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	<title>Comments on: Polar Urals: Shiyatov&#039;s Finnish Academy Article</title>
	<atom:link href="http://climateaudit.org/2005/08/04/polar-urals-shiyatovs-finnish-academy-article/feed/" rel="self" type="application/rss+xml" />
	<link>http://climateaudit.org/2005/08/04/polar-urals-shiyatovs-finnish-academy-article/</link>
	<description>by Steve McIntyre</description>
	<lastBuildDate>Tue, 21 May 2013 15:32:22 +0000</lastBuildDate>
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		<title>By: Lamarche on Treelines #2 &#171; Climate Audit</title>
		<link>http://climateaudit.org/2005/08/04/polar-urals-shiyatovs-finnish-academy-article/#comment-299421</link>
		<dc:creator><![CDATA[Lamarche on Treelines #2 &#171; Climate Audit]]></dc:creator>
		<pubDate>Thu, 28 Jul 2011 19:02:47 +0000</pubDate>
		<guid isPermaLink="false">http://www.climateaudit.org/?p=294#comment-299421</guid>
		<description><![CDATA[[...] of treeline elevations that I&#8217;ve seen is at the Polar Urals site, which I&#8217;ve shown here and here. The really odd coincidence &#8211; and I don&#8217;t believe in coincidences &#8211; is [...]]]></description>
		<content:encoded><![CDATA[<p>[...] of treeline elevations that I&#8217;ve seen is at the Polar Urals site, which I&#8217;ve shown here and here. The really odd coincidence &#8211; and I don&#8217;t believe in coincidences &#8211; is [...]</p>
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		<title>By: Louis Hissink</title>
		<link>http://climateaudit.org/2005/08/04/polar-urals-shiyatovs-finnish-academy-article/#comment-35303</link>
		<dc:creator><![CDATA[Louis Hissink]]></dc:creator>
		<pubDate>Fri, 05 Aug 2005 13:38:43 +0000</pubDate>
		<guid isPermaLink="false">http://www.climateaudit.org/?p=294#comment-35303</guid>
		<description><![CDATA[What is the sample support for this study?

Tree-rings? Which trees, what trees?

All rather unscientific]]></description>
		<content:encoded><![CDATA[<p>What is the sample support for this study?</p>
<p>Tree-rings? Which trees, what trees?</p>
<p>All rather unscientific</p>
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		<title>By: Paul Gosling</title>
		<link>http://climateaudit.org/2005/08/04/polar-urals-shiyatovs-finnish-academy-article/#comment-35302</link>
		<dc:creator><![CDATA[Paul Gosling]]></dc:creator>
		<pubDate>Fri, 05 Aug 2005 08:46:09 +0000</pubDate>
		<guid isPermaLink="false">http://www.climateaudit.org/?p=294#comment-35302</guid>
		<description><![CDATA[Steve

I don&#039;t really know how tree ring data is standardized. But for a single sample altitude will not have an effect, the tree does not move. When comparing two trees, say 200m appart (altitude), presumably the comparison is in the year to year variation. Not between the wood density of tree a and b. Presumably there are then some standardised trees which are correlated with measured temperatures? I guess the ideal situation would be sample over an altitudinal gradient, but I doubt they have it?

As for tree lines. I have been thinking about them. I know for a fact that tree lines are depressed by grazing. Though whether this is a factor in the northern Urals I don&#039;t know. The rate of reaction of tree lines will also depend on longevity of tree species. Larch is relativelty short lived so should be much better than bristlecones. I worry a bit about Shiyatov&#039;s data because the maximum change in altitude is only 60m. That is a very small change in temperature. It looks much stronger in the actual article with tree rings etc.]]></description>
		<content:encoded><![CDATA[<p>Steve</p>
<p>I don&#8217;t really know how tree ring data is standardized. But for a single sample altitude will not have an effect, the tree does not move. When comparing two trees, say 200m appart (altitude), presumably the comparison is in the year to year variation. Not between the wood density of tree a and b. Presumably there are then some standardised trees which are correlated with measured temperatures? I guess the ideal situation would be sample over an altitudinal gradient, but I doubt they have it?</p>
<p>As for tree lines. I have been thinking about them. I know for a fact that tree lines are depressed by grazing. Though whether this is a factor in the northern Urals I don&#8217;t know. The rate of reaction of tree lines will also depend on longevity of tree species. Larch is relativelty short lived so should be much better than bristlecones. I worry a bit about Shiyatov&#8217;s data because the maximum change in altitude is only 60m. That is a very small change in temperature. It looks much stronger in the actual article with tree rings etc.</p>
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		<title>By: John A</title>
		<link>http://climateaudit.org/2005/08/04/polar-urals-shiyatovs-finnish-academy-article/#comment-35301</link>
		<dc:creator><![CDATA[John A]]></dc:creator>
		<pubDate>Thu, 04 Aug 2005 16:28:37 +0000</pubDate>
		<guid isPermaLink="false">http://www.climateaudit.org/?p=294#comment-35301</guid>
		<description><![CDATA[Re #2

It works for me.]]></description>
		<content:encoded><![CDATA[<p>Re #2</p>
<p>It works for me.</p>
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		<title>By: Paul Gosling</title>
		<link>http://climateaudit.org/2005/08/04/polar-urals-shiyatovs-finnish-academy-article/#comment-35300</link>
		<dc:creator><![CDATA[Paul Gosling]]></dc:creator>
		<pubDate>Thu, 04 Aug 2005 15:19:35 +0000</pubDate>
		<guid isPermaLink="false">http://www.climateaudit.org/?p=294#comment-35300</guid>
		<description><![CDATA[PS the link to the article does not seem to work. Steve: fixed]]></description>
		<content:encoded><![CDATA[<p>PS the link to the article does not seem to work. Steve: fixed</p>
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		<title>By: Paul Gosling</title>
		<link>http://climateaudit.org/2005/08/04/polar-urals-shiyatovs-finnish-academy-article/#comment-35299</link>
		<dc:creator><![CDATA[Paul Gosling]]></dc:creator>
		<pubDate>Thu, 04 Aug 2005 15:18:24 +0000</pubDate>
		<guid isPermaLink="false">http://www.climateaudit.org/?p=294#comment-35299</guid>
		<description><![CDATA[Steve Its a bit difficult to comare the two as Briffas graph does not start until the 10th centruy. But from the start of the 11th C to the mid 13th Briffa does show a fairly consistent rise in temperature. I doubt the tree line would react fast enough to respond to the short term variation.

&lt;strong&gt;Steve: &lt;/strong&gt; But Briffa&#039;s level ~AD1200 is about the same as his level ~AD1650, while the altitudes of the trees are completely different.  If desnity is not a function of altitude per se, as Briffa argues, and it is a function of temperature, then one should presumably apply a lapse rate to adjust.]]></description>
		<content:encoded><![CDATA[<p>Steve Its a bit difficult to comare the two as Briffas graph does not start until the 10th centruy. But from the start of the 11th C to the mid 13th Briffa does show a fairly consistent rise in temperature. I doubt the tree line would react fast enough to respond to the short term variation.</p>
<p><strong>Steve: </strong> But Briffa&#8217;s level ~AD1200 is about the same as his level ~AD1650, while the altitudes of the trees are completely different.  If desnity is not a function of altitude per se, as Briffa argues, and it is a function of temperature, then one should presumably apply a lapse rate to adjust.</p>
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