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Atmospheric Flight
9-12 Grade Reading
Imperceptible to the human eye, air is in constant, frantic motion at
the surface of the Earth. As in any gas, the molecules (in Earth's case
nitrogen and oxygen) are moving and bumping into each other at various
speeds. Near the Earth's surface they move at an average of 1,090 miles
per hour. Warm the air and the molecules move faster, cool the air and
the molecules move more slowly. The impacts of billions and billions of
moving molecules cause pressure. At the surface of the Earth the air pressure
is greater than at the top layer of the atmosphere 50+ miles above the
Earth's surface.
Imagine a long tube standing up from the Earth's surface all the way up
to the top of the atmosphere, about 50 miles straight up. The weight of
all that air in that tube is pressing on the Earth's surface. How much does
all that air weigh? If the area in the cross section of the tube is one
square foot, then the weight of all the air in the tube would be more than
2000 pounds! The normal atmospheric pressure at the Earth's surface is 2,116
pounds per square foot.
Now, suppose we climb up the tube to a place about 4 miles above the
Earth's surface. If we could drill a hole in the tube at that point and
measure the pressure there, we would find that the pressure is much less,
only about 1000 pounds per square inch. Why is the pressure less? Because
there is less air in the tube above this point there is less weight of
air pressing down.
But if the whole atmosphere is about 50 miles thick, how can it be that
half the pressure is caused by the air in the first 4 miles? What happens
is that the pressure of the air above it, compresses it. The air closer
to the Earth's surface has more density, since the molecules are closer
together. Near the top of the atmosphere, there is very low air density
because there is very little pressure compressing the molecules together.
But at the surface of the Earth, the density is much higher. So, the layers
of air in the lower atmosphere are more compressed than those above it,
and adding much more to the pressure below. As one moves up in altitude,
the pressure and density are reduced very quickly.
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