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	<title>Comments on: Basic Radiative models/Earth&#8217;s climate system analysis Pt. 2</title>
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	<link>http://chriscolose.wordpress.com/2007/12/25/basic-radiative-modelsearths-climate-system-analysis-pt-2/</link>
	<description>An Analysis of Key Questions</description>
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		<title>By: J. R. Leicester</title>
		<link>http://chriscolose.wordpress.com/2007/12/25/basic-radiative-modelsearths-climate-system-analysis-pt-2/#comment-847</link>
		<dc:creator>J. R. Leicester</dc:creator>
		<pubDate>Mon, 04 May 2009 19:03:10 +0000</pubDate>
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		<description>Fully 45 % of the sun&#039;s radiation is infrared.  It exists in the spectrum wavelengths between 760 nm and 3E-4 cm.  Where is this accounted for?  CO2 does not absorb infrared in these wavelengths..

How is CO2 &quot;layered&quot; in the atmosphere?  By temperature?  Mass?  What is the absorptivity of CO2?

Noting that, with a doubling of CO2 in the atmosphere, there are virtually no changes in the capability of the gas to either transfer heat or diffuse it, how does it become such a &#039;superinsulator&#039;?

The temperature differential between earth&#039;s surface and the average atmospheric temperature indicates infrared radiation from earth to be, at best, insignificant.  Most of the heat carried to the atmosphere is by conduction and convection.  It is only at the atmospheric/space boundary where the radiant heat transfer becomes significant because of the lack of atmosphere.  How can earth&#039;s radiative heat loss be measured accurately with such a wide variance of surface temperatures throughout the  globe?</description>
		<content:encoded><![CDATA[<p>Fully 45 % of the sun&#8217;s radiation is infrared.  It exists in the spectrum wavelengths between 760 nm and 3E-4 cm.  Where is this accounted for?  CO2 does not absorb infrared in these wavelengths..</p>
<p>How is CO2 &#8220;layered&#8221; in the atmosphere?  By temperature?  Mass?  What is the absorptivity of CO2?</p>
<p>Noting that, with a doubling of CO2 in the atmosphere, there are virtually no changes in the capability of the gas to either transfer heat or diffuse it, how does it become such a &#8217;superinsulator&#8217;?</p>
<p>The temperature differential between earth&#8217;s surface and the average atmospheric temperature indicates infrared radiation from earth to be, at best, insignificant.  Most of the heat carried to the atmosphere is by conduction and convection.  It is only at the atmospheric/space boundary where the radiant heat transfer becomes significant because of the lack of atmosphere.  How can earth&#8217;s radiative heat loss be measured accurately with such a wide variance of surface temperatures throughout the  globe?</p>
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		<title>By: Basic Radiative models/Earth&#8217;s climate system analysis Pt. 3 &#171; Climate Change</title>
		<link>http://chriscolose.wordpress.com/2007/12/25/basic-radiative-modelsearths-climate-system-analysis-pt-2/#comment-20</link>
		<dc:creator>Basic Radiative models/Earth&#8217;s climate system analysis Pt. 3 &#171; Climate Change</dc:creator>
		<pubDate>Sun, 30 Dec 2007 08:59:07 +0000</pubDate>
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		<description>[...] Climate Change An Analysis of Key Questions    &#171; Basic Radiative models/Earth&#8217;s climate system analysis Pt.&#160;2 [...]</description>
		<content:encoded><![CDATA[<p>[...] Climate Change An Analysis of Key Questions    &laquo; Basic Radiative models/Earth&#8217;s climate system analysis Pt.&nbsp;2 [...]</p>
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