Tohoku Aftershock Intervals

geophysical · 37 views
geophysicalstochastic

What It Is

Log inter-event times of ~35k Tohoku 2011 M≥2 aftershocks --- Omori-law decay with temporal clustering, 3 months post-mainshock (ISC/JMA catalog, public domain)

Interpretation

Standard analysis sees: left-skewed; high-complexity (noise-like). The atlas finds no named structure, but the source is distinctively extreme on Nonstationarity:change_quantiles_low (+2.8z) — beyond what the standard bank predicts for it.

What standard analysis sees
tail heaviness0.72
asymmetry0.05
occupancy0.58
short-range corr0.44
long-range memory0.58
spectral colour0.60
periodicity0.36
complexity0.92
time-irreversibility0.71
volatility clustering0.36
multifractality0.41
dimensionality0.76
nonstationarity0.43
What the atlas adds
Atlas-extreme metrics the standard bank can’t predict for this source
Nonstationarity:change_quantiles_low+2.8zbank-miss 1.3σ
Ulam Spiral (Square):polynomial_concentration-2.1zbank-miss 1.5σ

Composition

dtypefloat64
range[0, 8.337]
unique values11865 / 16384
mean ± std5.17 ± 1.15

Render Gallery

Atlas Position

Nearest neighborDistance
Voyager 1 X-band3.04cross-origin
Earthquake Intervals3.19
VLF Radio (Eclipse)3.24

Open in Atlas →

Which Geometries Light Up

2-adic › 2-adic:valuation_spectral_concentrationrank 306/3060.0465
Catch24 › Catch24:DN_OutlierInclude_p_001_mdrmdrank 4/3060.3663
Nonstationarity › Nonstationarity:change_quantiles_lowrank 5/3060.1032
Ulam Spiral (Square) › Ulam Spiral (Square):polynomial_concentrationrank 303/3060.0200
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