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<?xml-stylesheet type="text/xsl" href="http://www.jets.dk/cs/rss.xsl" media="screen"?><rss version="2.0" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:slash="http://purl.org/rss/1.0/modules/slash/" xmlns:wfw="http://wellformedweb.org/CommentAPI/"><channel><title>Aviation Top 100 questions</title><link>http://www.jets.dk/cs/forums/21/ShowForum.aspx</link><description>Questions about the Aviation Top 100 list.</description><dc:language>en-US</dc:language><generator>CommunityServer 2.0 (Build: 60526.2668)</generator><item><title>Re: Anyone knows the aviation metrology?</title><link>http://www.jets.dk/cs/forums/thread/2128.aspx</link><pubDate>Thu, 23 Jan 2003 05:59:55 GMT</pubDate><guid isPermaLink="false">a23efcf1-9e75-4ff9-be18-cd9cb68b9485:2128</guid><dc:creator>rainman_02</dc:creator><slash:comments>0</slash:comments><comments>http://www.jets.dk/cs/forums/thread/2128.aspx</comments><wfw:commentRss>http://www.jets.dk/cs/forums/commentrss.aspx?SectionID=21&amp;PostID=2128</wfw:commentRss><description>This is in pilotspeak, so probably not as technical as you want.&lt;br /&gt;&lt;br /&gt;1) There is no real realtionship.  The troposphere is narrower at the poles and wider at the equator.&lt;br /&gt;&lt;br /&gt;2) Temp inversion is a low to the ground effect, usually from a clear night with calm winds.  The cooler air, because of its greater density, settles close to the ground, and the warmer air forms a blanket above it in a temperature inversion.  Thus, if you have winds, they mix the air and no inversion.&lt;br /&gt;&lt;br /&gt;3) See above.  You're now talking about temperature lapse rate.  -2* C per 1,000 feet of altitude up from sea level.  On a standard day, sea level is 15* C.  Therefore, 3,000m or 9,900 feet is approximately -5* C ... on a standard day.  There are many things that can change the temperature of a region, most important of which is the jet stream.&lt;br /&gt;&lt;br /&gt;4) The ozone layer is in top of the stratosphere.  The stratosphere is from 6 - 30 miles altitude.&lt;br /&gt;&lt;br /&gt;5) There's lots of aerodynamics and fluid flow for Mach and the speed of sound.  http://www.mathpages.com/home/kmath282/kmath282.htm  Go here.</description></item><item><title>Anyone knows the aviation metrology?</title><link>http://www.jets.dk/cs/forums/thread/2123.aspx</link><pubDate>Tue, 21 Jan 2003 07:05:48 GMT</pubDate><guid isPermaLink="false">a23efcf1-9e75-4ff9-be18-cd9cb68b9485:2123</guid><dc:creator>lucasiu</dc:creator><slash:comments>0</slash:comments><comments>http://www.jets.dk/cs/forums/thread/2123.aspx</comments><wfw:commentRss>http://www.jets.dk/cs/forums/commentrss.aspx?SectionID=21&amp;PostID=2123</wfw:commentRss><description>Can anyone answer the questions on aviation metrology?&lt;br /&gt;&lt;br /&gt;1. How is the height of the troposphere affected by ground temperature and pressure? Is higher ground temperature means higher troposphere height?&lt;br /&gt;&lt;br /&gt;2. Someone said there is temperature inversion when the ground temperature is low. What is the temperature inversion rate for different sea level temperature?&lt;br /&gt;&lt;br /&gt;3. If the rule of temperature inversion is true, then how to explain the extremely low temperature of Vostok, which is over 3000m above sea level, and has minimum temperature of -88C? What is the temperature inversion rate for different land height?&lt;br /&gt;&lt;br /&gt;4. Can anyone tell me the height of ozone layer?&lt;br /&gt;&lt;br /&gt;5. Can anyone tell me what is the speed of sound at different height at different ground temperature and pressure?&lt;br /&gt;&lt;br /&gt;Please answer the questions with figures stating the characteristics of the atmosphere.&lt;br /&gt;&lt;br /&gt;Thanks.</description></item></channel></rss>