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bottom water

   Also found in: Wikipedia 0.03 sec.

bottom water

Lowermost layer of ocean water that can be distinguished by its characteristic low temperature, high density, and low oxygen content compared with surface waters. Most bottom waters are formed near Antarctica during the southern winter. The partial freezing of seawater over the Antarctic continental shelf produces salt-free ice and residual brine with a high density, which causes it to sink; it then flows northward along the seafloor. The Arctic Ocean is less important as a source of bottom water because it is isolated by barriers such as the Bering Sill and submarine ridges and banks between Greenland and the British Isles.


bottom water [′bäd·əm ‚wȯd·ər]
(hydrology)
Water lying beneath oil or gas in productive formations.
(oceanography)
The water mass at the deepest part of a water column in the ocean.


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[ILLUSTRATION OMITTED] This cold bottom water washing up on east Florida beaches originated in Antarctica.
Darwin's mechanism would suggest that they drag some of the colder, heavier bottom water up with them toward warmer, lighter water at the top.
The dead zone, more properly known as the Gulf's hypoxic zone, is an area in which the levels of oxygen in the water are too low to support most aquatic life in bottom and near bottom water, causing fish to leave the area and killing bottom-dwelling organisms that cannot leave.
 
 
 
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