Criticality Part 2: Bifurcations, Universality, and Self-Organization

Introduction

  • Recap of Part 1: tipping point vs. continuous criticality
  • What’s missing: the geometric picture, why different systems share exponents, systems that find criticality on their own
  • Goal: connect phenomenological classification to deeper mathematical frameworks

Bifurcations: The Deterministic Skeleton

Phase Portraits and Fixed Points

  • State space, trajectories, attractors
  • Fixed point stability: linearization and eigenvalues
  • Basins of attraction: which initial conditions lead where

Catalog of Local Bifurcations

Saddle-Node Bifurcation

  • Normal form: $\dot{x} = r + x^2$
  • Two fixed points collide and annihilate
  • The canonical “tipping point”—no smooth return
  • Examples: extinction thresholds, financial crises, regime shifts in ecosystems

Transcritical Bifurcation

  • Normal form: $\dot{x} = rx - x^2$
  • Two fixed points exchange stability
  • Connection to exponential growth model from Part 1

Pitchfork Bifurcation

  • Supercritical: $\dot{x} = rx - x^3$ (smooth symmetry breaking)
  • Subcritical: $\dot{x} = rx + x^3$ (discontinuous jump)
  • Connection to continuous vs. tipping point criticality

Hopf Bifurcation

  • Fixed point gives way to limit cycle
  • Supercritical vs. subcritical variants
  • Examples: oscillations in predator-prey systems, electrical circuits

Global Bifurcations

  • Homoclinic and heteroclinic bifurcations
  • Why local analysis isn’t always enough
  • Catastrophe theory: Thom’s classification

Interactive: Bifurcation Explorer

  • Phase portrait that deforms as control parameter changes
  • Visualize fixed point creation/destruction/stability exchange
  • Show corresponding bifurcation diagram

From Bifurcations to Statistical Mechanics

The Role of Many Degrees of Freedom

  • Single ODE → lattice of coupled units
  • Fluctuations and noise enter naturally
  • Mean-field theory: averaging over neighbors recovers bifurcation-like equations

Landau Theory of Phase Transitions

  • Free energy as a function of order parameter
  • Equilibrium: minimize free energy
  • Taylor expansion near transition: $F(m) = a(T)m^2 + bm^4 + \ldots$
  • Connection to pitchfork bifurcation

Order Parameter Behavior Near Criticality

  • Power-law scaling: $m \sim |T - T_c|^\beta$
  • Critical exponent $\beta$ characterizes the transition
  • Mean-field prediction vs. reality: fluctuations matter in low dimensions

Correlation Length and Susceptibility

  • Correlation length $\xi$: how far do fluctuations propagate?
  • $\xi \sim |T - T_c|^{-\nu}$ diverges at criticality
  • Susceptibility $\chi \sim |T - T_c|^{-\gamma}$: response to perturbations diverges
  • Critical slowing down: relaxation time also diverges

Universality: Why Details Don’t Matter

The Puzzle

  • Liquid-gas transition in water and magnetization in iron follow same power laws
  • Microscopic physics completely different
  • How can this be?

What Determines Universality Class

  • Dimensionality of space
  • Symmetry of order parameter (scalar, vector, etc.)
  • Range of interactions (short vs. long range)
  • What doesn’t matter: lattice structure, precise interaction strengths, chemical details

The Renormalization Group Idea

Coarse-Graining

  • Block spins: average over small regions
  • Ask: what effective Hamiltonian describes the coarse-grained system?
  • Iterate: zoom out repeatedly

RG Flow and Fixed Points

  • Parameters flow under coarse-graining
  • Fixed points of the flow = scale-invariant systems = critical points
  • Behavior near fixed point determines critical exponents

Intuitive Picture

  • At criticality, zooming out doesn’t change statistical properties
  • The system “looks the same” at all scales
  • This self-similarity is the origin of power laws

Scaling Relations

  • Critical exponents aren’t independent
  • Relations like $\alpha + 2\beta + \gamma = 2$ (Rushbrooke)
  • Follow from self-consistency of RG picture
  • Reduces number of independent exponents

Table of Universality Classes

Class Examples $\beta$ $\nu$ $\gamma$
2D Ising Uniaxial magnets, lattice gas 1/8 1 7/4
3D Ising Liquid-gas, binary mixtures ~0.326 ~0.630 ~1.237
Mean-field High dimensions, long-range 1/2 1/2 1
2D Percolation Porous media, networks 5/36 4/3 43/18
3D Percolation Composite materials ~0.41 ~0.88 ~1.80

Fractals at Criticality

Why Fractals Emerge

  • No characteristic length scale at $p_c$ or $T_c$
  • Structures must be self-similar
  • Fractal geometry is the natural description

