Coriolis effect and base forces

Click For Summary

Discussion Overview

The discussion revolves around the atmospheric Coriolis effect, its underlying forces, and the complexities of convection phenomena. Participants explore various explanations, models, and implications of the Coriolis effect in the context of atmospheric dynamics and weather patterns.

Discussion Character

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

Main Points Raised

  • One participant questions the validity of common demonstrations of the Coriolis effect, suggesting they may not accurately represent the atmospheric phenomenon and instead focus on differences in reference frames.
  • Another participant argues that the merry-go-round analogy is indeed a correct explanation of the Coriolis effect, emphasizing the importance of using a rotating frame of reference.
  • There is a discussion about the role of fictitious forces in non-inertial frames, with one participant clarifying that these forces do not correspond to the four fundamental interactions but are necessary for modeling behavior in rotating frames.
  • A participant raises concerns about the computational challenges associated with the Navier-Stokes equations and seeks mathematical demonstrations of their chaotic nature.
  • One participant proposes a theory regarding the relationship between warmer atmospheric temperatures and the nature of convection, suggesting that it may lead to fewer but more violent storms.

Areas of Agreement / Disagreement

Participants express differing views on the validity of certain explanations and models related to the Coriolis effect and its implications. There is no consensus on the best way to understand or demonstrate the phenomenon, and multiple competing perspectives remain throughout the discussion.

Contextual Notes

Participants highlight the complexity of atmospheric convection and the challenges in modeling it accurately. There are references to the limitations of using non-inertial frames and the implications of fictitious forces, but these remain unresolved within the discussion.

Jamal26
Messages
4
Reaction score
0
I wonder if anybody can point me to a good explication of the atmospheric Coriolis effect broken down into base forces. Most of the explanations I've seen are problematic, even flawed as far as I can tell, and they rarely talk about force vectors.

I've seen demonstrations, for instance a popular one is throwing a ball on a child's merry-go-round. I could be wrong, but I think this is absolutely an incorrect demonstration of the atmospheric Coriolis effect. It merely demonstrates differences in reference frames, which I believe is what the original mathematics of the Coriolis effect is about.

Why h20 aggregates and starts to rotate in the Earth's atmosphere is a very complex phenomenon as far as I can tell. There's a radial convection force for pushing hot air from the equator towards the colder polls, that definitely happens. Why it starts to rotate is another issue, I think.

I've read that rotating objects don't create rotating gravitational fields, so the idea that a rotating Earth could provide any force on air/water molecules seems dubious to me, but like I said I could be wrong. How does the Earth's rotation create any force at all on atmospheric molecules? Friction? Perhaps the curvature of the Earth plays a role?

Convection seems to be a very complex phenom. Can anybody point me to some good theory about predicting convection behavior?

I have this pet theory that warmer atmospheric temperatures make organized convection less probable, but when it does happen it becomes more violent. It would explain why we seem to have fewer, but more violent storms nowadays. Don't want to start a war about whether climate change is man made or not, just trying to understand Coriolis effect and atmospheric convection.

Thanks.
 
Physics news on Phys.org
Turns out that the difference in reference frames as illustrated by child's merry-go-round that you dismissed off hand is the correct explanation.
 
I didn't dismiss anything. Maybe you can explain a little more. For instance what are the 2 frames, and how do they contribute to actual physical aggregation & rotation of atmospheric molecules?
 
You don't care. The coriolis effect is an essential part of the dynamics when you use a rotating frame of reference. If you want to describe the dynamics of a planetary atmosphere from the perspective of an inertial (non-rotating) frame where there is no coriolis effect, good luck. Conceptually, there's no problem with this. In practice, it is so ridiculously impractical that nobody does this.
 
Jamal26 said:
I didn't dismiss anything. Maybe you can explain a little more. For instance what are the 2 frames, and how do they contribute to actual physical aggregation & rotation of atmospheric molecules?

The Earth is the merry-go-round. If you're outside of the Earth looking at it spin, than there is no Coriolis. But if you're spinning along with the Earth than the Coriolis must be included because you're using a non-inertial (accelerated) reference frame.
 
Thanks for all of your replies. I have some things to say about them, but I want to generate some diagrams that will take a bit of time first.

I want to raise an issue on the question of computational impracticability that D H brings up. There are a lot of references to the concept of the Navier-Stokes equation being "chaotic," i.e. that solutions to it are extremely sensitive to initial conditions. Does anybody have any links to this being demonstrated mathematically?

Steven Wolfram discusses the issue a bit here where he talks about where randomness comes from in modeling mathematical systems.

http://www.wolframscience.com/reference/notes/997b

I really don't know enough about what Wolfram means by "intrinsic randomness" to know what he's talking about. Does he mean the equations generate randomness that can't be explained by initial conditions? Or does he mean that there is natural, perhaps quantum mechanical, randomness generation that can't be modeled?
 
Jamal26 said:
I didn't dismiss anything. Maybe you can explain a little more. For instance what are the 2 frames, and how do they contribute to actual physical aggregation & rotation of atmospheric molecules?
You are thinking that the fictitious forces represent something real, something that can be attributed to one of the four fundamental interactions (gravitation, electromagnetism, the weak interaction, or the strong interaction). They don't. They are fictitious, hence the name. You have two choices when you look at physics from the perspective of a non-inertial frame: (1) don't do that, or (2) use fictitious forces.

Option #1 says that strictly speaking, Newtonian mechanics is only valid in an inertial frame of reference. An object that isn't subject to any external forces does not remain stationary or move along a straight line when observed from the perspective of an accelerating or rotating frame of reference. If you want to use F=ma you should be describing behavior from the perspective of an inertial frame of reference.

Option #2 says that option #1 is a non-starter. There are a number of applications where describing behavior from the perspective of an inertial frame doesn't make sense from a practical point of view. The mathematics behind those fictitious forces is perfectly valid. With them, one can indeed describe behavior from the perspective of an accelerating and/or rotating frame of reference.

You seem to be thinking that those fictitious forces have to be traceable to something real (your opening post). They aren't. They're traceable to the fact that we have intentionally decided to model behaviors such as weather from the perspective of a non-inertial frame.
 

Similar threads

  • · Replies 39 ·
2
Replies
39
Views
6K
  • · Replies 4 ·
Replies
4
Views
1K
  • · Replies 5 ·
Replies
5
Views
2K
  • · Replies 5 ·
Replies
5
Views
2K
  • · Replies 7 ·
Replies
7
Views
5K
  • · Replies 14 ·
Replies
14
Views
4K
Replies
5
Views
2K
  • · Replies 25 ·
Replies
25
Views
2K
  • · Replies 10 ·
Replies
10
Views
7K
  • · Replies 1 ·
Replies
1
Views
2K