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	<title>Comments on: Waiting for HadCRUT</title>
	<atom:link href="http://wattsupwiththat.com/2008/06/11/waiting-for-hadcrut/feed/" rel="self" type="application/rss+xml" />
	<link>http://wattsupwiththat.com/2008/06/11/waiting-for-hadcrut/</link>
	<description>The world&#039;s most viewed site on global warming and climate change</description>
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		<title>By: jmrSudbury</title>
		<link>http://wattsupwiththat.com/2008/06/11/waiting-for-hadcrut/#comment-19802</link>
		<dc:creator><![CDATA[jmrSudbury]]></dc:creator>
		<pubDate>Wed, 18 Jun 2008 19:29:44 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1357#comment-19802</guid>
		<description><![CDATA[&lt;a href=&quot;http://hadobs.metoffice.com/hadcrut3/diagnostics/global/nh+sh/monthly&quot; rel=&quot;nofollow&quot;&gt;Hadcrut is now in for May&lt;/a&gt;:

2008/05  0.278  0.294  0.262  0.443  0.114  0.278  0.272  0.444  0.113  0.444  0.113

John M Reynolds]]></description>
		<content:encoded><![CDATA[<p><a href="http://hadobs.metoffice.com/hadcrut3/diagnostics/global/nh+sh/monthly" rel="nofollow">Hadcrut is now in for May</a>:</p>
<p>2008/05  0.278  0.294  0.262  0.443  0.114  0.278  0.272  0.444  0.113  0.444  0.113</p>
<p>John M Reynolds</p>
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		<title>By: Steve Stip</title>
		<link>http://wattsupwiththat.com/2008/06/11/waiting-for-hadcrut/#comment-19134</link>
		<dc:creator><![CDATA[Steve Stip]]></dc:creator>
		<pubDate>Sat, 14 Jun 2008 19:04:45 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1357#comment-19134</guid>
		<description><![CDATA[OldJim,

Thanks for the link.  It looks good and something that might be at my level.]]></description>
		<content:encoded><![CDATA[<p>OldJim,</p>
<p>Thanks for the link.  It looks good and something that might be at my level.</p>
]]></content:encoded>
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		<title>By: Steve Stip</title>
		<link>http://wattsupwiththat.com/2008/06/11/waiting-for-hadcrut/#comment-19128</link>
		<dc:creator><![CDATA[Steve Stip]]></dc:creator>
		<pubDate>Sat, 14 Jun 2008 18:33:59 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1357#comment-19128</guid>
		<description><![CDATA[Ric Werme (08:51:41) :

Yes, you are speaking of the difference between the analytic approach and the iterative approach (made practical by computers).  I always appreciate a math lesson though, particularly by a good teacher.  

&quot;At any rate, no solutions, the best we can hope for are good answers. We have a ways to go.&quot;  &lt;---- humility, the secret of greatness

Thanks.]]></description>
		<content:encoded><![CDATA[<p>Ric Werme (08:51:41) :</p>
<p>Yes, you are speaking of the difference between the analytic approach and the iterative approach (made practical by computers).  I always appreciate a math lesson though, particularly by a good teacher.  </p>
<p>&#8220;At any rate, no solutions, the best we can hope for are good answers. We have a ways to go.&#8221;  &lt;&#8212;- humility, the secret of greatness</p>
<p>Thanks.</p>
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		<title>By: Steve Stip</title>
		<link>http://wattsupwiththat.com/2008/06/11/waiting-for-hadcrut/#comment-19106</link>
		<dc:creator><![CDATA[Steve Stip]]></dc:creator>
		<pubDate>Sat, 14 Jun 2008 16:45:01 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1357#comment-19106</guid>
		<description><![CDATA[DAV,

My assertion about neural nets was rash.  Still, in my experience, a simulation can be tweaked to give the &quot;correct&quot; results.]]></description>
		<content:encoded><![CDATA[<p>DAV,</p>
<p>My assertion about neural nets was rash.  Still, in my experience, a simulation can be tweaked to give the &#8220;correct&#8221; results.</p>
]]></content:encoded>
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		<title>By: Steve Stip</title>
		<link>http://wattsupwiththat.com/2008/06/11/waiting-for-hadcrut/#comment-19105</link>
		<dc:creator><![CDATA[Steve Stip]]></dc:creator>
		<pubDate>Sat, 14 Jun 2008 16:37:07 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1357#comment-19105</guid>
		<description><![CDATA[DAV,

I meant, are the equations used false or not complete?   What is the basis for the AGW claim if they use the wrong equations in their models?

