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<!DOCTYPE article SYSTEM "http://www.nonlin-processes-geophys.net/inc/npg/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Nonlinear Processes  in Geophysics</journal_title>
		<journal_url>www.nonlin-processes-geophys.net</journal_url>
		<issn>1023-5809</issn>
		<eissn>1607-7946</eissn>
		<volume_number>2</volume_number>
		<issue_number>3/4</issue_number>
		<publication_year>1995</publication_year>
	</journal>
	<doi>10.5194/npg-2-206-1995</doi>
	<article_url>http://www.nonlin-processes-geophys.net/2/206/1995/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/2/206/1995/npg-2-206-1995.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/2/206/1995/npg-2-206-1995.pdf</fulltext_pdf>
	<start_page>206</start_page>
	<end_page>221</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">Non-equilibrium effects of core-cooling and time-dependent internal heating on mantle flush events</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>D. A. Yuen</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>S. Balachandar</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>V. C. Steinbach</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>S. Honda</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>D. M. Reuteler</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>J. J. Smedsmo</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>G. S. Lauer</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Dept. Geology, Geophysics and Minnesota Supercomputer Inst., Univ. of Minnesota, Minneapolis, MN 55415-1227, USA</affiliation>
		<affiliation numeration="2" content_type="html">Dept. of Theretical and Applied Mechanics, University of Illinois, Urbana, IL 61801, USA</affiliation>
		<affiliation numeration="3" content_type="html">Inst. für Geophysik und Meteorologie, Universität zu Köln, 60923 Köln, Germany</affiliation>
		<affiliation numeration="4" content_type="html">Dept. of Earth and Planetary Systems Science, Faculty of Science, University of Hiroshima, Higashi-Hiroshima 739, Japan</affiliation>
	</affiliations>
	<abstract content_type="html">We have examined the non-equilibrium effects of core-cooling
and time-dependent internal-heating on the thermal evolution of the Earth&apos;s mantle and on
mantle flush events caused by the two major phase transitions. Both two- and
three-dimensional models have been employed. The mantle viscosity responds to the secular
cooling through changes in the averaged temperature field. A viscosity which decreases
algebraically with the average temperature has been considered. The time-dependent
internal-heating is prescribed to decrease exponentially with a single decay time. We have
studied the thermal histories with initial Rayleigh numbers between 2 x 10&lt;sup&gt;7&lt;/sup&gt; and
10&lt;sup&gt;8&lt;/sup&gt; .
Flush events, driven by the non-equilibrium forcings, are much more dramatic than those
produced by the equilibrium boundary conditions and constant internal heating. Multiple
flush events are found under non-equilibrium conditions in which there is very little
internal heating or very fast decay rates of internal-heating. Otherwise, the flush events
take place in a relatively continuous fashion. Prior to massive flush events small-scale
percolative structures appear in the 3D temperature fields. Time-dependent signatures,
such as the surface heat flux, also exhibits high frequency oscillatory patterns prior to
massive flush events. These two observations suggest that the flush event may be a
self-organized critical phenomenon. The Nusselt number as a function of the time-varying
Ra does not follow the Nusselt vs. Rayleigh number power-law relationship based on
equilibrium (constant temperature) boundary conditions. Instead &lt;i&gt;Nu(t) &lt;/i&gt; may vary
non-monotonically with time because of the mantle flush events. Convective processes in
the mantle operate quite differently under non-equilibrium conditions from its
behaviour under the usual equilibrium situations.</abstract>
	<references>
	</references>
</article>

