Tehuantepecer, or Tehuano wind, is a violent mountain-gap wind traveling through Chivela Pass, most common between October and February, with a summer maximum in July. It originates from eastern Mexico and the Bay of Campeche as a post-frontal northerly wind, accelerated southward by cold air damming, which crosses the isthmus and blows through the gap between the Mexican and Guatemalan mountains. The term dates back to at least 1929. This wind can reach gale, storm, and hurricane force. The leading edge of its outflow (or cold front) may form rope cloud over the Gulf of Tehuantepec. These winds can be observed on satellite pictures such as scatterometer wind measurements, they influence waves which then propagate as swell and sometimes observed 1,600 km (990 mi) away (such as in the Galapagos Islands). These strong winds bring cooler sub-surface waters to the surface of the tropical eastern Pacific ocean and may last from a few hours to 6 days.
The synoptic condition is associated with high-pressure system forming in Sierra Madre in the wake of an advancing cold front. Tehuantepecers primarily occur during the cold season months for the region in the wake of cold fronts, between October and February, with a summer maximum in July caused by the westward extension of the Azores-Bermuda high pressure system. Wind magnitude is greater during El Niño years than during La Niña years, due to the more frequent cold frontal incursions during El Niño winters. Tehuantepec winds reach 20 knots (37 km/h) to 40 knots (74 km/h), and on rare occasions 100 knots (190 km/h). The wind's direction is from the north to north-northeast. It leads to a localized acceleration of the trade winds in the region, and can enhance thunderstorm activity when it interacts with the Intertropical Convergence Zone. The effects can last from a few hours to six days.
As seen by weather satellite
Its leading edge shows up as a rope cloud within the visible and infrared channels of weather satellite images, and since it lies at the leading edge of a density (temperature and dew point) discontinuity, its leading edge by definition it is a cold front, though it has also been described as a squall line, with embedded rain squalls sometimes seen. Within polar orbiting imagery, a corridor of strong low-level winds show up this feature within scatterometer data retrievals, with its leading edge at the south to southwest edge of the wind surge.
Tehuantepecers can be felt up to 160 kilometres (99 mi) out to sea in the tropical eastern Pacific ocean. Sustained winds at sea have been recorded as high as 49.9 m/s (97.0 kn), with gusts as high as 60.2 m/s (117.0 kn), with a wind event in February 1974 which sandblasted the ship which took the observation. These winds cause waves which then propagate as swell and are sometimes observed 1,600 kilometres (990 mi) away (e.g., in Galapagos Islands). Its effects can appear similar to a tropical cyclone, though the sky is usually clear. The surface wind can also change local ocean currents during an event. These strong winds bring cooler sub-surface waters to the surface of the tropical eastern Pacific ocean, by as much as 14°F (9°C), and may last 4–7 days.
- Willis E. Hurd (May 1929). "Northers of the Gulf of Tehuantepec". Monthly Weather Review (American Meteorological Society) 57 (5): 192–194.
- Rosario Romero-Centeno, Jorge Zavala-Hidalgo, Artemio Gallegos, and James J. O'Brien (August 2003). "Isthmus of Tehuantepec wind climatology and ENSO signal". Journal Of Climate 16 (15): 2628–2639.
- American Meteorological Society (2012-01-26). "Tehuantepecer". Glossary of Meteorology. Retrieved 2013-05-16.
- Bob Fett (2002-12-09). "World Wind Regimes - Central America Gap Wind Tutorial". United States Naval Research Laboratory Monterey, Marine Meteorology Division. Retrieved 2013-05-16.
- Paul A. Arnerich. "Tehuantepecer Winds of the West Coast of Mexico". Mariners Weather Log (National Oceanic and Atmospheric Administration) 15 (2): 63–67.
- David M. Schultz, W. Edward Bracken, Lance F. Bosart, Gregory J. Hakim, Mary A. Bedrick, Michael J. Dickinson, and Kevin R. Tyle (January 1997). "The 1993 Superstorm Cold Surge: Frontal Structure, Gap Flow, and Tropical Impact". Monthly Weather Review 125: 6–7. doi:10.1175/1520-0493%281997%29125<0005%3ATSCSFS>2.0.CO%3B2.
- Willis E. Hurd (November 1939). "Tehuantepecer of November 24, 1939". Monthly Weather Review (American Meteorological Society) 67 (11): 432.
- Steenburgh, W. J., D. M. Schultz, B. A. Colle, 1998: The Structure and Evolution of Gap Outflow over the Gulf of Tehuantepec, Mexico. Monthly Weather Review: Vol. 126, pp. 2673–2691
- Bourassa MA, Zamudio L, O'Brien JJ, Noninertial flow in NSCAT observations of Tehuantepec winds, JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS 104 (C5): 11311-11319 MAY 15 1999
- Chelton DB, Freilich MH, Esbensen SK, Satellite observations of the wind jets off the Pacific coast of Central America. Part I: Case studies and statistical characteristics, MONTHLY WEATHER REVIEW 128 (7): 1993-2018 Part 1 JUL 2000