Temperature - Effect on atmospheric pressure.

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Discussion Overview

The discussion centers on the correlation between temperature and atmospheric pressure, specifically examining why Titan has a higher atmospheric pressure than Earth despite similar atmospheric mass. Participants explore theoretical and mathematical aspects of atmospheric pressure, density, and temperature effects.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested
  • Mathematical reasoning

Main Points Raised

  • Some participants question the correlation between temperature and atmospheric pressure, particularly in the context of Titan's atmospheric conditions compared to Earth's.
  • One participant suggests that Titan's atmosphere is denser than Earth's, attributing this to lower temperatures and higher pressure, leading to a greater overall density.
  • Another participant provides calculations comparing Titan's and Earth's atmospheric pressures, noting that the expected increase in pressure due to atmospheric weight does not align with observed values, suggesting temperature may play a role.
  • Some participants argue that the mass of an atmosphere cannot be measured directly and must be computed based on various assumptions, which complicates the discussion.
  • There is mention of the scale height of the atmosphere and its relation to temperature, with some participants expressing uncertainty about how to apply this concept to estimate air pressure at sea level.
  • One participant emphasizes that pressure at sea level is an input variable and cannot be computed solely from scale height without additional data.
  • Another participant discusses the dynamic nature of the atmosphere, highlighting how temperature changes can lead to pressure fluctuations and the movement of air masses.

Areas of Agreement / Disagreement

Participants express differing views on the relationship between temperature and atmospheric pressure, with no consensus reached on the underlying causes of Titan's atmospheric conditions compared to Earth. Some calculations and assumptions are challenged, but no definitive conclusions are drawn.

Contextual Notes

Limitations include the reliance on assumptions for atmospheric mass calculations and the complexity introduced by varying gravitational effects with distance from the planet's center. The relationship between scale height and pressure remains unresolved, with participants noting the need for additional data to make accurate estimations.

ExcessRed
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What is correlation between temperature and atmospheric pressure?

For example, why does Titan have 1.6 times the atmospheric pressure of Earth despite having pretty much the same atmospheric 'weight', for lack of better term. (Total atmospheric mass times gravity.)

EDIT: Is this the right forum?
 
Last edited:
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ExcessRed said:
What is correlation between temperature and atmospheric pressure?

For example, why does Titan have 1.6 times the atmospheric pressure of Earth despite having pretty much the same atmospheric 'weight', for lack of better term. (Total atmospheric mass times gravity.)

EDIT: Is this the right forum?

Not sure where you got the mass and gravity product being the same between Earth and Titan from, but it follows from the fact that surface pressure is due to the weight of the air, and weight is mass times gravity.

The correlation between temperature and pressure is that the two related by the density - Titan's atmosphere at the surface is several times denser than Earth's. As the gas is roughly three times colder and 1.5 times higher pressure, the density is 4.5 times Earth's.
 
Titan's atmosphere is about 1.19 times as massive as Earth's overall. [Coustenis, Athéna and Taylor, F. W. (2008). Titan: Exploring an Earthlike World. World Scientific. p. 130.] Since only relative change matters in this context, we can say titan has 1.19 "earth atmospheric masses" - or EAMs - for simplicity instead of converting to a particular unit.

Gravity of titan is 1.35 m/s^2 and titan has about 8.3×10^7 km^2 surface area.

So Titan has an atmospheric pressure of (1.19*1.35) / 8.3×10^7 = 1.94×10^-8 EAM m/s^2 / km^2

Earth, on the other hand has an EAM of 1 (Duh!), gravity of 9.8 m/s^2, and surface area of 5.1×10^8 meaning an atmospheric pressure of (1*9.8)/5.1×10^8 = 1.92×10^-8 EAM m/s^2 / km^2

This implies that the surface pressure of Titan and Earth is roughly the same (1% increase), so obviously there is more to it than just the weight of the atmosphere divided by surface area since the figure is supposed to be more like a 60% increase.

I was told that discrepancy was due to temperature, but if that's not the case... please tell me what cause is, because I'm clearly missing something!
 
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That total mass figure for Titan is incorrect. You might want to check against another source.
 
The figure for atmospheric mass was correct.

