If I understand correctly, these stacked layers of air don't fly off into space because they are contained by a dome of ice.
Yes. They simply freeze due to expansion.
What evidence is there that these gasses cool enough up there ? Hydrogen gas and helium freeze only at extremely low temparature.
How can very thin layers of atmosphere freeze into a solid structure ?
It depends what you mean by a solid structure. It's basically a frozen skin.
I was thinking of a dome that is solid as if made of water ice. A frozen skin is a normally pliable sheet at such low temperature that it is not pliable anymore. I fail to see how frozen hydrogen and helium can be more like a frozen skin than as a sheet of water ice.
Even so, how could that frozen skin be formed ? I know if no example of a gas depositing into a frozen skin in the absense of a substrate (i.e. some surface to deposit on).
Why is that structure a dome ?
Most likely because we live inside a sort of sphere...a cell, if you like.
So we are living on an infinite plane inside a sphere under a frozen skin dome made from hydrogen and helium.
What is the boundary of that sphere made of ? How big is it ? Does it inersect with the earth ?
What are the dimensions of that dome ?
I have absolutely no clue whatsoever.
OK. For that ice dome no dimensions can be provided that are consistent with the evidence.
Are the sun and moon inside that ice dome ? Are the stars outside of it ?
Because it will go dormant and freeze by then.
If I understand correctly, going further over Antarctica, the distance from the sun keeps increasing and thus it becomes colder and colder.
I don't go with the Antarctica stuff in the terms others think.[4]
Towards the outer gradient the central Earth energy (sun) cannot agitate the matter due to distance[5], so gradually the matter changes until frozen is varying degrees up to the dome.
[4] Antractica is the continent at the south pole. In the monopole flat earth it is a land mass that forms a rim around the known world. Apparently you don't believe in that land mass. Does that mean that there is merely a water ice rim without land that rises above sea level ? I will assume that for now and use the term southern rim or water ice rim to refer to it.
Let's define terms. The southern rim or ice rim is the frozen wall of water ice that surrounds the habitable area of the earth. On the round globe that would be Antarctica. The air ice rim is some distance farther south beyond the southern ice ring. It is where the atmopheric gasses are depositing.
[5] In science, what you refer to as agitating matter is called heating. Matter, including gas, loses heat (agitation) through radiation. That is called cooling.
I don't understand your last sentence, but you appear to claim that gas is depositing (turning from gas to solid) outside of the southern rim. Hence, the amount of gaz decreases and the amount of solid increases, correct ?
The air from within the Antarctic rim flows over there and transitions directly from gaseous to solid state. Is that correct ?
The rimj is a rim somewhere on Earth. This is no rim.[6] It's one upwardly curved structure. A concave build.
[6] I assume 'this' is referring to the dome.
OK, but you haven't answerd my question. I was asking about the atmospheric gasses flowing over the southern ice ring, not the dome.
What is that, a gradual freeze ?
Yes.
I assume you have misunderstood my question. I had asked what a gradual freeze is.
What are those waves you are referring to ? Are you talking about electromagnetic waves, i.e. light from the sun ?
Pressure waves of agitation due to the central energy (sun)....yes.
So the waves you are referring to are actually the sun's light.
Are you claiming that light consists of pressure waves ?
If the air far over the Antarctic rim freezes solid, does that cause the atmospheric pressure over there to drop ?
The pressure would fluctuate the more you pushed towards the gradient, from high to lower pressure, until you would simply have to stop and where vehicles would simply seize up....etc.
I assume that with 'pushing towards the gradient' you mean, going where the atmospheric pressure is lower, i.e. closer to the air ice ring. Why would pressure fluctuate there ?
So yes, farther away, pressure would be lower. Hence there would be net wind from the high pressure area inside the southern rim to the low pressure region far outside of it. Does that wind exist in your reality ?
What is all that rest of the atmosphere ? Is there atmosphere that does not flow over the Antarctic rim ? If so, how does it get recycled ?
It's a cyclone.
The cyclone would be super strong at the centre of Earth....the feed for the sun's energy and the return back to atmosphere, creating a central cyclone that spans out, getting weaker and weaker depending on the movement of the energy reflections.
Needs more explanation but basically, something like this.
So there is one part of the atmosphere that flows over the Southern rim and deposits further away at the air ice rim. There is also another part, wich is a cyclone, which is strongest at the centre of the earth. Where is that centre of the earth ? Underground ?
You seem to mean that that cyclone is powered by the sun and returns back to the atmosphere. Where does that cyclone return to the atmopshere ? What is it's entry point ? Does the cyclone also leave the atmosphere that way ?
Then allegedly that cyclone spans out and becomes I imagine like a real weather phenomenon.
Because it will go dormant and freeze by then.
How will that stop more air moving there "going dormant and freezing" until there is virtually no gaseous air left?
Because air moving there would still be in energy range for agitation. It would be like brushing the walls.
So at the air ice rim air is depositing. Yet some air is still moving, presumably the air that is arriving to replace the air that is depositing (which takes less volume, making room for more air). So we have high pressure inside the southern ring, low pressure at the air ice ring and intermediate pressure at the southern ring. So one would expect air at the southern ring to flow outward to the air ice ring. Now according to you the air still in gas form at the air ice ring prevents that from happening because it still contains heat. How does that work ?
Added to that is the question of the helium-hydrogen ice dome, which presumably touches the earth somewhere. Where does it touch the earth at the air ice rim, that rim thereby forming the base of the dome ?