Barrier layer: Difference between revisions

From Glossary of Meteorology
imported>Perlwikibot
No edit summary
m (Rewrite with Template:Term and clean up)
 
Line 1: Line 1:
 
{{Term
 
|Display title=barrier layer
{{TermHeader}}
|Definitions={{Definition
{{TermSearch}}
|Num=1
 
|Meaning=
<div class="termentry">
The depth [[range]], where it exists, between the bottom of the [[oceanic surface mixed layer|oceanic surface mixed  layer]] and the [[thermocline]], usually at a depth between 30 and 80 m.<br/> The barrier layer is found in tropical regions where the [[mixed layer]] contains water of lower  [[salinity]] than but identical in [[temperature]] to that of the water below. Its significance is that it  acts as a barrier to the vertical penetration of [[heat]] into the ocean because, without a temperature  [[gradient]] at the bottom of the mixed layer, [[entrainment]] of water from below does not remove  any heat from the mixed layer.
  <div class="term">
}}
== barrier layer ==
}}
  </div>
 
<div class="definition"><div class="short_definition">The depth [[range]], where it exists, between the bottom of the [[oceanic surface mixed layer|oceanic surface mixed  layer]] and the [[thermocline]], usually at a depth between 30 and 80 m.</div><br/> <div class="paragraph">The barrier layer is found in tropical regions where the [[mixed layer]] contains water of lower  [[salinity]] than but identical in [[temperature]] to that of the water below. Its significance is that it  acts as a barrier to the vertical penetration of [[heat]] into the ocean because, without a temperature  [[gradient]] at the bottom of the mixed layer, [[entrainment]] of water from below does not remove  any heat from the mixed layer.</div><br/> </div>
</div>
 
{{TermIndex}}
{{TermFooter}}
 
[[Category:Terms_B]]

Latest revision as of 21:58, 13 January 2024

The depth range, where it exists, between the bottom of the oceanic surface mixed layer and the thermocline, usually at a depth between 30 and 80 m.
The barrier layer is found in tropical regions where the mixed layer contains water of lower salinity than but identical in temperature to that of the water below. Its significance is that it acts as a barrier to the vertical penetration of heat into the ocean because, without a temperature gradient at the bottom of the mixed layer, entrainment of water from below does not remove any heat from the mixed layer.


Copyright 2024 American Meteorological Society (AMS). For permission to reuse any portion of this work, please contact permissions@ametsoc.org. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act (17 U.S. Code § 107) or that satisfies the conditions specified in Section 108 of the U.S.Copyright Act (17 USC § 108) does not require AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, require written permission or a license from AMS. Additional details are provided in the AMS Copyright Policy statement.