Atmospheric Density - Equation to Model from Sea Level to 200km

In summary, the conversation discusses different equations and methods for modeling atmospheric density at different altitudes. There is not a single simple equation that accurately models atmospheric pressure, but there are several formulas that can be used for rough estimations. These formulas have certain assumptions and limitations and can vary depending on the standard atmosphere being used.
  • #1
ZachWeiner
6
0
Hey, does anyone have an equation that roughly models atmospheric density from sea level to about 200 km up?
 
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  • #2
There's not much of an equation for atmospheric pressure that's simple. If you have a CRC handbook you could look up a few values. You should know, as well, that it's quit variable at higher altitudes, dependent on solar activity.
 
  • #3
Hi ZachWeiner,
Pressure at a height "h" is given by :
P=(Patm)*e^(-Mgh/RT) [Patm is the pressure at sea level]
And D=PM/RT
But there is an assumption that T is const. this formula will only enable you to calculate the density roughly. So do not use it if you want accurate answers.
 
  • #4
aniketp said:
Hi ZachWeiner,
Pressure at a height "h" is given by :
P=(Patm)*e^(-Mgh/RT) [Patm is the pressure at sea level]
And D=PM/RT
But there is an assumption that T is const. this formula will only enable you to calculate the density roughly. So do not use it if you want accurate answers.

I have no excuse for it, but in response to this question, I actually tried an exponential curve of pressure vs. height, and fit it to two points of data; sea level and 100 Km. It was off by 28% at 50 Km. Very disappointing.

To get a decent curve fit, P = P0 * exp(ah^3 + bh^2 + h) might do it.
 
  • #5
what do you need to model it for? pretty much any fluid mechanics text will tell you in a table at the back.

lol.. if u really want to model it, put all the numbers into excel and graph it
 
  • #6
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FAQ: Atmospheric Density - Equation to Model from Sea Level to 200km

What is atmospheric density?

Atmospheric density is the measure of the mass of air particles per unit volume in Earth's atmosphere. It is affected by factors such as altitude, temperature, and air pressure.

How is atmospheric density calculated?

The equation used to model atmospheric density from sea level to 200km is called the Barometric formula. It takes into account the variation in air pressure with altitude and is based on the ideal gas law.

Why is it important to study atmospheric density?

Studying atmospheric density is important for understanding the behavior of Earth's atmosphere and how it affects weather patterns and climate change. It also has practical applications in fields such as aviation and space exploration.

How does atmospheric density change with altitude?

As altitude increases, atmospheric density decreases. This is because there is less air above, causing lower air pressure and therefore fewer air particles per unit volume.

What is the significance of 200km in the equation for atmospheric density?

200km is the approximate boundary between Earth's atmosphere and outer space. The atmospheric density at this altitude is very low, making it an important point of reference for understanding the behavior of Earth's atmosphere.

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