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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ESDD</journal-id>
<journal-title-group>
<journal-title>Earth System Dynamics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ESDD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Earth Syst. Dynam. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">2190-4995</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/esdd-2-241-2011</article-id>
<title-group>
<article-title>Climate change, in the framework of the constructal law</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Clausse</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Meunier</surname>
<given-names>F.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Reis</surname>
<given-names>A. H.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bejan</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Laboratory of Chemical Engineering applied to Environment, Energy and Health (LGP2ES-EA21), Conservatoire National des Art et Metiers (CNAM), case 331, 292, rue St Martin, 75141 Paris Cedex 03, France</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Physics and Evora Geophysics Centre, University of Évora, Ramalho, 59, 7000-67 1 Evora, Portugal</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Mechanical Engineering, Duke University, Durham, NC 27708-0300, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>07</day>
<month>03</month>
<year>2011</year>
</pub-date>
<volume>2</volume>
<issue>1</issue>
<fpage>241</fpage>
<lpage>270</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2011 M. Clausse et al.</copyright-statement>
<copyright-year>2011</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>
<self-uri xlink:href="https://esd.copernicus.org/preprints/2/241/2011/esdd-2-241-2011.html">This article is available from https://esd.copernicus.org/preprints/2/241/2011/esdd-2-241-2011.html</self-uri>
<self-uri xlink:href="https://esd.copernicus.org/preprints/2/241/2011/esdd-2-241-2011.pdf">The full text article is available as a PDF file from https://esd.copernicus.org/preprints/2/241/2011/esdd-2-241-2011.pdf</self-uri>
<abstract>
<p>Here we present a simple and transparent alternative to the complex models
of Earth thermal behavior under time-changing conditions. We show the
one-to-one relationship between changes in atmospheric properties and
time-dependent changes in temperature and its distribution on Earth. The
model accounts for convection and radiation, thermal inertia and changes in
albedo (&amp;rho;) and greenhouse factor (γ). The constructal law is
used as the principle that governs the evolution of flow configuration in
time, and provides closure for the equations that describe the model. In the
first part of the paper, the predictions are tested against the current
thermal state of Earth. Next, the model showed that for two time-dependent
scenarios, (&amp;delta;&amp;rho; = 0.002; &amp;delta;&amp;gamma; = 0.011) and
(&amp;delta;&amp;rho; = 0.002; &amp;delta;&amp;gamma; = 0.005) the predicted
equatorial and polar temperature increases and the time scales are
(&amp;Delta;&lt;i&gt;T&lt;/i&gt;&lt;sub&gt;H&lt;/sub&gt; = 1.16 K; &amp;Delta;&lt;i&gt;T&lt;/i&gt;&lt;sub&gt;L&lt;/sub&gt; = 1.11 K; 104 years)
and (0.41 K; 0.41 K; 57 years), respectively. In the second part, a continuous model of
temperature variation was used to predict the thermal response of the
Earth&apos;s surface for changes bounded by &amp;delta;&amp;rho; = &amp;delta;&amp;gamma;
and &amp;delta;&amp;rho; = &amp;minus;&amp;delta;&amp;gamma;. The results
show that the global warming amplitudes and time scales are consistent with
those obtained for &amp;delta;&amp;rho; = 0.002 and &amp;delta;&amp;gamma; = 0.005.
The poleward heat current reaches its maximum in the vicinity of 35°
latitude, accounting for the position of the Ferrel cell between the Hadley
and Polar Cells.</p>
</abstract>
<counts><page-count count="30"/></counts>
</article-meta>
</front>
<body/>
<back>
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