Most kind of you to reply. I couldn’t catch all that; I’m mathematically semiliterate. I was just wondering if the key idea “small differences” (in initial states) manifests at the output end (the weather forecast) too. I mean it’s quite possible (given what I know, not much) that (say) an atmospheric pressure difference of 0.01 Pa in the output could mean the difference between rain and shine. Given what you wrote I’m wrong, oui? If I were correct then the chaos resides in the weather, not the output (where the differences are as negligible as in the inputs).
I know that there’s something called the Lyapunov exponent. Could we “diminish the chaos” if we use logarithms, like with the Richter scale for earthquakes? I was told that logarithms, though they rise rapidly in the beginning, ultimately end up plateauing: log 1 million—log 100 = 4 (only)??? log 100 inches rain and log 1 inch rain = 2 (only)?
I hope you’ll forgive me if I’m talking out of my hat here. It’s an interesting topic and I tried my best to read and understand what I read.
I know that there’s something called the Lyapunov exponent. Could we “diminish the chaos” if we use logarithms, like with the Richter scale for earthquakes?
This is a neat question. I think the answer is no, and here’s my attempt to describe why.
The Lyapunov exponent measures the difference between the trajectories over time. If your system is the double pendulum, you need to be able to take two random states of the double pendulum and say how different they are. So it’s not like you’re measuring the speed, or the length, or something like that. And if you have this distance metric on the whole space of double-pendulum states, then you can’t “take the log” of all the distances at the same time (I think because that would break the triangle inequality).
Hopefully, not talking out of my hat, but the difference between the final states of a double pendulum can be typed:
Somewhere in the middle of the pendulum’s journey through space and time. I’ve seen this visually and true there’s divergence. This divergence is based on measurement of the pendulum’s position in space at a given time. So with initial state A, the pendulum at time Tn was at position P1 while beginning with initial stateB(|A−B|≈0), the pendulum at time Tn was at position P2. The alleged divergence is the difference |P1−P2|, oui? Take in absolute terms, |P1−P2|=106, but logarithmically, log|P1−P2|=only 6.
At the very end when the pendulum comes to rest. There’s no divergence there, oui?
Any physical system has a finite amount of mass and energy that limit its possible behaviors. If you take the log of (one variable of) the system, its full range of behaviors will use fewer numbers, but that’s all that will happen. For example, the wind is usually between 0.001 m/s (quite still) and 100 m/s (unprecedented hurricane). If you take the base-10 log, it’s usually between −3 and 2. A change of 2 can mean a change from .001 to .1 m/s (quite still to barely noticeable breeze) or a change from 1 m/s to 100 m/s (modest breeze to everything’s gone). For lots of common phenomena, log scales are too imprecise to be useful.
Chaotic systems can’t be predicted in detail, but physics and common sense still apply. Chaotic weather is just ordinary weather.
Most kind of you to reply. I couldn’t catch all that; I’m mathematically semiliterate. I was just wondering if the key idea “small differences” (in initial states) manifests at the output end (the weather forecast) too. I mean it’s quite possible (given what I know, not much) that (say) an atmospheric pressure difference of 0.01 Pa in the output could mean the difference between rain and shine. Given what you wrote I’m wrong, oui? If I were correct then the chaos resides in the weather, not the output (where the differences are as negligible as in the inputs).
I know that there’s something called the Lyapunov exponent. Could we “diminish the chaos” if we use logarithms, like with the Richter scale for earthquakes? I was told that logarithms, though they rise rapidly in the beginning, ultimately end up plateauing: log 1 million—log 100 = 4 (only)??? log 100 inches rain and log 1 inch rain = 2 (only)?
I hope you’ll forgive me if I’m talking out of my hat here. It’s an interesting topic and I tried my best to read and understand what I read.
Gracias, have an awesome day.
This is a neat question. I think the answer is no, and here’s my attempt to describe why.
The Lyapunov exponent measures the difference between the trajectories over time. If your system is the double pendulum, you need to be able to take two random states of the double pendulum and say how different they are. So it’s not like you’re measuring the speed, or the length, or something like that. And if you have this distance metric on the whole space of double-pendulum states, then you can’t “take the log” of all the distances at the same time (I think because that would break the triangle inequality).
Hopefully, not talking out of my hat, but the difference between the final states of a double pendulum can be typed:
Somewhere in the middle of the pendulum’s journey through space and time. I’ve seen this visually and true there’s divergence. This divergence is based on measurement of the pendulum’s position in space at a given time. So with initial state A, the pendulum at time Tn was at position P1 while beginning with initial stateB(|A−B|≈0), the pendulum at time Tn was at position P2. The alleged divergence is the difference |P1−P2|, oui? Take in absolute terms, |P1−P2|=106, but logarithmically, log|P1−P2|=only 6.
At the very end when the pendulum comes to rest. There’s no divergence there, oui?
Any physical system has a finite amount of mass and energy that limit its possible behaviors. If you take the log of (one variable of) the system, its full range of behaviors will use fewer numbers, but that’s all that will happen. For example, the wind is usually between 0.001 m/s (quite still) and 100 m/s (unprecedented hurricane). If you take the base-10 log, it’s usually between −3 and 2. A change of 2 can mean a change from .001 to .1 m/s (quite still to barely noticeable breeze) or a change from 1 m/s to 100 m/s (modest breeze to everything’s gone). For lots of common phenomena, log scales are too imprecise to be useful.
Chaotic systems can’t be predicted in detail, but physics and common sense still apply. Chaotic weather is just ordinary weather.