Why is the air less dense higher up you go?

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Discussion Overview

The discussion centers around the question of why air density decreases with altitude. Participants explore various factors influencing air density, including temperature, pressure, and gravitational effects, while considering both theoretical and conceptual aspects of atmospheric science.

Discussion Character

  • Exploratory
  • Technical explanation
  • Conceptual clarification
  • Debate/contested

Main Points Raised

  • Some participants suggest that air expands and becomes less dense at higher altitudes, but question how this occurs in cooler temperatures.
  • Others propose that gravitational effects create higher pressure at lower altitudes, influencing density.
  • It is noted that temperature relates to the kinetic energy of air molecules, while density is defined as mass per volume.
  • Some argue that warm air is less dense than cold air, but emphasize the importance of considering pressure when comparing densities at different altitudes.
  • A participant introduces the ideal gas equation to explain the relationship between pressure, volume, and density.
  • Another point raised is that air pressure is the weight of the air above, leading to less air and lower pressure at higher altitudes, which affects density.
  • One participant elaborates on how heating occurs near the Earth's surface and how this affects air density and temperature with altitude.
  • There is a discussion about the compressibility of gases and how this affects air density, particularly in relation to the distribution of air in the atmosphere.

Areas of Agreement / Disagreement

Participants express various viewpoints on the relationship between temperature, pressure, and density, indicating that multiple competing views remain. The discussion does not reach a consensus on the mechanisms involved.

Contextual Notes

Some assumptions about the ideal gas behavior and the effects of temperature and pressure on density are not fully resolved. The discussion also touches on the complexity of atmospheric layers and the varying properties of air at different altitudes.

sameeralord
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Hello everyone :smile:

I have a quick question why is the air less dense higher up you go. I can understand air expands and the volume is bigger hence less dence but that only happens if it is warm, higher you go it is cooler so how does air expand. Thank you! :smile:
 
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Think gravitation.
 
Borek said:
Think gravitation.

Thanksfor the reply. I can understand how this would create higher pressure lower down but how is this related to density. Warm air is more dense than cold air so how is cold air at the top be less dense.
 
Temperature is more or less equivalent to the total kinetical energy of the individual molecules. Density is the total mass (amount) of the molecules in a certain volume.
 
Andre said:
Temperature is more or less equivalent to the total kinetical energy of the individual molecules. Density is the total mass (amount) of the molecules in a certain volume.

Thanks a lot for your reply :redface: it makes sense but now I'm bit confused about density and I'll ask my question in form of a picture

http://www.hotlinkfiles.com/files/2614660_unkyz/Untitled.jpg
 
Pressure is average force per area. If you have fewer molecules hitting an area over a given time, and/or the molecules are traveling more slowly, then there is less pressure.
 
sameeralord said:
Warm air is more dense than cold air

Quite the opposite - assuming constant pressure, warm air is less dense.

But you can't directly compare densities, not taking pressures into account. The higher you go, the lower the pressure - so even if the air is colder, its density is lower.
 
Borek said:
Quite the opposite - assuming constant pressure, warm air is less dense.

But you can't directly compare densities, not taking pressures into account. The higher you go, the lower the pressure - so even if the air is colder, its density is lower.

Yes that is what I meant I just wrote it wrong way around. Why is density lower with lower pressure. For example in my picture. The gas molecules at the red area, if I want to look at the density of these molecules do I take the blue box or the yellow box as my volume.

Thanks for the help so far :smile:
 
sameeralord said:
Why is density lower with lower pressure.

Start with ideal gas equation:

n=\frac {PV} {RT}

Density is mass per volume, mass is number of moles times molar mass. Combine it all.
 
  • #10
What we feel as air pressure is the weight of the air above us, thus the higher you go the less air there is above you. To remain in equilibrium the force must be equalised in all directions, thus why it's even in the horizontal directions. Remember that air is compressible - it occupies less volume (gets denser) the more it is squeezed, thus it's denser where the pressure is higher near the ground and as you get higher the amount of weight from a given volume of air decreases, so the pressure squeeze eases off increasingly rapidly with altitude.
 
  • #11
sameeralord said:
Hello everyone :smile:

I have a quick question why is the air less dense higher up you go. I can understand air expands and the volume is bigger hence less dense but that only happens if it is warm, higher you go it is cooler so how does air expand. Thank you! :smile:
Air is less dense with altitude because there is less mass above a given elevation. It is the weight (force due to gravity) of the mass of air above a given elevation that produces the pressure.

At sea level, the air has a pressure of 1 atmosphere (1 atm, or ~14.7 psia, or 0.10132 MPa). With increasing elevation, the pressure decreases to the vacuum in space.

Heating occurs near the Earth's surface via conduction from the Earth's surface and direct heating, which is proportional to the density.

http://www.grc.nasa.gov/WWW/K-12/airplane/atmos.html
Variations in air properties extend upward from the surface of the Earth. The sun heats the surface of the Earth, and some of this heat goes into warming the air near the surface. The heated air is then diffused or convected up through the atmosphere. Thus the air temperature is highest near the surface and decreases as altitude increases. The speed of sound depends on the temperature and also decreases with increasing altitude. The pressure of the air can be related to the weight of the air over a given location. As we increase altitude through the atmosphere, there is some air below us and some air above us. But there is always less air above us than was present at a lower altitude. Therefore, air pressure decreases as we increase altitude. The air density depends on both the temperature and the pressure through the equation of state and also decreases with increasing altitude.
. . . .

Heating is also a function of composition, which also varies with altitude.
http://www.physicalgeography.net/fundamentals/7b.html
From an altitude of 20 to 50 kilometers, temperature increases with an increase in altitude. The higher temperatures found in this region of the stratosphere occurs because of a localized concentration of ozone gas molecules. These molecules absorb ultraviolet sunlight creating heat energy that warms the stratosphere. Ozone is primarily found in the atmosphere at varying concentrations between the altitudes of 10 to 50 kilometers. This layer of ozone is also called the ozone layer.

http://en.wikipedia.org/wiki/Ozone_layer
http://www.nas.nasa.gov/About/Education/Ozone/ozonelayer.html

Notice that the lowest 10% of the atmosphere holds 90% of the air. This is because gases are compressable. In a huge pile of feathers the bottom-most feathers become compressed under the weight of the feathers above them. Likewise the lower levels of the atmosphere are filled with compressed air while the upper levels, such as the stratosphere, contain very 'thin' uncompressed air. Although the stratosphere layer is over four times thicker than the lower atmosphere, the stratosphere holds so little gas that ozone is still considered one of the minor trace-gases of the overall atmosphere.
 

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