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	<title>Self-Organized Criticality in SD - Revision history</title>
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	<updated>2026-04-21T22:05:35Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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		<id>http://openworld.existencia.org:80/index.php?title=Self-Organized_Criticality_in_SD&amp;diff=130&amp;oldid=prev</id>
		<title>Jrising at 16:19, 13 April 2012</title>
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		<updated>2012-04-13T16:19:29Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;Typically, coupling two models (say, climate and oceans) requires that both be recalibrated, often with parameter values that are not internally reasonable.  I&amp;#039;d like to find another option.&lt;br /&gt;
&lt;br /&gt;
My approach is to consider {X_i} to be an underlying &amp;quot;true&amp;quot; process, which is passed through a parallel collection of noisy channels, which are the models.  The goal is uncover an estimate of each X_i.  X_i may not be encoded before being passed through the channel.&lt;br /&gt;
&lt;br /&gt;
If the X_i and Z_i errors are independent, the solution might just be an average or a maximum likelihood.  But what if the Z_i&amp;#039;s are correlated?  Suppose that the {X_i} come from a Gauss-Markov process with unknown coefficients-- can the coefficients be simultaneously estimated?  Suppose that something is known about the power spectrum of X-- how can that be used?  The entropy rate is a function of the spectrum, and determines the error bounds on the estimates of X_i, but what is that best estimate?&lt;/div&gt;</summary>
		<author><name>Jrising</name></author>
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