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  • Currents, Gyres, Eddies - Woods Hole Oceanographic Institution
    At the surface and beneath, currents, gyres and eddies physically shape the coasts and ocean bottom, and transport and mix energy, chemicals, within and among ocean basins
  • Sharks ride eddies to the depths - Woods Hole Oceanographic Institution
    White sharks in the open ocean seem to seek out eddies for a surprising reason: The eddies offer a beeline to a banquet of food
  • Eddies Found to be Deep, Powerful Modes of Ocean Transport
    April 28, 2011 Researchers from Woods Hole Oceanographic Institution (WHOI) and their colleagues have discovered that massive, swirling ocean eddies–known to be up to 500 kilometers across at the surface–can reach all the way to the ocean bottom at mid-ocean ridges, some 2,500 meters deep, transporting tiny sea creatures, chemicals, and heat from hydrothermal vents over large distances
  • Ocean Circulation - Woods Hole Oceanographic Institution
    Swirling parcels of water, called ocean eddies, spin off from the warm Gulf Stream, the powerful northward-flowing current that hugs the U S East Coast This visualization was generated by a numerical model that simulates ocean circulation
  • WHOI Arctic Group | Projects | Eddies
    Eddies in the Beaufort Gyre Associate Scientist, WHOI Supported by: This project used observations of velocity in the western Arctic pycnocline (25-300~m depth) made with Acoustic Doppler Current Profilers (ADCPs) to investigate the distribution and properties of subsurface eddies The ADCPs were deployed on autonomous drifters called, , that were frozen into the pack ice ()
  • Ocean eddies transporting plankton throughout the water column
    Plankton help reduce atmospheric carbon dioxide by using it to grow Larger particles sink to store carbon, while scientists study how smaller particles might also descend
  • Eddies in the Canada Basin, Arctic Ocean, Observed from Ice-Tethered . . .
    Five ice-tethered profilers (ITPs), deployed between 2004 and 2006, have provided detailed potential temperature and salinity S profiles from 21 anticyclonic eddy encounters in the central Canada Basin of the Arctic Ocean The 12–35-m-thick eddies have center depths between 42 and 69 m in the Arctic halocline, and are shallower and less dense than the majority of eddies observed previously
  • The Influence of Nonlinear Mesoscale Eddies on Near-Surface Oceanic . . .
    he eddies consists of dipoles with extrema out-side of the eddy cores, rather than monopoles of positive or neg tive CHL anomalies trapped at the eddy centers Monopole structures with very active physical-biological interaction are some-times observed within eddy cores In contrast to the ubiquitous presence of rotational advec-tion around the
  • Currents, Gyres, Eddies - Woods Hole Oceanographic Institution
    WHOI scientists are exploring an experimental technique to track the complex movements of water in the oceans using harmless fluorescent dyes and airplanes equipped with Light Detection and Ranging instruments To detect motion, LIDAR uses pulses of laser light, which cause the flowing dye to fluoresce
  • Experimental Observations of Baroclinic Eddies on a Sloping Bottom
    The oceanic eddies have a by Mory[1983, 1985], and Mory et al [1987] indicated that number of features that arecharacteristic of isolated eddies similareddies can be produced in a laboratoryturntable ex-and not characteristic of solitarywaves such as stronglo- periment but they possessed qualitative differences from the cal circulation, closed





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