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	<title>Comments on: Buckets, Inlets, SST’s and all that &#8211; part 2</title>
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	<link>http://wattsupwiththat.com/2008/05/30/buckets-inlets-sst%e2%80%99s-and-all-that-part-2/</link>
	<description>The world&#039;s most viewed site on global warming and climate change</description>
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		<title>By: referencelucinda</title>
		<link>http://wattsupwiththat.com/2008/05/30/buckets-inlets-sst%e2%80%99s-and-all-that-part-2/#comment-16609</link>
		<dc:creator><![CDATA[referencelucinda]]></dc:creator>
		<pubDate>Tue, 03 Jun 2008 14:24:08 +0000</pubDate>
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		<description><![CDATA[Interesting to see manual measurement of sea surface.]]></description>
		<content:encoded><![CDATA[<p>Interesting to see manual measurement of sea surface.</p>
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		<title>By: Pete</title>
		<link>http://wattsupwiththat.com/2008/05/30/buckets-inlets-sst%e2%80%99s-and-all-that-part-2/#comment-16540</link>
		<dc:creator><![CDATA[Pete]]></dc:creator>
		<pubDate>Mon, 02 Jun 2008 23:58:54 +0000</pubDate>
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		<description><![CDATA[For intake thermometers from 10-50 ft below the surface, one significant question would be how much of the water may actually be surface water that has been deflected downward, so a 20 foot deep inlet may be sucking water that was, say 8 ft deep (or whatever).  It seems that would be highly specific to hull shapes and inlet port details.  

I would almost guarantee that marine engineers have such data and probably for many hull shapes, and if they don&#039;t for all hull shapes they could probably fairly easily do that with a little bit of the global warming research $ that&#039;s floating around. 

Also, the comment about surface water churn in highly traveled waters contributing to lower readings seems to make sense, in the same way that a hurricane leaves behind a trail of cooler water, but I would be cautious about jumping to a numeric conclusion on this without some analysis.]]></description>
		<content:encoded><![CDATA[<p>For intake thermometers from 10-50 ft below the surface, one significant question would be how much of the water may actually be surface water that has been deflected downward, so a 20 foot deep inlet may be sucking water that was, say 8 ft deep (or whatever).  It seems that would be highly specific to hull shapes and inlet port details.  </p>
<p>I would almost guarantee that marine engineers have such data and probably for many hull shapes, and if they don&#8217;t for all hull shapes they could probably fairly easily do that with a little bit of the global warming research $ that&#8217;s floating around. </p>
<p>Also, the comment about surface water churn in highly traveled waters contributing to lower readings seems to make sense, in the same way that a hurricane leaves behind a trail of cooler water, but I would be cautious about jumping to a numeric conclusion on this without some analysis.</p>
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		<title>By: Chance Metz</title>
		<link>http://wattsupwiththat.com/2008/05/30/buckets-inlets-sst%e2%80%99s-and-all-that-part-2/#comment-16407</link>
		<dc:creator><![CDATA[Chance Metz]]></dc:creator>
		<pubDate>Sun, 01 Jun 2008 23:52:24 +0000</pubDate>
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		<description><![CDATA[No suprise if they were.]]></description>
		<content:encoded><![CDATA[<p>No suprise if they were.</p>
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		<title>By: AnyMouse</title>
		<link>http://wattsupwiththat.com/2008/05/30/buckets-inlets-sst%e2%80%99s-and-all-that-part-2/#comment-16303</link>
		<dc:creator><![CDATA[AnyMouse]]></dc:creator>
		<pubDate>Sun, 01 Jun 2008 02:34:53 +0000</pubDate>
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		<description><![CDATA[The following PPT mentions uninsulated buckets before WWII and insulated buckets after.  Was Britain behind the times and using uninsulated ones later?
http://www.authorstream.com/Presentation/Dixon-25940-reynolds-Sea-Surface-Temperature-SST-Analyses-Climate-Introduction-Change-Detection-SSTs-El-Ni-o-La-as-Entertainment-ppt-powerpoint/]]></description>
		<content:encoded><![CDATA[<p>The following PPT mentions uninsulated buckets before WWII and insulated buckets after.  Was Britain behind the times and using uninsulated ones later?<br />
<a href="http://www.authorstream.com/Presentation/Dixon-25940-reynolds-Sea-Surface-Temperature-SST-Analyses-Climate-Introduction-Change-Detection-SSTs-El-Ni-o-La-as-Entertainment-ppt-powerpoint/" rel="nofollow">http://www.authorstream.com/Presentation/Dixon-25940-reynolds-Sea-Surface-Temperature-SST-Analyses-Climate-Introduction-Change-Detection-SSTs-El-Ni-o-La-as-Entertainment-ppt-powerpoint/</a></p>
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		<title>By: Chance Metz</title>
		<link>http://wattsupwiththat.com/2008/05/30/buckets-inlets-sst%e2%80%99s-and-all-that-part-2/#comment-16289</link>
		<dc:creator><![CDATA[Chance Metz]]></dc:creator>
		<pubDate>Sun, 01 Jun 2008 00:38:39 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1282#comment-16289</guid>
		<description><![CDATA[Wow took about messed up readings!]]></description>
		<content:encoded><![CDATA[<p>Wow took about messed up readings!</p>
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		<title>By: Jon Jewett</title>
		<link>http://wattsupwiththat.com/2008/05/30/buckets-inlets-sst%e2%80%99s-and-all-that-part-2/#comment-16223</link>
		<dc:creator><![CDATA[Jon Jewett]]></dc:creator>
		<pubDate>Sat, 31 May 2008 17:49:13 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1282#comment-16223</guid>
		<description><![CDATA[NOTE:  I POSTED THIS WITH PART.  I HAVE JUST READ THIS PART AND BELIEVE THAT IT WOULD BE MORE PROPERLY POSTED HERE.

