Multifractal Spectrum

Spectrum width, dominant singularity, scaling nonlinearity
dynamicaldim variable2 metrics

What It Measures

Whether the signal's roughness is uniform or varies from place to place.

A monofractal signal (like fractional Brownian motion) has the same scaling behavior everywhere — zoom in anywhere and you see the same texture. A multifractal signal (like turbulence or financial returns) has smooth regions and rough regions interspersed. This geometry computes the singularity spectrum f(α) via structure functions and measures how wide it is.

Metrics

spectrum_width

The range of local scaling exponents (α_max − α_min). Zero means monofractal: every point has the same roughness. Seismic noise (ANMO) dominates the atlas at 0.78 — earthquake background has wildly varying local regularity from microseisms to cultural noise. GOES X-ray flux (0.49) is next: solar flares inject bursts of irregular scaling into a smooth background. Sawtooth wave (0.45) is surprisingly wide because the discontinuous resets create a sharp transition between smooth ramps and singular jumps. Constants score 0.0 (no scaling structure at all).

hurst_estimate

The self-affinity exponent H = τ(2)/2. Sine wave scores 0.90 (strongly persistent, smooth). Chua's circuit (0.86) is also highly persistent — its double-scroll attractor stays in each lobe for extended stretches. Prime gaps and divisor count score 0.0: number-theoretic sequences have no self-affine scaling.

Atlas Rankings

hurst_estimate
SourceDomainValue
Sine Wavewaveform0.9006
Chua's Circuitexotic0.8571
Projectile with Dragmotion0.8243
···
Divisor Countnumber_theory0.0000
Prime Gapsnumber_theory0.0000
Constant 0xFFnoise0.0000
spectrum_width
SourceDomainValue
Seismic Noise (ANMO)geophysics0.7795
GOES X-Ray Fluxastro0.4935
Sawtooth Wavewaveform0.4529
···
Constant 0xFFnoise0.0000
Constant 0x00noise0.0000
Collatz Paritynumber_theory0.0000

When It Lights Up

Multifractal width is the primary separator between "simple" dynamics (periodic, noise, low-dimensional chaos) and "complex" dynamics (turbulence, geophysical processes, financial markets). In the seismic P-wave investigation, multifractal metrics contributed to the top discriminators — earthquake arrivals temporarily broaden the local spectrum width by injecting a new scaling regime into the ambient noise.

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