Earthquake P-wave

geophysical · 37 views
geophysicalstochastic

What It Is

P-wave arrivals from 80 earthquakes (M3.7-5.4 realized; 111-498 km) at IU.ANMO --- 40 sps broadband vertical --- impulsive, relatively anti-persistent

Interpretation

Standard analysis sees: heavy-tailed; left-skewed; red spectrum (low-frequency / 1-over-f power); time-irreversible (sharp rises, slow decay); nonstationary / drifting. The atlas finds no named structure, but the source is distinctively extreme on AutoRegressive:ar_coef_2 (-3.9z) — beyond what the standard bank predicts for it.

What standard analysis sees
tail heaviness0.87
asymmetry0.14
occupancy0.34
short-range corr0.70
long-range memory0.66
spectral colour0.06
periodicity0.43
complexity0.42
time-irreversibility0.89
volatility clustering0.70
multifractality0.73
dimensionality0.39
nonstationarity0.96
What the atlas adds
Atlas-extreme metrics the standard bank can’t predict for this source
AutoRegressive:ar_coef_2-3.9zbank-miss 1.3σ
Fractal (Mandelbrot):interior_fraction+2.3zbank-miss 1.2σ

Composition

dtypefloat64
range[-2.555e+04, 2.166e+04]
unique values5239 / 16384
mean ± std773 ± 2.49e+03

Render Gallery

Atlas Position

Nearest neighborDistance
EEG Tumor2.92cross-origin
Bearing Ball3.20cross-origin
EEG Healthy3.22cross-origin

Open in Atlas →

Which Geometries Light Up

AutoRegressiveAutoRegressive:ar_coef_2rank 303/307-2.5469
IsochronicityIsochronicity:amplitude_explorationrank 1/3072.1025
SL(2,ℝ) (Thurston)SL(2,ℝ) (Thurston):mean_spectral_radiusrank 303/3071.0199
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