The Earth's Atmosphere
Chemical Composition:
- 78% N2
- 21% O2
- 1% CO2, H2O, Ar, Ne, O3
Why is the atmosphere not H and He (like the Sun, or Jupiter)?
Why is there an atmosphere at all (compare to Mercury, or
the Moon)?
What is the pressure/density structure of the atmosphere?
The pressure scale height of an atmosphere (or "how thick is it?")
The pressure of an atmosphere is determined by its
weight -- the force of gravity pulling it down. What
is this effect called?
From this we know that
Since the atmosphere is very thin,
we can assume plane parallel geometry
so that we have instead
Now, we can't assume constant density like we did for the
Earth's interior. Gases are compressible, and density and pressure are related
by the ideal gas law:
Substituting for density, we get
Rearranging terms, we have the following differential equation:
So let's integrate. P goes from
P0 to P as z goes from 0 to z:
and so we get
or
Let's define the pressure scale
height to be
so that we end up with
We see that:
- Pressure and density drop as height increases
- Scale height defines the distance over which the
pressure drops by 1/e = 0.37
- Scale height smaller for heavier atoms/molecules.
Example: What is the scale
height of the Earth's atmosphere?
It's mostly N2, so m=2 x 14 x 1.66x10-27
kg = 4.65x10-26 kg
and we also have g=9.8 m/s2 and T ~ 300
K
so we get H = 9x103 m = 9 km
Pretty thin...
(Try this at home: What would
the scale height be for a hydrogen atmosphere on the Earth?)