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Currents, Gyres, Eddies - Woods Hole Oceanographic Institution How the Ocean Works Diving in Eddies How the Ocean Works Following the Eddies How the Ocean Works Of Wings, Waves, and Winds “Great albatross! The meanest birds Spring up and flit away, While thou must toil to…
The Oceans Have Their Own Weather Systems - Woods Hole Oceanographic . . . The largest eddies can contain up to 1,200 cubic miles (5,000 cubic kilometers) of water and can last for months to a year Earth’s rotation—the Coriolis force—gives eddies their spin To hunt for their target, McGillicuddy and colleagues used data from satellites, whose measurements of sea surface heights show telltale signs of eddies
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
Warm Eddies in a Cold Sea - Woods Hole Oceanographic Institution Warm Eddies in a Cold Sea Animation by Jack Cook, Kate Madin :: Originally published online November 30, 2007 Save to resources More Content From : How the Ocean Works Video Multimedia | Mid-ocean Ridges Jason to the Rescue Video Multimedia | Biological Carbon Pump Climate Hero: The Ocean’s Super-Powered Carbon Pump Virtual Series Multimedia
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 ()
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
Satellite observations of chlorophyll, phytoplankton biomass, and Ekman . . . Eddies originating in the eastern South Indian Ocean are unique in that anticyclones, typically associated with downwelling, contain elevated levels of chlorophyll-a, enhanced primary production and phytoplankton communities generally associated with nutrient-replete environments
A Warm Eddy Swirling in the Cold Labrador Sea Eddies can maintain their integrity for long distances—in this case, carrying cargoes of warm water from a warm current flowing around Greenland into the cold Labrador Sea We know very little about these eddies, but we think they play an important role in the circulation of the Labrador Sea, and perhaps the whole Atlantic Ocean