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Deep ocean water is the name for cold, salty water found deep below the surface of Earth's oceans. Deep ocean water makes up about 90% of the volume of the oceans. Deep ocean water has a very uniform temperature of around 0-3 °C. Its salinity is about 3.5% or 35 ppt (parts per thousand). [3]
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
The Atlantic meridional overturning circulation (AMOC) is the main current system in the Atlantic Ocean [1]: 2238 and is also part of the global thermohaline circulation, which connects the world's oceans with a single "conveyor belt" of continuous water exchange. [18]
The Drake is part of the most voluminous ocean current in the world, with up to 5,300 million cubic feet flowing per second. Squeezed into the narrow passage, the current increases, traveling west ...
As the temperature continues to drop, the water on the surface may get cold enough to freeze and the lake/ocean begins to ice over. A new thermocline develops where the densest water (4 °C (39 °F)) sinks to the bottom, and the less dense water (water that is approaching the freezing point) rises to the top.
The water transport in the Gulf Stream gradually increases from 30 Sv in the Florida Current to a maximum of 150 Sv south of Newfoundland at 55° W longitude. [4] The Antarctic Circumpolar Current, at approximately 125 Sv, is the largest ocean current. [5] The entire global input of fresh water from rivers to the ocean is approximately 1.2 Sv. [6]
In the southeastern United States Liriope is sometimes referred to by the common name monkey grass or spider grass. The pronunciation of "Liriope" varies. Commonly recommended pronunciation are / l ɪ ˈ r aɪ ə p i / lih-RY-ə-pee (US), [4] [5] and / l ɪəˈr iː oʊ p eɪ / leer-EE-oh-pay (British), [6] but there are many regional variations.
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