Atlantic Ocean
The Atlantic Ocean is Earth's second-largest ocean, covering approximately one-fifth of its surface. The ocean's name, derived from Greek mythology, means the "Sea of Atlas".
Water characteristics
The salinity of the surface waters in the open ocean ranges from 33 to 37 parts per thousand by mass and varies with latitude and season. Although the minimum salinity values are found just north of the equator, in general the lowest values are in the high latitudes and along coasts where large rivers flow into the ocean. Maximum salinity values occur at about 25° north latitude. Surface salinity values are influenced by evaporation, precipitation, river inflow, and melting of sea ice.
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Surface water temperatures, which vary with latitude, current systems, and season and reflect the latitudinal distribution of solar energy, range from less than ?2 °C to 29 °C (28 °F to 84 °F). Maximum temperatures occur north of the equator, and minimum values are found in the polar regions. In the middle latitudes, the area of maximum temperature variations, values may vary by 7 °C to 8 °C (13 °F to 15 °F).
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The Atlantic Ocean consists of four major water masses. The North and South Atlantic central waters constitute the surface waters. The sub-Antarctic intermediate water extends to depths of 1,000 m (3,300 ft). The North Atlantic deep water reaches depths of as much as 4,000 m (13,200 ft). The Antarctic bottom water occupies ocean basins at depths greater than 4,000 m (13,200 ft).
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Within the North Atlantic, ocean currents isolate a large elongated body of water known as the Sargasso Sea, in which the salinity is noticeably higher than average. The Sargasso Sea contains large amounts of seaweed, and is also the spawning ground for the European eel.
Related Topics:
Sargasso Sea - Seaweed - European eel
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Due to the Coriolis effect, water in the North Atlantic circulates in a clockwise direction, whereas water circulation in the South Atlantic is counter clockwise. The South tides in the Atlantic Ocean are semi-diurnal; that is, two high tides occur during each 24 lunar hours. The tides are a general wave that moves from south to north. In latitudes above 40° north some east-west oscillation occurs.
Related Topics:
Coriolis effect - Tide - Diurnal
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~ Table of Content ~
| ► | Introduction |
| ► | Ocean bottom |
| ► | Water characteristics |
| ► | Climate |
| ► | History and economy |
| ► | Terrain |
| ► | Current environmental issues |
| ► | Notes on geography |
| ► | Ports and harbours |
| ► | External links |
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