Why does less dense air rise and more dense air come down?

In summary, in order for less dense air to rise, the pressure on the bottom face of the cube must be greater than the pressure on the top face.
  • #1
vcsharp2003
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Homework Statement
I am trying to explain a common phenomenon in nature. The phenomenon is that warm air in room rises in a room and colder air at the top of the room settles down closer to the floor of the room.
Relevant Equations
##\rho = \frac {m} {v}##, where ##\rho## is density of material and ##m## , ##v## are mass and volume of a certain amount of the material
My answer given below seems incomplete.

Since warm air causes the air to expand in volume, so its density becomes less as compared to the colder air at the top of the room. After this, I generally find all books saying the less dense air rises and more dense air from top comes down and therefore this phenomenon occurs in nature.

But, how would I explain why less dense air rises and more dense air falls. I have tried to explain it using the diagram below which shows two cubes of air at the top and bottom of the room. The arrows for each cube indicate the pressure acting on the cube from all directions. Wouldn't the force due to pressure on each face of the cube be balanced by the force due to pressure on the opposite face of the cube? If yes, then I cannot explain why the cube of air at the bottom would rise since it needs to have a net upward force acting on it in order for it to rise. If the upward pressure is greater than the downward pressure on the bottom cube, then I could say that the less dense cube of air will rise since it would end up having a net upward force.

Or perhaps, there is another explanation for this.

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  • #2
vcsharp2003 said:
Wouldn't the force due to pressure on each face of the cube be balanced by the force due to pressure on the opposite face of the cube?
For the sides, yes. For the top and bottom, no. Remember that the fluid (air or liquid) near the bottom of the box is holding up more stuff against gravity than the fluid near the top of the box. This means there is a greater pressure on that part of the fluid, which is exerted against the bottom of the box, lifting it up.

In other words, the pressure at the bottom of the box is greater than at the top, leading to a net upward force against the box.
 
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  • #3
Drakkith said:
the pressure at the bottom of the box is greater than at the top, leading to a net upward force against the box.
Quite so, and that underpins Archimedes' Principle.
 
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  • #4
Drakkith said:
Remember that the fluid (air or liquid) near the bottom of the box is holding up more stuff against gravity than the fluid near the top of the box. This means there is a greater pressure on that part of the fluid, which is exerted against the bottom of the box, lifting it up.
Can we say the following?

The pressure on the top face of bottom cube is greater than pressure at the bottom face of the same cube because the temperature decreases as we go up and for a gas ##P \propto T## (at constant volume), so we can say that top face has a lower temperature and therefore lower pressure.
 
  • #5
haruspex said:
Quite so, and that underpins Archimedes' Principle.
So, can we apply Archimedes' Principle to each of air cubes in the diagram in OP? Normally, we apply this principle only when a solid is partially or fully submerged in a fluid.
 
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  • #6
Not sure I understand what is being said, so I drew a diagram (as always for me!)
airRising.png

Now, I'm as troubled as you (or whoever) that when there is no solid box, there can't be two different pressures in the same place. So I guess that as soon as there is the smallest difference in density, something starts moving and we can add terms like F=ma to bring the pressures at the interface back in line.
If the packet of air ascends at a steady speed, I'm still struggling with that one.
 

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  • #7
Does having cold fluid on top and warm fluid below violate any of Newton's 3 laws of motion for static equilibrium? Is this condition of static equilibrium stable?
 
  • #8
Chestermiller said:
Does having cold fluid on top and warm fluid below violate any of Newton's 3 laws of motion for static equilibrium? Is this condition of static equilibrium stable?
Warm air at bottom would expand and this would mean that the force of normal reaction on bottom cube from the cube just above it would have decreased so the cube at bottom would expand upwards till its pressure on top fave equals the pressure on its top face from cube just above it.
 
  • #9
vcsharp2003 said:
... Wouldn't the force due to pressure on each face of the cube be balanced by the force due to pressure on the opposite face of the cube? If yes, then I cannot explain why the cube of air at the bottom would rise since it needs to have a net upward force acting on it in order for it to rise. If the upward pressure is greater than the downward pressure on the bottom cube, then I could say that the less dense cube of air will rise since it would end up having a net upward force.

Or perhaps, there is another explanation for this.
For that to happen in a closed room or system, there must be a heat source or heat sink that keeps a flow of energy.
The result will be a draft circulation in the room, within which air is heated or cooled at an area or point, being displaced or forced to move by air that has not been yet heated or cooled.

If that source or sink equals its temperature with the air’s, a stratification process begins, when circulation or draft stops (there is no more energy for that), and an equilibrium of temperatures and densities slowly happens, in which top layers of warmer air transfer thermal energy to the lower layers of cooler air.
 
  • #10
vcsharp2003 said:
Warm air at bottom would expand and this would mean that the force of normal reaction on bottom cube from the cube just above it would have decreased so the cube at bottom would expand upwards till its pressure on top fave equals the pressure on its top face from cube just above it.
This is incorrect. If it is warmer, it had already expanded.
 