I found the answer: temperature increase the density of the atmosphere. As density increases, the atmosphere compresses and sits closer to the surface of the planet. Gravity now has a greater effect on the mass of the atmosphere, since the mass is closer to the planet and the atmospheric weight increases.

Mass times gravity divided by surface area only holds true if gravity constant regardless of distance.

EDIT: I'm reading more now to confirm, but I believe to properly calculate the pressure you have to use the 'http://en.wikipedia.org/wiki/Scale_height" ' of the atmosphere - for which temperature is a factor.
 
Last edited by a moderator:
ExcessRed said:
The figure for atmospheric mass was correct.

I found the answer: temperature increase the density of the atmosphere. As density increases, the atmosphere compresses and sits closer to the surface of the planet. Gravity now has a greater effect on the mass of the atmosphere, since the mass is closer to the planet and the atmospheric weight increases.

Mass times gravity divided by surface area only holds true if gravity constant regardless of distance.

EDIT: I'm reading more now to confirm, but I believe to properly calculate the pressure you have to use the 'http://en.wikipedia.org/wiki/Scale_height" ' of the atmosphere - for which temperature is a factor.

Hi ExcessRed

Possibly. One thing to keep in mind is that the mass of an atmosphere can't be measured directly, but must be computed according to various assumptions.

Another point is that the volume of the column of atmosphere which presses down on a given area of surface increases as the radial distance increases, exactly compensating for the decrease in the force of gravity.

To see why, consider a square metre of surface area bounded by radii from the centre of a planet. As we move outwards, the area bounded by those radii increases. At twice the planet's radius, the area is now 4 square metres. Thus the volume contained within a unit height times the area enclosed has increased four-fold. But that larger volume's weight (enclosed mass by gravity) has also declined due to the inverse square law of gravity, thus decreasing four-fold.

To work out the scale-height is complicated by gravity's decline with radial distance, but you can probably figure it out for yourself.
 
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I have figured out how to calculate the scale height - it's a pretty simple formula - but I don't know exactly how to use this value to get a more accurate estimation of air pressure at sea level.

Any suggestions?
 
ExcessRed said:
I have figured out how to calculate the scale height - it's a pretty simple formula - but I don't know exactly how to use this value to get a more accurate estimation of air pressure at sea level.

Any suggestions?

Sea-Level pressure isn't related to the scale height. It's an input variable, not one you can compute without other data (for example pressure at a given altitude and the behaviour of the atmosphere's temperature with altitude.) Scale height is related directly to the ratio of the kinetic energy of the air at a given location, and the gravitational potential needed to match that energy. Pressure doesn't feature in the equation. But, of course, the rate at which pressure declines with altitude is directly related to the scale-height via the Barometric Formula. Look it up.
 
I have looked it up. Assuming scale height is not related to air pressure at sea level, then what is a different way to estimate the affect of temperature on air pressure at sea level?
 
  • #11
That's the same formula with scale height integrated rather than calculating it separately.

That equation uses one height to determine the pressure at another height by calculating the change based on scale height. Basically it requires you to have one pressure before you can solve for the other. I have no pressure - that's what I want to estimate. Woe.

If there is some fancy maths I can use to circumvent this problem ... advise would be great!
 
  • #12
Ahh, ok. My mistake.
 
  • #13
Drakkith said:
Ahh, ok. My mistake.

Meh - no worries. This question has become more math than science at this point! I should probably post a simplified query with nothing but the equation in the math forum. There's a math forum right? :P
 
  • #14
ExcessRed said:
I have looked it up. Assuming scale height is not related to air pressure at sea level, then what is a different way to estimate the affect of temperature on air pressure at sea level?

If the temperature rises in a small volume then for a short time pressure increases - but it immediately tries to reach a new equilibrium by expanding. That's why the atmosphere is in ceaseless motion over differently heated parts of the surface - convection lifts parcels of hot air and vapour into the sky to cool off, and cold air and rain drops down again. Then there's different winds carrying energy back and forth between sea and land. The net result, over the whole surface, is the heat added by the Sun is equal to the heat radiated by the atmosphere. And, when the inputs and outputs are added up, the equatorial regions gain more, while the polar regions lose more, thus a net flow of heat from the equator to the poles.
 

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