Labrador sea water: Difference between revisions

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<div class="definition"><div class="short_definition">The last [[water mass]] to contribute to the formation of [[North Atlantic Deep  Water]] before it enters the southward path of the [[ocean conveyor belt]].</div><br/> <div class="paragraph">It occupies the central Labrador Sea with temperatures of 3.0&deg;&ndash;3.6&deg;C, [[salinities]] of 34.86&ndash;34.96  [[psu]], and consistently high oxygen content.</div><br/> </div>
<div class="definition"><div class="short_definition">The last [[water mass]] to contribute to the formation of [[North Atlantic Deep  Water]] before it enters the southward path of the [[ocean conveyor belt]].</div><br/> <div class="paragraph">It occupies the central Labrador Sea with temperatures of 3.0&#x000b0;&ndash;3.6&#x000b0;C, [[salinities]] of 34.86&ndash;34.96  [[psu]], and consistently high oxygen content.</div><br/> </div>
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Revision as of 14:33, 20 February 2012



Labrador Sea Water

The last water mass to contribute to the formation of North Atlantic Deep Water before it enters the southward path of the ocean conveyor belt.

It occupies the central Labrador Sea with temperatures of 3.0°–3.6°C, salinities of 34.86–34.96 psu, and consistently high oxygen content.


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