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ℹ The Tehuantepecer is a regional gap wind that develops when a strong pressure gradient forms between cold, dense air over the Gulf of Mexico and lower pressure over the eastern tropical Pacific. The air is funnelled through the low-elevation Isthmus of Tehuantepec, where topographic channelling leads to a marked increase in wind speed. The flow is predominantly northerly to northeasterly, forming a narrow low-level jet over the Gulf of Tehuantepec. Downstream over the Pacific Ocean, the jet sp
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ℹ The Tehuantepecer is a regional gap wind that develops when a strong pressure gradient forms between cold, dense air over the Gulf of Mexico and lower pressure over the eastern tropical Pacific. The air is funnelled through the low-elevation Isthmus of Tehuantepec, where topographic channelling leads to a marked increase in wind speed. The flow is predominantly northerly to northeasterly, forming a narrow low-level jet over the Gulf of Tehuantepec. Downstream over the Pacific Ocean, the jet sp
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