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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? |
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