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El Nino Events
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Paradoxically, while surface currents weaken, the Equatorial Undercurrent (EUC), a deep, subsurface flow of warm water, often exhibits a transient surge in speed during the mature phase of a strong El Niño. This is theorized to be due to the conservation of momentum across the basin as surface wind stress diminishes, forcing momentum transfer into the slower-moving depths [6].
| El Niño Strength Category | Niño 3.4 SST Anomaly Threshold ($\circ\text{C}$) | Primary Oceanic…