Yes, predicting the past is easy, a neural net could learn to do that.

Also, the highest temperature I can imagine the earth reaching would be if it were painted black.  How hot is that?]]></description>
		<content:encoded><![CDATA[<p>DAV,</p>
<p>I meant, are the equations used false or not complete?   What is the basis for the AGW claim if they use the wrong equations in their models?</p>
<p>Yes, predicting the past is easy, a neural net could learn to do that.</p>
<p>Also, the highest temperature I can imagine the earth reaching would be if it were painted black.  How hot is that?</p>
]]></content:encoded>
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		<title>By: Ric Werme</title>
		<link>http://wattsupwiththat.com/2008/06/11/waiting-for-hadcrut/#comment-19098</link>
		<dc:creator><![CDATA[Ric Werme]]></dc:creator>
		<pubDate>Sat, 14 Jun 2008 15:51:41 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1357#comment-19098</guid>
		<description><![CDATA[Steve Stip (07:34:47) :

&quot;In the days before computers, I reckon it made sense to simplify equations but with computers what need is there for that anymore?&quot;

It&#039;s not so much simplifying equations, but solving them.  For example, if you know that acceleration is force / mass, then you can derive velocity and position given the initial values.  One way is to derive the solution by integrating acceleration wrt time once for velocity and again for position.  The other way is to let the computer do it with small steps in time.  The differential equation is simple, a = f / m.  The solution is more complex, s = s0 + (v0 x t) + (a x t^2)/2, where s0 and v0 are the initial position and velocity.  (And things are more complex is acceleration isn&#039;t constant.)

The advantage of the calculus solution is better understanding and having a new equation that can be readily applied.  The disadvantage is that it doesn&#039;t take much of a system that is described by a set of differential equations that cannot be solved.  Then there&#039;s really no choice these days other than letting the computer chew.

Checking one&#039;s work, be it a suspension bridge or spacecraft heat shield or planet is never easy, but it is important.

While Miskolczi&#039;s paper is very important, the feedback factor used in the models to try to handle the effect of more water vapor as the atmosphere warms appears to provide an even bigger error in the models.

Sidebar:
Any chaotic system doesn&#039;t have a single equation that describes how it behaves.  The best know and one of the first documented is the &lt;a href=&quot;http://en.wikipedia.org/wiki/Lorenz_attractor&quot; rel=&quot;nofollow&quot;&gt;Lorenz attractor&lt;/a&gt; that takes three simple equations that describe atmospheric convection.  I assume some variant of them are in weather prediction models, possibly not in climate models.

At any rate, no solutions, the best we can hope for are good answers.  We have a ways to go.