Fractal Dimension

  • Definition: $M(L) \sim L^{d_f}$ where $d_f$ is fractal dimension
  • For percolation cluster at $p_c$: $d_f < d$ (spatial dimension)
  • 2D percolation: $d_f = 91/48 \approx 1.896$
  • The cluster fills space “incompletely”

Fractal Dimension as Critical Exponent

  • Related to other exponents through scaling relations
  • $d_f = d - \beta/\nu$ connects geometry to thermodynamics
  • Measuring $d_f$ gives information about universality class

Examples of Critical Fractals

  • Percolation clusters at threshold
  • Ising domain boundaries at $T_c$
  • Coastlines and river networks (approximately)
  • Diffusion-limited aggregation

Interactive: Box-Counting on Critical Cluster

  • Generate percolation cluster at $p = p_c$
  • Overlay boxes of decreasing size
  • Plot $\log N$ vs. $\log (1/\epsilon)$
  • Slope gives fractal dimension

Self-Organized Criticality

The Tuning Problem

  • In standard criticality: must tune control parameter precisely to $p_c$
  • But power laws appear everywhere in nature
  • Who is doing the tuning?

SOC: Criticality Without Tuning

  • Some systems naturally evolve toward critical state
  • Separation of timescales is key: slow drive, fast relaxation
  • System “self-organizes” to the boundary between stability and instability

The BTW Sandpile Model

Rules

  • 2D lattice, each site has “sand grains” $z_{ij}$
  • Slowly add grains at random sites
  • If $z_{ij} \geq 4$, site topples: loses 4 grains, neighbors each gain 1
  • Toppling can trigger neighbors → avalanche
  • Grains fall off at boundaries

Emergent Behavior

  • System reaches statistical steady state
  • Avalanche size distribution follows power law: $P(s) \sim s^{-\tau}$
  • No characteristic avalanche size
  • Always poised at criticality

Other Examples of SOC

  • Earthquakes: Gutenberg-Richter law $P(E) \sim E^{-b}$
  • Forest fires: burned area distribution
  • Mass extinctions: species loss events
  • Neural avalanches in brain activity
  • Solar flares: energy release distribution

Controversies and Limitations

  • Is true SOC common, or are power laws often misidentified?
  • Many claimed power laws don’t survive rigorous statistical testing
  • Alternative mechanisms: finite-size effects, superposition, tuning to different points
  • SOC requires specific conditions: slow drive, fast relaxation, no characteristic scale in driving

Interactive: Sandpile Simulation

  • Add grains one by one
  • Visualize avalanches as they propagate
  • Plot avalanche size histogram (log-log)
  • Show approach to power-law distribution

Synthesis: A Unified View of Criticality

The Common Thread

  • Criticality = diverging correlation length = loss of characteristic scale
  • Power laws, fractals, and scale invariance are manifestations of same phenomenon
  • Universality: only symmetry and dimension matter near the fixed point

Hierarchy of Descriptions

Bifurcation Theory (deterministic, low-dimensional)
         ↓ add noise, many degrees of freedom
Mean-Field / Landau Theory (averaged, approximate)
         ↓ include fluctuations properly
Renormalization Group (full critical behavior)
         ↓ special dynamics
Self-Organized Criticality (criticality as attractor)

Mapping the Landscape

Framework Tipping Point Continuous Transition
Bifurcations Saddle-node, subcritical Supercritical pitchfork, transcritical
Phase transitions First-order Second-order (continuous)
Order parameter Discontinuous jump Power-law approach to zero
Correlation length Finite Diverges
Hysteresis Often present Absent
Critical exponents Not applicable Universal values

Early Warning Signals

  • Approaching tipping points: critical slowing down
  • Variance and autocorrelation increase before transition
  • Flickering between states
  • Potential for prediction and intervention

Open Questions

  • Criticality in non-equilibrium systems: active matter, driven systems
  • Quantum criticality: phase transitions at zero temperature
  • Criticality and computation: is the brain critical? Why might this be advantageous?
  • Machine learning on critical systems: can neural networks learn critical exponents?

Conclusion

  • Criticality connects dynamical systems, statistical mechanics, and geometry
  • The same mathematical structures appear across physics, biology, and social systems
  • Understanding criticality gives tools for prediction, control, and recognizing universal patterns
  • Much remains unknown, especially in non-equilibrium and living systems

Sources

  • Nonlinear Dynamics and Chaos by Steven H. Strogatz
  • Statistical Mechanics by James Sethna (especially Chapter 12 on RG)
  • Scale Invariance and Beyond edited by Dubrulle, Graner, Sornette
  • How Nature Works by Per Bak (original SOC book)
  • Critical Phenomena in Natural Sciences by Didier Sornette
  • Clauset, Shalizi, Newman: “Power-Law Distributions in Empirical Data” (arXiv:0706.1062)