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  2. Coastal ocean dynamics applications radar - Wikipedia

    en.wikipedia.org/wiki/Coastal_ocean_dynamics...

    CODAR is a noninvasive system that can measure and map near-surface ocean currents in coastal waters. It is transportable and can produce ocean current maps on site in near real time. Moreover, using CODAR it is possible to measure wave heights and produce an indirect estimate of local wind direction.

  3. Ocean current - Wikipedia

    en.wikipedia.org/wiki/Ocean_current

    Ocean surface currents Distinctive white lines trace the flow of surface currents around the world. Visualization showing global ocean currents from January 1, 2010, to December 31, 2012, at sea level, then at 2,000 m (6,600 ft) below sea level Animation of circulation around ice shelves of Antarctica

  4. Atlantic meridional overturning circulation - Wikipedia

    en.wikipedia.org/wiki/Atlantic_meridional...

    A summary of the path of the thermohaline circulation. Blue paths represent deep-water currents, while red paths represent surface currents. The NADW is not the deepest water layer in the Atlantic Ocean; the Antarctic bottom water (AABW) is always the densest, deepest ocean layer in any basin deeper than 4,000 metres (2.5 mi). [27]

  5. Drifter (oceanography) - Wikipedia

    en.wikipedia.org/wiki/Drifter_(oceanography)

    The main type of surface drifter is the CODE drifter. The CODE drifter gets its name from the 1985 Coastal Dynamics Experiment (CODE), and it is also called a Davis drifter. [8] [9] [10] It is designed to track the wind-driven surface currents in the upper meter of oceanic mixed layer. [11]

  6. Ocean - Wikipedia

    en.wikipedia.org/wiki/Ocean

    Ocean surface currents A map of the global thermohaline circulation; blue represents deep-water currents, whereas red represents surface currents. ... and tuna live.

  7. Canary Current - Wikipedia

    en.wikipedia.org/wiki/Canary_Current

    The vertical Canary Current. The Canary Current is a wind-driven surface current that is part of the North Atlantic Gyre.This eastern boundary current branches south from the North Atlantic Current and flows southwest about as far as Senegal where it turns west and later joins the Atlantic North Equatorial Current.

  8. California Current - Wikipedia

    en.wikipedia.org/wiki/California_Current

    Additionally, extensive upwelling of colder sub-surface waters occurs, caused by the prevailing northwesterly winds acting through the Ekman Effect. The winds drive surface water to the right of the wind flow, that is offshore, which draws water up from below to replace it. The upwelling further cools the already cool California Current.

  9. Azores Current - Wikipedia

    en.wikipedia.org/wiki/Azores_Current

    The Azores current represented north of the Azores High, seen around 40°N in the map. The Azores Current is a generally eastward to southeastward-flowing ocean current in the North Atlantic Ocean. It originates near the Grand Banks of Newfoundland where the Gulf Stream splits into two branches, the northern branch becoming the North Atlantic ...

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