Into The Milfy-verse [v0.02] By Phase X Studios
The El Niño/Southern Oscillation (ENSO) resolves into a warm phase (El Niño), a cold phase (La Niña), and a neutral phase. During El Niño events (ENSO warm phase), tropospheric vertical shear is increased inhibiting tropical cyclone genesis and intensification, primarily by causing the 200 mb (12 km or 8 mi) westerly winds to be stronger (Gray 1984). La Niña events (ENSO cold phase) enhances activity. Recently, Tang and Neelin (2004) also identified that changes to the moist static stability can also contribute toward hurricane changes due to ENSO, with a drier, more stable environment present during El Niño events.
Into the Milfy-verse [v0.02] By Phase X Studios
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