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Автор: Vázquez Broquá, Juan Ignacio
Формат: Recurso digital
Мова:Англійська
Опубліковано: Zenodo 2026
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Онлайн доступ:https://doi.org/10.5281/zenodo.19600331
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author Vázquez Broquá, Juan Ignacio
author_facet Vázquez Broquá, Juan Ignacio
contents <p>We introduce Geometric Transfer Entropy (GTE), a measure of directional<br>information flow between time series that preserves the grade structure of the<br>Clifford-algebraic embedding underlying the Geometric Signal Dynamics (GSD)<br>programme. Building on the kinematic embedding and geometric product of Vázquez<br>Broquá (2026a), the spectral bivector identity of Vázquez Broquá (2026b), the joint<br>embedding for cointegration of Vázquez Broquá (2026c), and the antisymmetric<br>entropy HAS of Vázquez Broquá (2026d), we define GTEX→Y (τ ) as the sum of<br>two grade-resolved channels: a scalar channel T(0)X→Y that captures transfer of alignment/level information, and a bivector channel T(2)X→Y that captures transfer of rotational information (velocity, curvature, phase). The net flow ΦXY = GTEX→Y −GTEY →X decomposes analogously into a scalar and a rotational flow, ΦXY = Φ(0) XY + Φ(2) XY . Across seven benchmark systems, GTE recovers the classical Schreiber transfer entropy on level-coupled linear systems, detects velocity-coupled systems four times more strongly than Schreiber TE, and correctly identifies the direction<br>of coupling in stochastic oscillators where classical TE reverses sign. The bivariate signature (Φ(0), Φ<br>(2)) produces a taxonomy of dynamical coupling mechanisms and yields geometric diagnostics of cointegration, common confounding, and pure rotational transfer that classical information flow measures cannot provide.</p>
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spellingShingle Geometric Transfer Entropy: A Grade-Resolved Directional Information Flow for Dynamical Coupling of Time Series
Vázquez Broquá, Juan Ignacio
transfer entropy
clifford algebra
geometric signal dynamics
directional coupling
non-commutative information
cointegration
coupled oscillators
<p>We introduce Geometric Transfer Entropy (GTE), a measure of directional<br>information flow between time series that preserves the grade structure of the<br>Clifford-algebraic embedding underlying the Geometric Signal Dynamics (GSD)<br>programme. Building on the kinematic embedding and geometric product of Vázquez<br>Broquá (2026a), the spectral bivector identity of Vázquez Broquá (2026b), the joint<br>embedding for cointegration of Vázquez Broquá (2026c), and the antisymmetric<br>entropy HAS of Vázquez Broquá (2026d), we define GTEX→Y (τ ) as the sum of<br>two grade-resolved channels: a scalar channel T(0)X→Y that captures transfer of alignment/level information, and a bivector channel T(2)X→Y that captures transfer of rotational information (velocity, curvature, phase). The net flow ΦXY = GTEX→Y −GTEY →X decomposes analogously into a scalar and a rotational flow, ΦXY = Φ(0) XY + Φ(2) XY . Across seven benchmark systems, GTE recovers the classical Schreiber transfer entropy on level-coupled linear systems, detects velocity-coupled systems four times more strongly than Schreiber TE, and correctly identifies the direction<br>of coupling in stochastic oscillators where classical TE reverses sign. The bivariate signature (Φ(0), Φ<br>(2)) produces a taxonomy of dynamical coupling mechanisms and yields geometric diagnostics of cointegration, common confounding, and pure rotational transfer that classical information flow measures cannot provide.</p>
title Geometric Transfer Entropy: A Grade-Resolved Directional Information Flow for Dynamical Coupling of Time Series
topic transfer entropy
clifford algebra
geometric signal dynamics
directional coupling
non-commutative information
cointegration
coupled oscillators
url https://doi.org/10.5281/zenodo.19600331