Antarctic intermediate water: Difference between revisions

Revision as of 16:30, 7 November 2023

A water mass identified by a salinity minimum found at depths between 700 and 1000 m in the Southern Hemisphere.
It is formed at various locations along the Antarctic Polar Front and through deep winter convection east of southern Chile and south of the Great Australian Bight. It enters all oceans with the Antarctic Circumpolar Current and spreads toward the equator between the central water and the deep water.

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+{{Term
+|Display title=Antarctic Intermediate Water
-{{TermHeader}}
+|Definitions={{Definition
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+|Num=1
+|Meaning=
-<div class="termentry">
+A [[water mass]] identified by a [[salinity]] minimum found at depths  between 700 and 1000 m in the Southern Hemisphere.<br/> It is formed at various locations along the [[Antarctic Polar Front]] and through deep winter  convection east of southern Chile and south of the Great Australian Bight. It enters all oceans  with the [[Antarctic Circumpolar Current]] and spreads toward the [[equator]] between the [[central water|central  water]] and the [[deep water]].
-  <div class="term">
+}}
-== Antarctic Intermediate Water ==
+}}
-  </div>
-<div class="definition"><div class="short_definition">A [[water mass]] identified by a [[salinity]] minimum found at depths  between 700 and 1000 m in the Southern Hemisphere.</div><br/> <div class="paragraph">It is formed at various locations along the [[Antarctic Polar Front]] and through deep winter  convection east of southern Chile and south of the Great Australian Bight. It enters all oceans  with the [[Antarctic Circumpolar Current]] and spreads toward the [[equator]] between the [[central water|central  water]] and the [[deep water]].</div><br/> </div>
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-[[Category:Terms_A]]