http://en.wikipedia.org/wiki/Lorenz_attractor]]></description>
		<content:encoded><![CDATA[<p>Steve Stip (07:34:47) :</p>
<p>&#8220;In the days before computers, I reckon it made sense to simplify equations but with computers what need is there for that anymore?&#8221;</p>
<p>It&#8217;s not so much simplifying equations, but solving them.  For example, if you know that acceleration is force / mass, then you can derive velocity and position given the initial values.  One way is to derive the solution by integrating acceleration wrt time once for velocity and again for position.  The other way is to let the computer do it with small steps in time.  The differential equation is simple, a = f / m.  The solution is more complex, s = s0 + (v0 x t) + (a x t^2)/2, where s0 and v0 are the initial position and velocity.  (And things are more complex is acceleration isn&#8217;t constant.)</p>
<p>The advantage of the calculus solution is better understanding and having a new equation that can be readily applied.  The disadvantage is that it doesn&#8217;t take much of a system that is described by a set of differential equations that cannot be solved.  Then there&#8217;s really no choice these days other than letting the computer chew.</p>
<p>Checking one&#8217;s work, be it a suspension bridge or spacecraft heat shield or planet is never easy, but it is important.</p>
<p>While Miskolczi&#8217;s paper is very important, the feedback factor used in the models to try to handle the effect of more water vapor as the atmosphere warms appears to provide an even bigger error in the models.</p>
<p>Sidebar:<br />
Any chaotic system doesn&#8217;t have a single equation that describes how it behaves.  The best know and one of the first documented is the <a href="http://en.wikipedia.org/wiki/Lorenz_attractor" rel="nofollow">Lorenz attractor</a> that takes three simple equations that describe atmospheric convection.  I assume some variant of them are in weather prediction models, possibly not in climate models.</p>
<p>At any rate, no solutions, the best we can hope for are good answers.  We have a ways to go.</p>
<p><a href="http://en.wikipedia.org/wiki/Lorenz_attractor" rel="nofollow">http://en.wikipedia.org/wiki/Lorenz_attractor</a></p>
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		<title>By: Oldjim</title>
		<link>http://wattsupwiththat.com/2008/06/11/waiting-for-hadcrut/#comment-19087</link>
		<dc:creator><![CDATA[Oldjim]]></dc:creator>
		<pubDate>Sat, 14 Jun 2008 15:16:22 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1357#comment-19087</guid>
		<description><![CDATA[If you want to read a simplified explanation (even I can understand most of it) this may help.
The subsequent 3 parts are also available as links within the comments
http://landshape.org/enm/modeling-global-warming/]]></description>
		<content:encoded><![CDATA[<p>If you want to read a simplified explanation (even I can understand most of it) this may help.<br />
The subsequent 3 parts are also available as links within the comments<br />
<a href="http://landshape.org/enm/modeling-global-warming/" rel="nofollow">http://landshape.org/enm/modeling-global-warming/</a></p>
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		<title>By: Steve Stip</title>
		<link>http://wattsupwiththat.com/2008/06/11/waiting-for-hadcrut/#comment-19074</link>
		<dc:creator><![CDATA[Steve Stip]]></dc:creator>
		<pubDate>Sat, 14 Jun 2008 14:34:47 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1357#comment-19074</guid>
		<description><![CDATA[OldJim,

Thanks,  I wish I had paid more attention in differential equations.  

In the days before computers, I reckon it made sense to simplify equations but with computers what need is there for that anymore?]]></description>
		<content:encoded><![CDATA[<p>OldJim,</p>
<p>Thanks,  I wish I had paid more attention in differential equations.  </p>
<p>In the days before computers, I reckon it made sense to simplify equations but with computers what need is there for that anymore?</p>
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		<title>By: DAV</title>
		<link>http://wattsupwiththat.com/2008/06/11/waiting-for-hadcrut/#comment-19062</link>
		<dc:creator><![CDATA[DAV]]></dc:creator>
		<pubDate>Sat, 14 Jun 2008 13:50:57 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1357#comment-19062</guid>
		<description><![CDATA[Steve Stip: &lt;blockquote&gt;is this article true?&lt;/blockquote&gt;

True in what respect?

That the equations being used are incorrect or that Miskolczi re-derived the solution?

One of the tricks I learned long ago that helps when dealing with complex problems is &quot;follow the energy.&quot; There&#039;s obviously something wrong with the &quot;runaway GHG&quot; scenario. Physical systems don&#039;t usually do that -- if only because it normally requires a release of internal energy. I can&#039;t envision a scenario where an opaque gas could release internal energy without transforming itself chemically.

I say &quot;obviously&quot; because ... well ... it doesn&#039;t happen. The temperature is stable. I don&#039;t buy the &quot;tipping point&quot; logic for even a second. It&#039;s not like the atmosphere is similar to a ball about to fall off the edge of a cliff where downward energy suddenly &quot;appears&quot; in the form of gravity. Nor is it like a chemical explosive that experiences sudden energy release after passing a threshold.

