is a major novelty of S-MODE. All S-MODE data are freely available, and their use is encouraged.
Copyright and License
© 2025 American Meteorological Society. This published article is licensed under the terms of the default AMS reuse license.
Acknowledgement
This work is a contribution to the S-MODE project, an EVS-3 Investigation awarded under NASA Research Announcement NNH17ZDA001N-EVS3. The success of the S-MODE field campaigns required the dedicated efforts of more than 100 people who supported the data collection at sea and in the air. We thank the captains and crews of the R/V Oceanus, M/V Bold Horizon, and R/V Sally Ride and the pilots and ground crew of the NASA Armstrong B200, the NASA Langley Gulfstream III, and the Twin Otter International aircraft. We thank the staff of the Earth Science Project Office at the NASA Ames Research Center for facilitating many aspects of the project, including the aircraft operations at Ames. We thank two anonymous reviewers for helpful suggestions, and we thank Professor Christine Gommenginger for an extensive and constructive review that substantially improved the manuscript.
Data Availability
All of the S-MODE data are freely available at https://podaac.jpl.nasa.gov/S-MODE or at the DOIs listed in Table 2. The satellite sea surface temperature data shown in Figs. 5 and 7 are available at https://doi.org/10.5067/GHVRS-2PO28 and https://doi.org/10.5067/GHV20-2PO28. The computational code to reproduce Fig. 10 is available through Simoes-Sousa (2024).
Additional details
Related works
- Is supplemented by
- Software: 10.5281/zenodo.13942622 (DOI)
Funding
- National Aeronautics and Space Administration
- NNH17ZDA001N-EVS3
Dates
- Submitted
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2023-07-14
- Accepted
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2025-01-21
- Available
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2025-04-25Published online