Colder with increasing altitude.

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Discussion Overview

The discussion revolves around the phenomenon of temperature decreasing with increasing altitude, particularly in the context of mountains and hill stations. Participants explore various explanations related to atmospheric pressure, gas expansion, heat absorption, and the effects of altitude on air density and temperature.

Discussion Character

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

Main Points Raised

  • Some participants suggest that temperature drops with altitude due to decreasing pressure and the expansion of gas, which leads to cooling as it does work against gravitational forces.
  • Others argue that air at higher altitudes absorbs less heat due to its lower density and the inability to conduct heat effectively from the ground.
  • It is noted that clouds act as a heat shield, preventing heat from reaching the upper atmosphere, which contributes to lower temperatures above cloud cover.
  • Some participants question the relationship between gravitational force and temperature, seeking clarification on how decreasing gravitational force affects gas temperature during expansion.
  • There are discussions about the role of radiation in heat transfer, with some participants asserting that heat from the ground is more significant than radiation from the air above clouds.
  • One participant mentions the complexity of temperature variations in different atmospheric layers, referencing the stratosphere and thermosphere where temperature trends differ from the troposphere.
  • Concerns are raised about the effects of altitude on breathing and the perception of temperature at hill stations compared to plains.

Areas of Agreement / Disagreement

Participants express multiple competing views regarding the mechanisms behind temperature changes with altitude. There is no consensus on the explanations provided, and several points remain contested or unclear.

Contextual Notes

Some claims rely on assumptions about heat transfer mechanisms and the behavior of gases under varying pressure and temperature conditions. The discussion does not resolve the complexities of these interactions or the specific conditions under which they apply.

Who May Find This Useful

This discussion may be of interest to individuals exploring atmospheric science, meteorology, or those curious about the physical principles governing temperature variations with altitude.

  • #61
olivermsun said:
So you would prefer the explanation that radiative equilibrium, moderated by convection (where the adiabatic cooling comes in), is the "cause" of the decreasing temperature with altitude?

Not sure it's necessary to specify equilibrium, but yes, the primary cause is atmospheric absorption/reradiation.
 
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  • #62
haruspex said:
If I asked you what caused sand dunes in the desert you wouldn't say it was the angle of repose; you'd say it was the wind.
Saying that the angle of repose is responsible for sand dunes is exactly what you have done by saying that greenhouse gases are the cause of the lapse rate.

Take away the sand and you don't get sand dunes. Take away the 99% of the dry atmosphere that is transparent to thermal IR and you don't get anything like our atmosphere.

To say that one specific thing is the cause of a complex process is fallacious reasoning.
 
  • #63
D H said:
Saying that the angle of repose is responsible for sand dunes is exactly what you have done by saying that greenhouse gases are the cause of the lapse rate.
I didn't say GHGs cause the lapse rate, and that wasn't the original question.

The analogy runs like this:
Q1. Why do sand dunes form?
A1. The wind blows sand uphill.
Q2. What stops them getting really steep?
A2. Gravity
Q3. Why doesn't gravity flatten them out?
A3. The angle of repose.

Q1. Why does it tend to get colder as you go higher?
A1. Because the Earth is a source of radiation that GHGs trap and release
Q2. If I do the maths on that, the temperature gradient would be much steeper than it is.
A2. Convection tends to move excess heat upwards
Q3. Why doesn't convection bring it back to uniform?
A3. Because of adiabatic cooling.

To say that one specific thing is the cause of a complex process is fallacious reasoning.
The lapse rate, i.e. the specific gradient observed, is certainly a result of the whole shebang. I won't object violently to giving that answer also to the question as posed, but I certainly object to giving adiabatic cooling as the main or only explanation. There would be a cooling with altitude without convection and adiabatic cooling; but without some primary cause such as GHGs or diurnal variation there would be no convection, no adiabatic cooling, and no temperature drop with altitude.
 
  • #64
haruspex said:
Not sure it's necessary to specify equilibrium, but yes, the primary cause is atmospheric absorption/reradiation.

That seems fair.
 
  • #65
It's always hard to specify a "cause" of anything, it somewhat depends on the logic being used. But my perspective is, greenhouse gases "try to" cause the temperature to fall at high altitude (or more correctly, be warm at low altitude), and then the temperature gradient they "try" to cause is too steep to be stable, so convection sets the actual gradient. But radiation and thermal equilibrium is what sets the ball rolling, so that does kind of sound like a cause, and indeed convection is not a cause of it being colder at altitude, it is a cause of it not being even colder than it is at altitude (hence it should be thought of as a warming effect). Thus I would say, in agreement with haruspex, that the greenhouse effect "causes" the temperature to be higher at low altitude, but it is convection that determines the actual gradient. Shall we mince words thusly, or just agree with D_H that a complex process is best understood by the process itself, rather than any labels we might tend to hang on it? The labels "cause" and "effect" are surprisingly vague in physics, as they mean something rather different in an equilibrium process than they do in a time varying process (in the latter, they have to do with time ordering, whereas in the former, they have more to do with "if I had the power, what would I achieve the greatest impact by changing").
 
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