CHYPHNX / MISSIONGRID / POSEIDON
ARCHIVE ONLINE
◆ EXPERIMENTAL ATMOSPHERIC INTELLIGENCE v0.4

Predict the storm.
Protect the block.

A governed research environment built to evaluate storm prediction errors, identify dangerous local impacts, and test whether new variables improve decisions before the next event.

RESEARCH PRODUCT — NOT AN OFFICIAL EMERGENCY ADVISORY. The archive contains hindsight best-track observations, not advance forecasts. Follow NWS, NHC and local emergency management for current conditions.
HISTORICAL CYCLONES—1950–2025 Atlantic archive
SEASONS ANALYZED76Chronological replay
MAJOR HURRICANES—Observed peak intensity
VERIFIED POSEIDON WINS0Source recovery outstanding
01 / BEST-TRACK INTELLIGENCE

Historical storm explorer

Select any Atlantic tropical cyclone from 1950–2025. Map displays best-track observations.

Historical trackTrack endpoint
ATLANTIC / SCHEMATIC VIEWNOAA HURDAT2 • POST-EVENT BEST TRACK
Schematic lat/lon view; not an evacuation, maritime-navigation, or street-level flood map.
SELECTED HISTORICAL SYSTEM

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MAX WIND—kt
MIN PRESSURE—mb
U.S. LANDFALL ENTRIES—public-mirror matches
TRACK POINTS—sampled at 00/12 UTC
OBSERVED WIND HISTORY
This curve is observed history and cannot be scored as a forecast. Future Poseidon and NOAA forecast vintages will be captured separately.
02 / MODEL FAILURE INTELLIGENCE

What makes forecasts right—or wrong?

Compare documented inputs, expected failure modes, and the data needed for a genuine apples-to-apples experiment.

CANDIDATE FEATURES · NOT VALIDATED
Candidate variablePotential forecast valueFailure we would investigate
WEIGHTING RULE

Train a constrained, regularized mixture of available model predictions using past errors, lead time, geography and storm regime. Freeze weights before testing on later seasons.

ERROR ATTRIBUTION

Separate bad inputs, poor initialization, incorrect physics, track miss, intensity miss, drainage-model miss and missing local exposure.

ANTI-LEAKAGE CONTROL

Only use source runs completed before the decision deadline. Never fit to a storm's eventual damage, track or final intensity.

References: NOAA HAFS physics and coupling; NHC SHIPS/LGEM rapid-intensification research; NHC P-Surge. HAFS ↗ · P-Surge ↗ · Verification ↗

03 / SCIENTIFIC VALIDATION

Blind-year benchmark

Each historical prediction uses only earlier seasons; adaptive weights also use only previous errors.

WALK-FORWARD MEAN ABSOLUTE ERROR—Storms / season · lower is better
RMSE —
HOLDOUT YEARS 26
MODEL TYPE Climatology
Not a Poseidon-versus-NOAA accuracy claim. Evaluate source-vintage NHC and HAFS forecasts separately.
OBSERVED VS OUT-OF-SAMPLE PRIOR MODEL
ObservedBacktest
04 / ADVERSARIAL REPLAY

Break the forecast on purpose.

Replay a transparent persistence baseline with data corruption, lead-time and input perturbations.

EXPERIMENT · NOT POSEIDON CORE
RESEARCH DIAGNOSTIC

Awaiting replay

Input wind—
Actual future wind—
Error—

Perturbation is applied to a naive persisted wind estimate. This does not recreate an operational numerical forecast.

05 / MICRO-LOCAL EXPOSURE

One flooded street is still a disaster.

Coupling rainfall and coastal surge with drainage, road geometry, critical facilities and vulnerability is a separate high-resolution modeling problem.

ILLUSTRATIVE ONLY
SYNTHETIC TRIAGE INDEX
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Not a flood depth, probability, property-specific forecast or evacuation trigger. A real risk engine requires surveyed land elevation, drains, rainfall nowcasts, soils, river stages, tide gauges and buildings.

Official NHC surge guidance does not capture all rainfall-induced freshwater flooding; distinct physical inputs must be fused. Do not make location-specific safety decisions from this slider.