Tehuano gap wind event
As a strong arctic cold front moved southward across the Gulf of Mexico toward southern Mexico on 04-05 February 2026, the cold front fractured as it moved inland across Mexico’s Isthmus of Tehuantepec — the cold air was then channeled southward through Chivela Pass and emerged as a Tehuano (or “Tehuantepecer“) gap wind that eventually fanned outward across the Gulf of Tehuantepec and adjacent Pacific Ocean. 10-minute Full Disk scan GOES-19 (GOES-East) Near-Infrared images (above) showed the hazy plume of dust that was being transported offshore — along with a narrow arc cloud that marked the edges of this Tehuano flow.The pulse of Tehuano winds emerging southward across the Gulf of Tehuantepec and the Pacific Ocean was seen in ASCAT winds from Metop-B and Metop-C (below).

ASCAT winds from Metop-B and Metop-C
The highest Metop-B wind speed was 40 kts (below).

GOES-19 Near-Infrared image at 1550 UTC on 05 February, with a cursor sample of Metop-B wind speed at 1551 UTC [click to enlarge]

GOES-19 Near-Infrared image at 1800 UTC on 05 February, showing a ship report with NE winds gusting to 35 kts [click to enlarge]

10-minute True Color RGB images from GOES-18 (left) and GOES-19 (right) [click to play MP4 animation]
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Altimeter significant wave height values from SWOT at 2321 UTC on 05 February