  • #11
Chestermiller said:
This is incorrect. If it is warmer, it had already expanded.
Sorry, I don't get how a Newton's Law could be applied in this scenario, except in the way I explained in my OP.
 
  • #12
vcsharp2003 said:
Sorry, I don't get how a Newton's Law could be applied in this scenario, except in the way I explained in my OP.
I said it doesn't violate any of Newton's laws of motion for equilibrium to be established. What I'm saying is that a fluid stratified from warm below to cold on top is an allowable equilibrium state, although it is unstable, and will result in an inversion flow with the slightest perturbation.
 
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  • #13
vcsharp2003 said:
Can we say the following?

The pressure on the top face of bottom cube is greater than pressure at the bottom face of the same cube because the temperature decreases as we go up and for a gas ##P \propto T## (at constant volume), so we can say that top face has a lower temperature and therefore lower pressure.
The pressure difference is not primarily caused by temperature. Note that there are parts of the atmosphere where temperature rises with altitude instead of falling, and yet buoyancy works just fine there. There are also temperature inversions in the oceans, and yet submarines work just fine there too. Also, water isn't very compressible, so its change in density vs temperature is extremely small.
 
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  • #14
vcsharp2003 said:
Normally, we apply this principle only when a solid is partially or fully submerged in a fluid.
You are treating the parcel of air as a body, and the surrounding air is a fluid.
 
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  • #15
Lnewqban said:
For that to happen in a closed room or system, there must be a heat source or heat sink that keeps a flow of energy.
I donot see the connection between this and the question being asked.
 
  • #16
Merlin3189 said:
Not sure I understand what is being said, so I drew a diagram (as always for me!)
View attachment 318718
Now, I'm as troubled as you (or whoever) that when there is no solid box, there can't be two different pressures in the same place. So I guess that as soon as there is the smallest difference in density, something starts moving and we can add terms like F=ma to bring the pressures at the interface back in line.
If the packet of air ascends at a steady speed, I'm still struggling with that one.
I do not understand your diagram. The pressures inside the box differ by 2d1h-dh. Shouldn’t that be just d1h?
 
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  • #17
vcsharp2003 said:
because the temperature decreases as we go up
Whoa! That’s a whole other topic (see "6. the lapse rate" at https://www.physicsforums.com/insights/frequently-made-errors-climate-science-greenhouse-effect/) and plays no part in the question you asked in post #1.

The pressure difference with altitude is to do with the weight of air, in exactly the same way that pressure increases with depth in water.

I admit there is a conundrum in your post #1 scenario, though. If we put a flimsy box around the parcel of warm air, we are saying it rises because the density is less inside the box. But in that case the internal pressure difference between top and bottom should be less than the external pressure difference between top and bottom; on the other hand, the internal pressure should be the same as the external pressure everywhere on the box boundary, or the box would deform accordingly.
To resolve this we need to consider the dynamics. If we warm a parcel of air the first thing that happens is its pressure increases. As soon as that starts to happen, its excess pressure over the surroundings causes it to expand. Now Archimedes' Principle kicks in and causes it to rise bodily. So the mistake was treating it as though internal and external pressures have to balance everywhere exactly all the time.
 
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  • #18
haruspex said:
I donot see the connection between this and the question being asked.
What is the question being asked?

My answer reflects what I understood (incorrectly perhaps) after reading the “Homework statement”:

“I am trying to explain a common phenomenon in nature. The phenomenon is that warm air in room rises in a room and colder air at the top of the room settles down closer to the floor of the room.”

Maybe @vcsharp2003 could clarify how the warm air was originally (and unnaturally) at the bottom of the room and the colder air at the top.
 
  • #19
Lnewqban said:
My answer reflects what I understood (incorrectly perhaps) after reading the “Homework statement”:
Sadly, that is quite common on this forum. The question @vcsharp2003 is asking us is more specific and is further down in post #1.
 

1. Why does less dense air rise?

Less dense air rises because it is lighter than the surrounding air. This is due to the fact that it has a lower mass per unit volume compared to the denser air around it. This creates a buoyant force that causes the less dense air to rise.

2. How does the density of air affect its movement?

The density of air plays a crucial role in its movement. Less dense air will always rise while more dense air will sink. This is because the less dense air is buoyant and exerts a force on the surrounding air, causing it to rise. On the other hand, the denser air is pulled down by gravity, causing it to sink.

3. Why does more dense air come down?

More dense air comes down because it is heavier than the surrounding air. This is due to its higher mass per unit volume compared to the less dense air around it. The force of gravity pulls the denser air down, causing it to sink.

4. How does temperature affect the density of air?

Temperature has a direct impact on the density of air. As temperature increases, the air molecules gain energy and spread out, leading to a decrease in density. On the other hand, as temperature decreases, the air molecules lose energy and become more compact, resulting in an increase in density.

5. What role does air pressure play in the movement of air?

Air pressure is closely related to air density and plays a significant role in the movement of air. As air rises, it expands and cools, leading to a decrease in air pressure. Conversely, as air sinks, it compresses and warms, resulting in an increase in air pressure. This difference in air pressure causes the movement of air from areas of high pressure to areas of low pressure.

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