10
views
0
recommends
+1 Recommend
0 collections
    0
    shares
      • Record: found
      • Abstract: found
      • Article: found
      Is Open Access

      Ocean convergence and the dispersion of flotsam

      research-article

      Read this article at

      Bookmark
          There is no author summary for this article yet. Authors can add summaries to their articles on ScienceOpen to make them more accessible to a non-specialist audience.

          Significance

          Ocean currents move material released on the ocean surface away from the release point and, over time, spread it over an increasingly large area. However, observations also show high concentrations of the material even after significant spreading. This work examines a mechanism for creating such concentrations: downwelling of water at the boundaries of different water masses concentrates floating material at this boundary. Hundreds of satellite-tracked drifters were released near the site of the 2010 Deepwater Horizon oil spill. Surprisingly, most of these gathered into a single cluster less than 100 m in size, dramatically demonstrating the strength of this mechanism.

          Abstract

          Floating oil, plastics, and marine organisms are continually redistributed by ocean surface currents. Prediction of their resulting distribution on the surface is a fundamental, long-standing, and practically important problem. The dominant paradigm is dispersion within the dynamical context of a nondivergent flow: objects initially close together will on average spread apart but the area of surface patches of material does not change. Although this paradigm is likely valid at mesoscales, larger than 100 km in horizontal scale, recent theoretical studies of submesoscales (less than ∼10 km) predict strong surface convergences and downwelling associated with horizontal density fronts and cyclonic vortices. Here we show that such structures can dramatically concentrate floating material. More than half of an array of ∼200 surface drifters covering ∼20 × 20 km 2 converged into a 60 × 60 m region within a week, a factor of more than 10 5 decrease in area, before slowly dispersing. As predicted, the convergence occurred at density fronts and with cyclonic vorticity. A zipperlike structure may play an important role. Cyclonic vorticity and vertical velocity reached 0.001 s −1 and 0.01 ms −1, respectively, which is much larger than usually inferred. This suggests a paradigm in which nearby objects form submesoscale clusters, and these clusters then spread apart. Together, these effects set both the overall extent and the finescale texture of a patch of floating material. Material concentrated at submesoscale convergences can create unique communities of organisms, amplify impacts of toxic material, and create opportunities to more efficiently recover such material.

          Related collections

          Most cited references19

          • Record: found
          • Abstract: not found
          • Article: not found

          Atmospheric Diffusion Shown on a Distance-Neighbour Graph

            Bookmark
            • Record: found
            • Abstract: not found
            • Article: not found

            Mesoscale to Submesoscale Transition in the California Current System. Part I: Flow Structure, Eddy Flux, and Observational Tests

              Bookmark
              • Record: found
              • Abstract: found
              • Article: found
              Is Open Access

              Submesoscale currents in the ocean

              This article is a perspective on the recently discovered realm of submesoscale currents in the ocean. They are intermediate-scale flow structures in the form of density fronts and filaments, topographic wakes and persistent coherent vortices at the surface and throughout the interior. They are created from mesoscale eddies and strong currents, and they provide a dynamical conduit for energy transfer towards microscale dissipation and diapycnal mixing. Consideration is given to their generation mechanisms, instabilities, life cycles, disruption of approximately diagnostic force balance (e.g. geostrophy), turbulent cascades, internal-wave interactions, and transport and dispersion of materials. At a fundamental level, more questions remain than answers, implicating a programme for further research.
                Bookmark

                Author and article information

                Journal
                Proc Natl Acad Sci U S A
                Proc. Natl. Acad. Sci. U.S.A
                pnas
                pnas
                PNAS
                Proceedings of the National Academy of Sciences of the United States of America
                National Academy of Sciences
                0027-8424
                1091-6490
                6 February 2018
                16 January 2018
                16 January 2018
                : 115
                : 6
                : 1162-1167
                Affiliations
                [1] aSchool of Oceanography, College of the Environment, University of Washington , Seattle, WA 98105;
                [2] bApplied Physics Laboratory, University of Washington , Seattle, WA 98105;
                [3] cSchool of Earth and Ocean Sciences, University of Victoria , Victoria, BC, Canada, V8W 3P6;
                [4] dDepartment of Physics and Astronomy, University of Victoria , Victoria, BC, Canada, V8W 3P6;
                [5] eDepartment of Atmospheric and Oceanic Sciences, University of California , Los Angeles, CA 90095;
                [6] fRosenstiel School of Marine and Atmospheric Sciences, University of Miami , Miami, FL 33149;
                [7] gNaval Research Laboratory, Stennis Space Center , MS 39529;
                [8] hSchool of Marine Science and Policy, College of Earth, Ocean and Environment, University of Delaware , Newark, DE 19716;
                [9] iLamont-Doherty Earth Observatory, Earth Institute, Columbia University , Palisades, NY 10964;
                [10] jDepartment of Atmospheric Sciences, College of the Environment, University of Washington , Seattle, WA 98195;
                [11] kMesoscale and Microscale Meteorology Laboratory, National Center for Atmospheric Research , Boulder, CO 80307;
                [12] lDepartment of Mathematics, College of Staten Island , Staten Island, NY 10314
                Author notes
                1To whom correspondence should be addressed. Email: dasaro@ 123456apl.washington.edu .

                Contributed by Eric A. D’Asaro, December 11, 2017 (sent for review October 25, 2017; reviewed by Thomas Farrar and Patrice Klein)

                Author contributions: E.A.D., G.N., B.K.H., G.A.J., H.S.H., J.C.M., R.B., A.D.K., A.C.P., and T.M.Ö. designed research; E.A.D., A.Y.S., J.M.K., J.M., G.N., C.M.G., A.C.H., B.K.H., E.H.R., G.A.J., N.J.M.L., S.C., F.J., and T.M.Ö. performed research; E.A.D., A.Y.S., G.N., C.M.G., B.K.H., G.A.J., and S.C. contributed new reagents/analytic tools; E.A.D., A.Y.S., J.M., A.C.H., E.H.R., G.A.J., H.S.H., N.J.M.L., F.J., and R.B. analyzed data; and E.A.D. and J.M. wrote the paper.

                Reviewers: T.F., Woods Hole Oceanographic Institution; and P.K., IFREMER and CNRS.

                Author information
                http://orcid.org/0000-0002-8453-854X
                http://orcid.org/0000-0001-9560-7304
                http://orcid.org/0000-0002-0373-9236
                http://orcid.org/0000-0001-7710-9862
                Article
                201718453
                10.1073/pnas.1718453115
                5819445
                29339497
                a4839d83-86d3-49fc-8d44-3154aaa19db3
                Copyright © 2018 the Author(s). Published by PNAS.

                This open access article is distributed under Creative Commons Attribution-NonCommercial-NoDerivatives License 4.0 (CC BY-NC-ND).

                History
                Page count
                Pages: 6
                Funding
                Funded by: Gulf of Mexico Research Initiative (GoMRI) 100007240
                Award ID: GoMRI SA-1515
                Categories
                Physical Sciences
                Earth, Atmospheric, and Planetary Sciences

                ocean,submesoscale,dispersion,eddy,vertical velocity
                ocean, submesoscale, dispersion, eddy, vertical velocity

                Comments

                Comment on this article