Why energy makes predictions more stable ✎

Original: "Universal thermokinetic decomposition of short-time information fluctuations"
arXiv:2605.29957 · 2026-05-28 · arXiv non-exclusive · independent analysis · 1 min
Energy expenditure doesn't improve the average forecast, but it does reduce the spread from attempt to attempt.

A shooter fires a series of shots. The average point of impact stays the same, but the spread of the bullet holes changes depending on how much the hands tremble. In the world of random processes, fluctuations play the role of the trembling, and dissipation, that is, energy loss, plays the role of the steadying hand.

Scientists considered a system where the future depends on the present only with some probability. For each pair of states, one can calculate how well one predicts the other. It turned out that average predictability doesn't depend on thermodynamics: it is determined only by the stationary distribution and the noise. However, the spread of predictability follows a simple rule.

The spread of predictability is made up of three parts: noise, geometric, and thermokinetic. Dissipation reduces the spread, while dynamic activity increases it.

In linear systems, these two contributions cancel each other out, so energy cannot influence the spread. Only nonlinear forces allow dissipation to suppress fluctuations. It's as if the steadying hand didn't shift the average point of impact but merely reduced the trembling of the hands.

In linear systems, dissipation and dynamic activity always cancel each other, so fluctuations in predictability do not depend on how far from equilibrium the system is. Only nonlinear forces allow energy to influence the reliability of information transfer.

F_\tau = \frac{N}{2} + F_H[-\log p_{st}] - 2\tau(\Sigma - 4T)
Fluctuations in predictability equal the sum of the noise contribution (N/2), the geometric contribution (varientropy of the stationary distribution), and the thermokinetic contribution, where dissipation (Σ) suppresses and traffic (T) amplifies the fluctuations.
\Sigma = \int dx \frac{J_{st}(x)^T D^{-1} J_{st}(x)}{p_{st}(x)}
A measure of the irreversibility of the process, determined by the stationary probability flux and the diffusion matrix.
T = \frac{1}{4} \int dx \, p_{st}(x) F(x)^T D^{-1} F(x) + \frac{1}{2} \int dx \, p_{st}(x) \nabla \cdot F(x)
A measure of the frequency and speed of transitions regardless of their direction; it reflects the kinetic activity of the system.
Concepts
fluctuation-dissipation theorem information thermodynamics natural variability information theory heat heat dissipation second law of thermodynamics Boltzmann equation Landauer's principle stochastic self organization random fluctuation stochastic dynamical system efficiency energy distribution data transmission Dynamical Systems climate network energy conservation data compression fluctuation