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<front>
<journal-meta>
<journal-id journal-id-type="publisher">OS</journal-id>
<journal-title-group>
<journal-title>Ocean Science</journal-title>
<abbrev-journal-title abbrev-type="publisher">OS</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Ocean Sci.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1812-0792</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/os-5-271-2009</article-id>
<title-group>
<article-title>Understanding mixing efficiency in the oceans: do the nonlinearities of the equation of state for seawater matter?</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Tailleux</surname>
<given-names>R.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Meteorology, University of Reading, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>20</day>
<month>07</month>
<year>2009</year>
</pub-date>
<volume>5</volume>
<issue>3</issue>
<fpage>271</fpage>
<lpage>283</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2009 R. Tailleux</copyright-statement>
<copyright-year>2009</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
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<self-uri xlink:href="https://os.copernicus.org/articles/5/271/2009/os-5-271-2009.pdf">The full text article is available as a PDF file from https://os.copernicus.org/articles/5/271/2009/os-5-271-2009.pdf</self-uri>
<abstract>
<p>There exist two central measures of turbulent mixing in
turbulent stratified fluids that are both caused by molecular diffusion:
1) the dissipation rate &lt;i&gt;D&lt;/i&gt;(APE) of available potential energy APE;
2) the turbulent rate of change &lt;i&gt;W&lt;/i&gt;&lt;sub&gt;&lt;i&gt;r&lt;/i&gt;, turbulent&lt;/sub&gt; of background gravitational
potential energy GPE&lt;sub&gt;&lt;i&gt;r&lt;/i&gt;&lt;/sub&gt;. So far, these two quantities have often been
regarded as the same energy conversion, namely the irreversible conversion
of APE into GPE&lt;sub&gt;&lt;i&gt;r&lt;/i&gt;&lt;/sub&gt;, owing to the well known exact equality &lt;i&gt;D&lt;/i&gt;(APE)=&lt;i&gt;W&lt;/i&gt;&lt;sub&gt;&lt;i&gt;r&lt;/i&gt;, turbulent&lt;/sub&gt;
for a Boussinesq fluid with a linear equation of state.
Recently, however, Tailleux (2009) pointed out that the above equality
no longer holds for a thermally-stratified compressible, with the ratio
&amp;xi;=&lt;i&gt;W&lt;/i&gt;&lt;sub&gt;&lt;i&gt;r&lt;/i&gt;, turbulent&lt;/sub&gt;/&lt;i&gt;D&lt;/i&gt;(APE) being generally lower than unity
and sometimes even negative for water or seawater, and argued that &lt;i&gt;D&lt;/i&gt;(APE)
and &lt;i&gt;W&lt;/i&gt;&lt;sub&gt;&lt;i&gt;r&lt;/i&gt;, turbulent&lt;/sub&gt; actually represent two distinct types of energy
conversion, respectively the dissipation of APE into one particular subcomponent
of internal energy called the &quot;dead&quot; internal energy IE&lt;sub&gt;0&lt;/sub&gt;, and the conversion
between GPE&lt;sub&gt;&lt;i&gt;r&lt;/i&gt;&lt;/sub&gt; and a different subcomponent of internal energy called
&quot;exergy&quot; IE&lt;sub&gt;exergy&lt;/sub&gt;. In this paper, the behaviour of the
ratio ξ is examined
for different stratifications having all the same buoyancy frequency
&lt;i&gt;N&lt;/i&gt; vertical profile, but different vertical profiles of the parameter
&amp;Upsilon;=&amp;alpha; &lt;i&gt;P&lt;/i&gt;/(&amp;rho;&lt;i&gt;C&lt;sub&gt;p&lt;/sub&gt;&lt;/i&gt;),
where α is the thermal expansion coefficient, &lt;i&gt;P&lt;/i&gt; the
hydrostatic pressure, &amp;rho; the density, and &lt;i&gt;C&lt;sub&gt;p&lt;/sub&gt;&lt;/i&gt; the specific heat capacity
at constant pressure, the equation
of state being that for seawater for different particular constant values of salinity.
It is found that ξ and &lt;i&gt;W&lt;/i&gt;&lt;sub&gt;&lt;i&gt;r&lt;/i&gt;, turbulent&lt;/sub&gt; depend critically on the sign
and magnitude of &lt;i&gt;d&lt;/i&gt;&amp;Upsilon;/&lt;i&gt;dz&lt;/i&gt;, in contrast with &lt;i&gt;D&lt;/i&gt;(APE), which appears largely
unaffected by the latter. These results have important consequences for how
the mixing efficiency should be defined and measured in practice, which are
discussed.</p>
</abstract>
<counts><page-count count="13"/></counts>
</article-meta>
</front>
<body/>
<back>
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