Localized Cascade Risk at the 16 September 2026 Model-D Phase Boundary: A Pre-Registered Fast-Slow Stabilization and Falsification Protocol

This pre-registration fixes a limited-disclosure Model-D hypothesis before a model-defined 16 September 2026 phase boundary. It tests whether localized thermosphere/ionosphere residual structure can be materially stronger than globally smoothed representations suggest, and whether a predeclared fast/slow representation improves holdout performance over a single-timescale baseline. Established space-weather literature supports strong spatial and temporal heterogeneity in thermospheric density and nontrivial storm-time model uncertainty; it does not establish the Model-D date, the fixed internal anchor mu=0.218, or a deterministic cascade. The release defines explicit falsification criteria and a model-independent emergency fallback while withholding the full live-state resolver, private joining/synchronization logic, operational thresholds and any actuation code.

Authors

Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2026-09-15
DOI
https://doi.org/10.5281/zenodo.22775628
Primary Topic
Ionosphere and magnetosphere dynamics
Type
preprint
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preprint

Localized Cascade Risk at the 16 September 2026 Model-D Phase Boundary: A Pre-Registered Fast-Slow Stabilization and Falsification Protocol

Jessica Schmidt
Zenodo (CERN European Organization for Nuclear Research)
Ionosphere and magnetosphere dynamics
preprint

Localized Cascade Risk at the 16 September 2026 Model-D Phase Boundary: A Pre-Registered Fast-Slow Stabilization and Falsification Protocol

Jessica Schmidt
preprint en

Abstract

This pre-registration fixes a limited-disclosure Model-D hypothesis before a model-defined 16 September 2026 phase boundary. It tests whether localized thermosphere/ionosphere residual structure can be materially stronger than globally smoothed representations suggest, and whether a predeclared fast/slow representation improves holdout performance over a single-timescale baseline. Established space-weather literature supports strong spatial and temporal heterogeneity in thermospheric density and nontrivial storm-time model uncertainty; it does not establish the Model-D date, the fixed internal anchor mu=0.218, or a deterministic cascade. The release defines explicit falsification criteria and a model-independent emergency fallback while withholding the full live-state resolver, private joining/synchronization logic, operational thresholds and any actuation code.

Zenodo (CERN European Organization for Nuclear Research)
Climate action
Ionosphere and magnetosphere dynamics
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