The Chivela Pass is a narrow mountain pass in the Sierra Madre Mountains that funnels cooler, drier air from the North American continent, through southern Mexico, into the Pacific. These northeasterly winds, specifically the Tehuano wind, which periodically blows across the Isthmus of Tehuantepec in southern Mexico, and offshore over hundreds of miles of the Pacific Ocean, forcing the upwelling of colder subsurface waters. This strong upwelling brings nutrients from the subsurface layers of the ocean, thereby enhancing the fertility of the offshore waters. This results in strong plankton growth which in turn supports a more bountiful fishery in the region.
| Chivela Pass | |
|---|---|
 | |
| Elevation | 224 m (735 ft)[1] |
| Traversed by | Mexican Federal Highway 185 Tren Interoceánico |
| Location | Istmo de Tehuantepec, Asunción Ixtaltepec, Oaxaca, Mexico |
| Range | Sierra Madre de Oaxaca |
| Coordinates | 16°43′26″N 94°59′49″W / 16.724°N 94.997°W |
   | |
In extreme circumstances during the winter, truly cold, dense, air occasionally flows from the Bay of Campeche in the Gulf of Mexico through the Chivela Pass into the Gulf of Tehuantepec on the Pacific side. These winds can be strong enough to sandblast paint off ships in near-coastal waters.[2]
Notes edit
- ^ . Encyclopædia Britannica. Vol. 26 (11th ed.). 1911. p. 507.
- ^ "Moving Vectors for Gap Flow Through Mexico's Chivela Pass". Retrieved 2007-07-15.
External links edit
- The Gulf of Tehuantepec Hurricane Force Wind Event of 30-31 March 2003
- The Structure and Evolution of Gap Outflow over the Gulf of Tehuantepec, Mexico
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