The dropping-off-a-cliff scenario is not completely out of the picture, though. It is possible that whatever negative feedback system that is currently operating to keep temperature in check could become overwhelmed. Still, the &lt;strike&gt;handwaving&lt;/strike&gt; postulation of atmospheric &quot;tipping point&quot; is a guess. The proponents certainly can&#039;t say what that feedback currently &lt;i&gt;is&lt;/i&gt; let alone how much it can take before breakdown.]]></description>
		<content:encoded><![CDATA[<p>Steve Stip:<br />
<blockquote>is this article true?</p></blockquote>
<p>True in what respect?</p>
<p>That the equations being used are incorrect or that Miskolczi re-derived the solution?</p>
<p>One of the tricks I learned long ago that helps when dealing with complex problems is &#8220;follow the energy.&#8221; There&#8217;s obviously something wrong with the &#8220;runaway GHG&#8221; scenario. Physical systems don&#8217;t usually do that &#8212; if only because it normally requires a release of internal energy. I can&#8217;t envision a scenario where an opaque gas could release internal energy without transforming itself chemically.</p>
<p>I say &#8220;obviously&#8221; because &#8230; well &#8230; it doesn&#8217;t happen. The temperature is stable. I don&#8217;t buy the &#8220;tipping point&#8221; logic for even a second. It&#8217;s not like the atmosphere is similar to a ball about to fall off the edge of a cliff where downward energy suddenly &#8220;appears&#8221; in the form of gravity. Nor is it like a chemical explosive that experiences sudden energy release after passing a threshold.</p>
<p>The dropping-off-a-cliff scenario is not completely out of the picture, though. It is possible that whatever negative feedback system that is currently operating to keep temperature in check could become overwhelmed. Still, the <strike>handwaving</strike> postulation of atmospheric &#8220;tipping point&#8221; is a guess. The proponents certainly can&#8217;t say what that feedback currently <i>is</i> let alone how much it can take before breakdown.</p>
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		<title>By: Mike Bryant</title>
		<link>http://wattsupwiththat.com/2008/06/11/waiting-for-hadcrut/#comment-19055</link>
		<dc:creator><![CDATA[Mike Bryant]]></dc:creator>
		<pubDate>Sat, 14 Jun 2008 12:46:25 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1357#comment-19055</guid>
		<description><![CDATA[Mike Bryant issues a challenge to all climate models... 
Please publish Earth&#039;s monthly temperatures for the next twelve months. This should be no problem whatsoever since one hundred years is well within possibility.
Mike Bryant]]></description>
		<content:encoded><![CDATA[<p>Mike Bryant issues a challenge to all climate models&#8230;<br />
Please publish Earth&#8217;s monthly temperatures for the next twelve months. This should be no problem whatsoever since one hundred years is well within possibility.<br />
Mike Bryant</p>
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		<title>By: Oldjim</title>
		<link>http://wattsupwiththat.com/2008/06/11/waiting-for-hadcrut/#comment-19035</link>
		<dc:creator><![CDATA[Oldjim]]></dc:creator>
		<pubDate>Sat, 14 Jun 2008 10:37:05 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1357#comment-19035</guid>
		<description><![CDATA[I think this is the original paper which caused Miklós Zágoni to change his mind
http://met.hu/doc/idojaras/vol111001_01.pdf]]></description>
		<content:encoded><![CDATA[<p>I think this is the original paper which caused Miklós Zágoni to change his mind<br />
<a href="http://met.hu/doc/idojaras/vol111001_01.pdf" rel="nofollow">http://met.hu/doc/idojaras/vol111001_01.pdf</a></p>
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		<title>By: Oldjim</title>
		<link>http://wattsupwiththat.com/2008/06/11/waiting-for-hadcrut/#comment-19033</link>
		<dc:creator><![CDATA[Oldjim]]></dc:creator>
		<pubDate>Sat, 14 Jun 2008 10:21:52 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1357#comment-19033</guid>
		<description><![CDATA[Although I am not sufficiently knowledgeable to fully understand the details of the paper this is exactly the scenario I found when I started using an existing elastoplastic strain calculation with indeterminate bend rates on a relatively modern computer. I found several problems with transition points and end conditions which cast doubt on the whole theory. 
However when I went back to the original work I found that several third order variables had been omitted to simplify the calculation on the grounds that they had no real effect in the range of results which were then being considered.
It was only when these variables were reinstated that the results started to match the theory over the extended range of parameters.
If, as seems reasonable, the boundary conditions for CO2 warming were simplified to make the calculation easier for the range of condition then being considered then using the same formulae when going well outside the original assumed parameters could well be a serious error.]]></description>
		<content:encoded><![CDATA[<p>Although I am not sufficiently knowledgeable to fully understand the details of the paper this is exactly the scenario I found when I started using an existing elastoplastic strain calculation with indeterminate bend rates on a relatively modern computer. I found several problems with transition points and end conditions which cast doubt on the whole theory.<br />
However when I went back to the original work I found that several third order variables had been omitted to simplify the calculation on the grounds that they had no real effect in the range of results which were then being considered.<br />
It was only when these variables were reinstated that the results started to match the theory over the extended range of parameters.<br />
If, as seems reasonable, the boundary conditions for CO2 warming were simplified to make the calculation easier for the range of condition then being considered then using the same formulae when going well outside the original assumed parameters could well be a serious error.</p>
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		<title>By: Steve Stip</title>
		<link>http://wattsupwiththat.com/2008/06/11/waiting-for-hadcrut/#comment-18941</link>
		<dc:creator><![CDATA[Steve Stip]]></dc:creator>
		<pubDate>Sat, 14 Jun 2008 00:51:11 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1357#comment-18941</guid>
		<description><![CDATA[Pam,

