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  2. Kuroshio Current - Wikipedia

    en.wikipedia.org/wiki/Kuroshio_Current

    Kuroshio Current

  3. Fish or cut bait - Wikipedia

    en.wikipedia.org/wiki/Fish_or_cut_bait

    Fish or cut bait

  4. Ocean current - Wikipedia

    en.wikipedia.org/wiki/Ocean_current

    Ocean current - Wikipedia ... Ocean current

  5. Gulf Stream - Wikipedia

    en.wikipedia.org/wiki/Gulf_Stream

    Gulf Stream - Wikipedia ... Gulf Stream

  6. Juan de Fuca Channel - Wikipedia

    en.wikipedia.org/wiki/Juan_de_Fuca_Channel

    At 150 metres (500 ft) below the surface, water has flowed as fast as 0.40 metres per second (1.3 ft/s), showing mixing up to 1,000 times the normal rate in the deep ocean. The flow is hydraulically-controlled, which means it flows smoothly over a shallow ridge just off Cape Flattery then on the other side forms a turbulent breaking undersea ...

  7. Slack tide - Wikipedia

    en.wikipedia.org/wiki/Slack_tide

    Slack tide or slack water is the short period in a body of tidal water when the water is completely unstressed, and there is no movement either way in the tidal stream. It occurs before the direction of the tidal stream reverses. [1] Slack water can be estimated using a tidal atlas or the tidal diamond information on a nautical chart. [2]

  8. Mediterranean outflow - Wikipedia

    en.wikipedia.org/wiki/Mediterranean_outflow

    Black arrows show the two different branches of the outflow. The Mediterranean Outflow is a current flowing from the Mediterranean Sea towards the Atlantic Ocean through the Strait of Gibraltar. Once it has reached the western side of the Strait of Gibraltar, it divides into two branches, one flowing westward following the Iberian continental ...

  9. Water table - Wikipedia

    en.wikipedia.org/wiki/Water_table

    The water table is the upper surface of the zone of saturation. The zone of saturation is where the pores and fractures of the ground are saturated with groundwater, [1] which may be fresh, saline, or brackish, depending on the locality. It can also be simply explained as the depth below which the ground is saturated.