I am a retired merchant marine engineer.  I made my living on merchant ships from 1966 to 1999, when I retired as Chief Engineer of a 32,000 SHP steam turbine powered container ship.  

A ship moves through the water at between 12 knots and 22 knots.  (Twelve knots for an old Liberty Ship from WWII, 22 knots fairly representative of new ships.)  At even 12 knots, the speed is fast enough to cause turbulent flow of the sea water and thereby prevent a “warm” layer forming along the ship.  In addition, very little of the ship is a significant heat source; only the area in way of the machinery spaces.  Most of the ship is thermally inert cargo space that may be warmer or colder than the sea temperature.  The main cooling water pump (Main Circulator) takes suction through the hull at a depth of 15 feet to 60 feet (depending on the ship) below the surface of the water.  In addition, a Main Circulator will pump up to several thousand gallons per minute.

In short, the concept that the water would be heated by a measurable amount is far fetched at best.  The statement indicates that assumptions were made about the measurement process and there was no meaningful investigation before these opinions were voiced.  

Actually, there is cause for concern in using these numbers.  Typically, either alcohol type bulb thermometers or bimetallic type thermometers were used.  They were calibrated at the factory before they were installed, but never after that as long as the readings were “close enough”.  It was not until the late ‘60s that thermo-electronic (e.g. RTD and Thermister) methods started to enter the fleet.  It is to be expected that, particularly with the older readings, each one may be on the order of up to 10 degrees off, with a random distribution.

Regards,

Steamboat Jack]]></description>
		<content:encoded><![CDATA[<p>NOTE:  I POSTED THIS WITH PART.  I HAVE JUST READ THIS PART AND BELIEVE THAT IT WOULD BE MORE PROPERLY POSTED HERE.</p>
<p>I am a retired merchant marine engineer.  I made my living on merchant ships from 1966 to 1999, when I retired as Chief Engineer of a 32,000 SHP steam turbine powered container ship.  </p>
<p>A ship moves through the water at between 12 knots and 22 knots.  (Twelve knots for an old Liberty Ship from WWII, 22 knots fairly representative of new ships.)  At even 12 knots, the speed is fast enough to cause turbulent flow of the sea water and thereby prevent a “warm” layer forming along the ship.  In addition, very little of the ship is a significant heat source; only the area in way of the machinery spaces.  Most of the ship is thermally inert cargo space that may be warmer or colder than the sea temperature.  The main cooling water pump (Main Circulator) takes suction through the hull at a depth of 15 feet to 60 feet (depending on the ship) below the surface of the water.  In addition, a Main Circulator will pump up to several thousand gallons per minute.</p>
<p>In short, the concept that the water would be heated by a measurable amount is far fetched at best.  The statement indicates that assumptions were made about the measurement process and there was no meaningful investigation before these opinions were voiced.  </p>
<p>Actually, there is cause for concern in using these numbers.  Typically, either alcohol type bulb thermometers or bimetallic type thermometers were used.  They were calibrated at the factory before they were installed, but never after that as long as the readings were “close enough”.  It was not until the late ‘60s that thermo-electronic (e.g. RTD and Thermister) methods started to enter the fleet.  It is to be expected that, particularly with the older readings, each one may be on the order of up to 10 degrees off, with a random distribution.</p>
<p>Regards,</p>
<p>Steamboat Jack</p>
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		<title>By: jerry bono</title>
		<link>http://wattsupwiththat.com/2008/05/30/buckets-inlets-sst%e2%80%99s-and-all-that-part-2/#comment-16200</link>
		<dc:creator><![CDATA[jerry bono]]></dc:creator>
		<pubDate>Sat, 31 May 2008 15:33:09 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1282#comment-16200</guid>
		<description><![CDATA[Maybe this is in the literature I don&#039;t know since I have not read it but it seems to me all the bucket data came from right on the surface of the ocean, the real interface between air and sea.  Now, how deep was the sample taken from the engine inlets. I know it depends on the size of the ship but it should be deep enough to get away from potential wave troughs, maybe say 10 feet?  I don&#039;t know.  From my scuba diving experiences I can tell you that I have felt some very sever thermal gradients.  Most of this was near the cost obviously and I would expect open ocean to to be less variable but there should be a variation.]]></description>
		<content:encoded><![CDATA[<p>Maybe this is in the literature I don&#8217;t know since I have not read it but it seems to me all the bucket data came from right on the surface of the ocean, the real interface between air and sea.  Now, how deep was the sample taken from the engine inlets. I know it depends on the size of the ship but it should be deep enough to get away from potential wave troughs, maybe say 10 feet?  I don&#8217;t know.  From my scuba diving experiences I can tell you that I have felt some very sever thermal gradients.  Most of this was near the cost obviously and I would expect open ocean to to be less variable but there should be a variation.</p>
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		<title>By: JohnL</title>
		<link>http://wattsupwiththat.com/2008/05/30/buckets-inlets-sst%e2%80%99s-and-all-that-part-2/#comment-16193</link>
		<dc:creator><![CDATA[JohnL]]></dc:creator>
		<pubDate>Sat, 31 May 2008 14:41:57 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1282#comment-16193</guid>
		<description><![CDATA[Hmm.  Didn&#039;t you leave out the predominant means of measuring sea water temperature in the latter half of the twentieth century-- the sea water intake temperature?

