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#1
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![]() other than the heat t was a nice day in mid-Misouri - lots of fluffy clouds with pancake-flat bottoms. Driving with my daughter, we were talking about clouds and weather and how there really was moisture below the clouds but the temperature was just a bit too high to condense it. the converstaion drifted to dew point and how each 1000 feet represents a 4.5 degree F temperature change. she asked, basically, 'if its 104 here and the cloud bottoms are at 6000 feet it must be (104 - 6*4.5) 77 degrees there'. I dialed asos and the dew point was actually 63. who can help with this calculus? does density altitude play a role in the equation? |
#2
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On 7/25/2012 9:43 AM, HankC wrote:
the converstaion drifted to dew point and how each 1000 feet represents a 4.5 degree F temperature change. ... I dialed asos and the dew point was actually 63. who can help with this calculus? does density altitude play a role in the equation? I'm no expert on the theory, but keep in mind that the 4.5/1000 temperature change is a rule of thumb, and local conditions can be different for a variety of reasons. I find that cloud bases are seldom exactly where they are predicted to be. Vaughn |
#3
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On Jul 25, 9:00*am, Vaughn wrote:
On 7/25/2012 9:43 AM, HankC wrote: the converstaion drifted to dew point and how each 1000 feet represents a 4.5 degree F temperature change. ... I dialed asos and the dew point was actually 63. who can help with this calculus? does density altitude play a role in the equation? I'm no expert on the theory, but keep in mind that the 4.5/1000 temperature change is a rule of thumb, and local conditions can be different for a variety of reasons. I find that cloud bases are seldom exactly where they are predicted to be.. Vaughn lol - just realized it's my eyeball-o-meter giving the cloud altitudes. it's been a while since it was calibrated and could easily be off by 2000 feet ![]() |
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