I have not seen it addressed here, perhaps because I am a late arrival, but apparently the basic differential equations in some climate models are wrong.

More info at:  http://www.dailytech.com/Researcher+Basic+Greenhouse+Equations+Totally+Wrong/article10973.htm

others,  is this article true?]]></description>
		<content:encoded><![CDATA[<p>Pam,</p>
<p>I have not seen it addressed here, perhaps because I am a late arrival, but apparently the basic differential equations in some climate models are wrong.</p>
<p>More info at:  <a href="http://www.dailytech.com/Researcher+Basic+Greenhouse+Equations+Totally+Wrong/article10973.htm" rel="nofollow">http://www.dailytech.com/Researcher+Basic+Greenhouse+Equations+Totally+Wrong/article10973.htm</a></p>
<p>others,  is this article true?</p>
]]></content:encoded>
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	<item>
		<title>By: Steve Stip</title>
		<link>http://wattsupwiththat.com/2008/06/11/waiting-for-hadcrut/#comment-18942</link>
		<dc:creator><![CDATA[Steve Stip]]></dc:creator>
		<pubDate>Sat, 14 Jun 2008 00:49:11 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1357#comment-18942</guid>
		<description><![CDATA[Pam,

I have not seen it addressed here, perhaps because I am a late arrival, but apparently the basic differential equations in some climate models are wrong.

More info at:  http://www.dailytech.com/Researcher+Basic+Greenhouse+Equations+Totally+Wrong/article10973.htm

others,  is this article true?]]></description>
		<content:encoded><![CDATA[<p>Pam,</p>
<p>I have not seen it addressed here, perhaps because I am a late arrival, but apparently the basic differential equations in some climate models are wrong.</p>
<p>More info at:  <a href="http://www.dailytech.com/Researcher+Basic+Greenhouse+Equations+Totally+Wrong/article10973.htm" rel="nofollow">http://www.dailytech.com/Researcher+Basic+Greenhouse+Equations+Totally+Wrong/article10973.htm</a></p>
<p>others,  is this article true?</p>
]]></content:encoded>
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		<title>By: jmrsudbury</title>
		<link>http://wattsupwiththat.com/2008/06/11/waiting-for-hadcrut/#comment-18830</link>
		<dc:creator><![CDATA[jmrsudbury]]></dc:creator>
		<pubDate>Fri, 13 Jun 2008 19:15:58 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1357#comment-18830</guid>
		<description><![CDATA[Your blog&#039;s homepage shows postings up to June 10th.  I can only find the newer posts by opening the bees and sunspots post and finding the Next Article link to get the newer articles one at a time.  Opera 9.5, IE7, and firefox 3 were tested.  -- John M Reynolds

&lt;strong&gt;REPLY:&lt;/strong&gt; I&#039;ve seen that with some connections, it may be an upstream cache issue, there is nothing I can do about it.]]></description>
		<content:encoded><![CDATA[<p>Your blog&#8217;s homepage shows postings up to June 10th.  I can only find the newer posts by opening the bees and sunspots post and finding the Next Article link to get the newer articles one at a time.  Opera 9.5, IE7, and firefox 3 were tested.  &#8212; John M Reynolds</p>
<p><strong>REPLY:</strong> I&#8217;ve seen that with some connections, it may be an upstream cache issue, there is nothing I can do about it.</p>
]]></content:encoded>
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