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Document time-varying forcing rationale in ensemble README
Co-Authored-By: Claude Opus 4.6 (1M context) <noreply@anthropic.com>
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simulations/glorysv12-curvilinear/ensemble/README.md

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**8 breeding cycles**: Empirically sufficient for convergence. Monitor with
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`breed_vectors.py status` — the per-variable RMS should stabilize by cycle 5–6.
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### Time-varying forcing during breeding
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Breeding is performed under the full time-varying atmospheric (ERA5) and ocean
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boundary (GLORYS) forcing — not frozen or climatological forcing. This is the
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correct approach for two reasons:
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1. **Bred vectors should capture the growing modes of the actual system
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trajectory.** The fastest-growing instabilities in the North Atlantic depend
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on the seasonal forcing state — Gulf Stream separation behavior differs
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between winter and summer, deep convection only occurs in winter, and summer
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stratification modulates baroclinic instability. Breeding under realistic
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forcing ensures the perturbations project onto modes that are actually
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growing in the flow regime the ensemble will simulate.
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2. **The forcing cancels in the bred vector computation.** Both the control and
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perturbed members see identical forcing. The bred vector (`member − control`)
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isolates perturbation growth only — the common forcing signal drops out.
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Time-varying forcing drives the background state but does not contaminate
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the perturbation structure.
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If breeding were performed under constant (frozen) forcing, the perturbations
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would lock onto modes specific to that frozen state and need time to readjust
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when exposed to evolving forcing in the production ensemble — partially
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defeating the purpose of breeding.
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**Seasonal timing**: Ideally, start breeding from the same season as the
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production ensemble start date, so the bred vectors are tuned to the relevant
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flow regime. For multi-year ensembles this is a minor consideration — bred
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vectors readjust within the first few weeks of the production run regardless.
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## Workflow
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### Prerequisites

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