Atmospheric Pressure Above the Sea Level

Click For Summary
SUMMARY

The atmospheric pressure decreases exponentially with height, described by the equation P(h) = P0e-h/H, where H is the scale height, approximately 7 km. At sea level, the pressure is 101325 Pa, and at 5.5 km, it is half that value. To find the height where the pressure is one-eighth of sea level, the correct setup involves using the scale height in conjunction with the hydrostatic equation and the ideal gas law. The correct height is determined to be approximately 16.5 km, contrasting with the initial incorrect calculation of 1.38 km.

PREREQUISITES
  • Understanding of exponential functions and their applications in physics.
  • Familiarity with the hydrostatic equation: dp/dz = -ρg.
  • Knowledge of the ideal gas law: ρ = (pM)/(RT).
  • Concept of scale height in atmospheric science.
NEXT STEPS
  • Study the derivation of the scale height formula H = (RT)/(Mg).
  • Learn about the relationship between pressure and altitude in the context of the atmosphere.
  • Explore the implications of the ideal gas law on atmospheric pressure calculations.
  • Investigate the variations of temperature with altitude and its effect on scale height.
USEFUL FOR

Students studying physics or atmospheric science, educators teaching concepts of pressure and altitude, and anyone interested in understanding the behavior of gases under varying atmospheric conditions.

anomalocaris
Messages
23
Reaction score
0

Homework Statement



The atmospheric pressure deceases exponentially with height. At 5.5 km, the pressure is half that at sea level. At what height is the pressure one eighth that of sea level?

Homework Equations


All I can think of is Pat=ρgh

I know 1 atm=101325 Pa=101.325 kPa and that this is the atmospheric pressure at sea level.

The Attempt at a Solution


\frac{101325 Pa}{2}=ρ(9.8 m/s2)(5.5 km)
50662.5 Pa=ρ(9.8 m/s2)(5500 m)
50662.5 Pa=ρ(53900 m2s-1)
ρ=0.93993 kg/m3

I thought that in solving for density, I could change the equation to make
\frac{101325 Pa}{8}=(0.93993 kg/m3)(9.8 m/s2)h
and then solve for h.
h=(12665.625 Pa)/((0.93993 kg/m3)(9.8 m/s2))
h=1380 m=1.38 km

This was my homework and for the life of me I do not know how I got this right, because the answer I found above is "incorrect." The correct answer should be 16.5 km. Does anyone have any ideas as to where I am going wrong? I'm wondering if I used the wrong formula? I do not think I understand the concept so well.

Thank you!
 
Physics news on Phys.org
The key to this problem statement is the words deceases exponentially with height. So

P = P0e-h/H

where H is the so called scale height, and is equal to the height interval over which the pressure decreases by a factor of e.
 
Chestermiller said:
The key to this problem statement is the words deceases exponentially with height. So

P = P0e-h/H

where H is the so called scale height, and is equal to the height interval over which the pressure decreases by a factor of e.
Oh okay! We didn't go over this in lecture and it is not in my textbook. I'm not familiar with this formula. From what equation does one derive this?

For this particular problem, would I set it up like this:

101325 Pa/8=(101325 Pa/2)e-5.5 km/H

Thank you so much for your help!
 
Last edited:
anomalocaris said:
From what equation does one derive this?
It's what is meant by the information you were given: atmospheric pressure deceases exponentially with height. That is, there exist some constants P0 and H s.t. the pressure at height h is P0e-h/H.
101325 Pa/8=(101325 Pa/2)e-5.5 km/H
No, you have no unknowns in there, and you have the relationship backwards.
Given that P(h) = P0e-h/H, what equations do you get for h=0 (sea level) and h = 5.5km?
 
I agree with haruspex on his answer to the first part of your question. As to the second part, where does the relation come from: It comes from a combination of the hydrostatic equation and the ideal gas law:

dp/dz = -ρg

where ρ is the density of air and g is the acceleration of gravity. From the ideal gas law,

ρ = (pM)/(RT)

where M is the molecular weight of air.

Combining the two equations, we get

dp/dz = -p / H

where H is called the scale height:

H = (RT)/(Mg)

In reality, since T varies with altitude z, H does also. But, often people use an average value over the troposphere to estimate how the pressure varies with altitude. Often, the scale height is taken to be constant at ~ 7 km.
 

Similar threads

Replies
3
Views
2K
  • · Replies 8 ·
Replies
8
Views
4K
  • · Replies 6 ·
Replies
6
Views
5K
  • · Replies 9 ·
Replies
9
Views
1K
  • · Replies 4 ·
Replies
4
Views
4K
  • · Replies 10 ·
Replies
10
Views
2K
  • · Replies 12 ·
Replies
12
Views
2K
Replies
2
Views
1K
  • · Replies 9 ·
Replies
9
Views
3K
  • · Replies 11 ·
Replies
11
Views
4K