Jett
Well-Known Member
I like it...but that's the part I'm having trouble explaining to my students. I understand at 10,000 feet you'd have less molecules because the density decreased but how are you cutting through the molecules faster just because there are less molecules going through the pitot-tube?
You aren't cutting through the molecules faster. You are moving through the molecules at exactly the same rate. But now the molecules are further apart. Ask your student if he could swim faster in syrup or water...
That is one of the concepts I'm still trying to understand. Cold air is less dense than warm air, but as you gain altitude, there are less air molecules, making the air less dense. Does the loss in molecules make up for the increased density of cold air?
Edit: I meant to say that cold air is more dense, not less.
Temperature is a measure of molecular energy. Your classic Mercury thermometer is being "squeezed" by the air around it. When the air is hot, there is a lot of molecular energy, the atoms that make up the air are basically vibrating and bouncing off the thermometer. The force they impart into the Mercury causes it to rise in the tube. At high altitude there are far fewer atoms to bounce off the thermometer, the temperature decreases.
When you think of colder air being more dense think of it at sea level. Yes, cold air at sea level is always denser than warm air at sea level. When you start going up in altitude the pressure will decrease because there is less atmosphere above it pushing down, wether it is cold or warm to begin with won't change this.