I served on aFletcher class destroyer.  My memory is hazy, but I seem to recall an intake pipe about 18&quot; in diameter (though that may have been after it was split). The principal use of sea water was in the steam condensers.

   More importantly it was located well below the waterline, at least sufficiently deep so that heavy weather would not expose the inlet.

I am not sure why sea water say 10&#039;  in depth  can be presumed to be the same temperature as water retrieved by a bucket on the surface.

&lt;strong&gt;REPLY:&lt;/strong&gt; Your last line says it all, and I have plans to discuss that in part 3, and maybe part 4 if I have enough material.]]></description>
		<content:encoded><![CDATA[<p>Hmm.  Didn&#8217;t you leave out the predominant means of measuring sea water temperature in the latter half of the twentieth century&#8211; the sea water intake temperature?</p>
<p>I served on aFletcher class destroyer.  My memory is hazy, but I seem to recall an intake pipe about 18&#8243; in diameter (though that may have been after it was split). The principal use of sea water was in the steam condensers.</p>
<p>   More importantly it was located well below the waterline, at least sufficiently deep so that heavy weather would not expose the inlet.</p>
<p>I am not sure why sea water say 10&#8242;  in depth  can be presumed to be the same temperature as water retrieved by a bucket on the surface.</p>
<p><strong>REPLY:</strong> Your last line says it all, and I have plans to discuss that in part 3, and maybe part 4 if I have enough material.</p>
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		<title>By: kim</title>
		<link>http://wattsupwiththat.com/2008/05/30/buckets-inlets-sst%e2%80%99s-and-all-that-part-2/#comment-16190</link>
		<dc:creator><![CDATA[kim]]></dc:creator>
		<pubDate>Sat, 31 May 2008 13:40:40 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1282#comment-16190</guid>
		<description><![CDATA[Charles Blow at the New York Times is tardy with some ignorance about AGW and tornadoes.   Blow, blow, blow ye winds, blow.
========================================]]></description>
		<content:encoded><![CDATA[<p>Charles Blow at the New York Times is tardy with some ignorance about AGW and tornadoes.   Blow, blow, blow ye winds, blow.<br />
========================================</p>
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		<title>By: KlausB</title>
		<link>http://wattsupwiththat.com/2008/05/30/buckets-inlets-sst%e2%80%99s-and-all-that-part-2/#comment-16189</link>
		<dc:creator><![CDATA[KlausB]]></dc:creator>
		<pubDate>Sat, 31 May 2008 13:05:09 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1282#comment-16189</guid>
		<description><![CDATA[Aviator,
me too,  would certainly know what happened to all the bathytermograph datas we got 24/7, every four hours on all Navy vessels. 
Personally, I did it in the 70ties on a Federal German Navy ship, from Barents Sea down to Gibraltar, from mid Atlantic to the east of Baltic sea,  SST to temperatures downto 50 meters sub surface.
As far as I know, it was common procedure by all NATO vessels.
All these datas could be a treasure for getting the real.]]></description>
		<content:encoded><![CDATA[<p>Aviator,<br />
me too,  would certainly know what happened to all the bathytermograph datas we got 24/7, every four hours on all Navy vessels.<br />
Personally, I did it in the 70ties on a Federal German Navy ship, from Barents Sea down to Gibraltar, from mid Atlantic to the east of Baltic sea,  SST to temperatures downto 50 meters sub surface.<br />
As far as I know, it was common procedure by all NATO vessels.<br />
All these datas could be a treasure for getting the real.</p>
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		<title>By: Tom in Florida</title>
		<link>http://wattsupwiththat.com/2008/05/30/buckets-inlets-sst%e2%80%99s-and-all-that-part-2/#comment-16188</link>
		<dc:creator><![CDATA[Tom in Florida]]></dc:creator>
		<pubDate>Sat, 31 May 2008 12:06:43 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1282#comment-16188</guid>
		<description><![CDATA[Sea water surface temps can vary quite a bit at any particular spot depending on cloud cover, humidity, time of day, wave action, precipitation, upwelling conditions, currents and the previous days weather conditions. Unless all this was recorded at the time, each and every time, we simply have an isolated snap shot of a few cubic feet of water.]]></description>
		<content:encoded><![CDATA[<p>Sea water surface temps can vary quite a bit at any particular spot depending on cloud cover, humidity, time of day, wave action, precipitation, upwelling conditions, currents and the previous days weather conditions. Unless all this was recorded at the time, each and every time, we simply have an isolated snap shot of a few cubic feet of water.</p>
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		<title>By: rex</title>
		<link>http://wattsupwiththat.com/2008/05/30/buckets-inlets-sst%e2%80%99s-and-all-that-part-2/#comment-16178</link>
		<dc:creator><![CDATA[rex]]></dc:creator>
		<pubDate>Sat, 31 May 2008 08:20:42 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1282#comment-16178</guid>
		<description><![CDATA[anybody know what happened to COLA maps?]]></description>
		<content:encoded><![CDATA[<p>anybody know what happened to COLA maps?</p>
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		<title>By: rex</title>
		<link>http://wattsupwiththat.com/2008/05/30/buckets-inlets-sst%e2%80%99s-and-all-that-part-2/#comment-16177</link>
		<dc:creator><![CDATA[rex]]></dc:creator>
		<pubDate>Sat, 31 May 2008 08:19:29 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1282#comment-16177</guid>
		<description><![CDATA[interesting sharp dip in global temps lately
http://www.cdc.noaa.gov/map/images/fnl/sfctmpmer_01a.fnl.anim.html
http://discover.itsc.uah.edu/amsutemps/

