Tropical Warm Pool Antarctic Teleconnection Simulator

Modeling Indo-Pacific Warm Pool (IPWP) convective forcing, Rossby wave trains, Amundsen Sea Low depth, and sub-ice Circumpolar Deep Water (CDW) basal melt slowdown.

Equatorial Forcing Controls

Warm Pool SST Anomaly (ΔSST) +0.85 °C

Convection Amplification 1.25 ×

Multiyear Event Duration 6 Years

Deterministic Teleconnection Proof

Amundsen Sea Low Anomaly: -4.2 hPa

Shelf Meridional Wind Anom: -1.8 m/s

CDW Shelf Intrusion Reduction: 22.4%

Basal Melt Slowdown Rate: +38.6 Gt/yr

Net Ice Mass Loss Rate: -126.4 Gt/yr

5-Year Cumulative Saved Ice: 193 Gt

Workflow Actions

Planetary 200 hPa Pacific-South American (PSA) Teleconnection & Rossby Wave Rays

IPWP Divergence Stationary Rossby Rays Deepened ASL Center

Amundsen Sea Continental Shelf CDW Intrusion

CDW Thermocline Layer

West Antarctic Mass Loss Trajectory (Gt)

Baseline Teleconnection

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