
Name the ocean currents and describe what happens when the hot and cold currents meet.
Answer
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Hint: The motion of ocean waters from one element to every other takes place because of the consequences of earth's rotation, wind difference, salinity and density of sea waters etc. The motion of ocean water is known as ocean current.
Complete answer:
Ocean flow derives its power at the ocean surface from sources that outline flow kinds: (1) wind-driven circulation compelled through wind stress on the ocean floor, inducing a momentum exchange, and (2) thermohaline flow pushed through the versions in water density imposed at the ocean floor through trade of ocean warmth and water with the atmosphere, inducing a buoyancy trade.
These flow kinds aren't completely independent, due to the fact that the ocean-air buoyancy and momentum trade are depending on wind speed.
Areas in which heat and cold currents meet generally tend to have normal foggy conditions, because the overlying heat and cold air come in touch with every other. They additionally generally tend to have excessive organic productivity, due to the fact plankton growth is inspired through the integration of heat and cold currents. Some of the world's maximum efficient fishing grounds are placed in which heat and cold currents converge. For example, in which Labrador current (cold) and Gulf stream (warm) meet, a dense fog is there and it's miles one of the richest fishing grounds of the world.
Note:The Ocean Currents withinside the northern hemisphere deflect toward their proper and withinside the southern hemisphere deflect toward their left because of the Coriolis force. The handiest exception to this rule of the go with the drift of ocean water is located withinside the Indian Ocean, in which the path of current go with the drift modifications with the extrade withinside the path of monsoon wind go with the drift. It is noteworthy that the cold currents are lesser in variety compared to the nice and cozy or warm current.
Complete answer:
Ocean flow derives its power at the ocean surface from sources that outline flow kinds: (1) wind-driven circulation compelled through wind stress on the ocean floor, inducing a momentum exchange, and (2) thermohaline flow pushed through the versions in water density imposed at the ocean floor through trade of ocean warmth and water with the atmosphere, inducing a buoyancy trade.
These flow kinds aren't completely independent, due to the fact that the ocean-air buoyancy and momentum trade are depending on wind speed.
Areas in which heat and cold currents meet generally tend to have normal foggy conditions, because the overlying heat and cold air come in touch with every other. They additionally generally tend to have excessive organic productivity, due to the fact plankton growth is inspired through the integration of heat and cold currents. Some of the world's maximum efficient fishing grounds are placed in which heat and cold currents converge. For example, in which Labrador current (cold) and Gulf stream (warm) meet, a dense fog is there and it's miles one of the richest fishing grounds of the world.
Note:The Ocean Currents withinside the northern hemisphere deflect toward their proper and withinside the southern hemisphere deflect toward their left because of the Coriolis force. The handiest exception to this rule of the go with the drift of ocean water is located withinside the Indian Ocean, in which the path of current go with the drift modifications with the extrade withinside the path of monsoon wind go with the drift. It is noteworthy that the cold currents are lesser in variety compared to the nice and cozy or warm current.
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