&lt;strong&gt;REPLY:&lt;/strong&gt; Thanks Rex, I had not looked in awhile. I&#039;ll showcase this soon.]]></description>
		<content:encoded><![CDATA[<p>interesting sharp dip in global temps lately<br />
<a href="http://www.cdc.noaa.gov/map/images/fnl/sfctmpmer_01a.fnl.anim.html" rel="nofollow">http://www.cdc.noaa.gov/map/images/fnl/sfctmpmer_01a.fnl.anim.html</a><br />
<a href="http://discover.itsc.uah.edu/amsutemps/" rel="nofollow">http://discover.itsc.uah.edu/amsutemps/</a></p>
<p><strong>REPLY:</strong> Thanks Rex, I had not looked in awhile. I&#8217;ll showcase this soon.</p>
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		<title>By: Aviator</title>
		<link>http://wattsupwiththat.com/2008/05/30/buckets-inlets-sst%e2%80%99s-and-all-that-part-2/#comment-16173</link>
		<dc:creator><![CDATA[Aviator]]></dc:creator>
		<pubDate>Sat, 31 May 2008 06:04:57 +0000</pubDate>
		<guid isPermaLink="false">http://wattsupwiththat.wordpress.com/?p=1282#comment-16173</guid>
		<description><![CDATA[Since the 1960&#039;s, we dropped literally hundreds of Bathythermograph bouys from maritime patrol aircraft.  These relayed a temperature signal back to the aircraft where a temperature plots was traced on a graph.  We used these to plot &quot;ray path diagrams&quot; to calculate sound travel in the water in aid of tracking submarines.  All the records went ultimately &quot;up the chain&quot;, so it would be nice to know where those records are as they would provide a bit more history and fill in some of the gaps.  I know Canadian records were handed to the Russians as part of an international study - and that was during the Cold War...]]></description>
		<content:encoded><![CDATA[<p>Since the 1960&#8242;s, we dropped literally hundreds of Bathythermograph bouys from maritime patrol aircraft.  These relayed a temperature signal back to the aircraft where a temperature plots was traced on a graph.  We used these to plot &#8220;ray path diagrams&#8221; to calculate sound travel in the water in aid of tracking submarines.  All the records went ultimately &#8220;up the chain&#8221;, so it would be nice to know where those records are as they would provide a bit more history and fill in some of the gaps.  I know Canadian records were handed to the Russians as part of an international study &#8211; and that was during the Cold War&#8230;</p>
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