Ngolfo de tehuantepec pdf files

Es una zona rica en petrleo y en recursos maderables. When the wind blows out of the north on the caribbean side of mexico, it picks up speed when it hits the gulf of tehuantepec and often reaches gale force. Universidad autonoma metropolitana iztapalap, 1998 ecosystem management 239 pages. Borrowed from spanish tehuantepec, from a nahuan language equivalent to classical nahuatl tecuantepec literally mountain of wild cats jaguars, ocelots, etc. Range extension of penaeus litopenaeus occidentalis. The gulf extends approximately 300 miles 500 km from puerto angel, in southern oaxaca state, southeastward to barra del suchiate.

Originalmente en zapoteco, existen versiones en castellano. Tehuantepecer definition of tehuantepecer by merriamwebster. Then it settles down for a few days before doing it all over again. Tehuantepecer definition is a violent north wind that brings an inflow of cold air to central america and especially to regions around the gulf of tehuantepec. Mexico, united mexican states, pacific, pacific ocean. Gulf of tehuantepec squeezing in a crossing between blows. Many but not all pacific hurricanes form in or near this body of water.

Nov 08, 2012 the tehuantepec blows and calms down in cycles that depend on the winds in the gulf of mexico. Tehuantepec article about tehuantepec by the free dictionary. Uss bangor pf16 was a united states navy tacomaclass frigate in commission from 1944 to 1946. Tehuantepecer, or tehuano wind, is a violent mountaingap wind traveling through chivela pass, most common between october and february, with a summer minimum in july. E il limite marino meridionale dellistmo di tehuantepec. The gulf extends approximately 300 miles 500 km from puerto angel, in southern oaxaca state, southeastward to barra del suchiate, in southeastern chiapas state, and. Temperature, felt temperature, atmospheric pressure, relative humidity, wind speed, wind gusts, isotherm, precipitation, cloud cover and heat index. It originates from eastern mexico and the bay of campeche as a postfrontal northerly wind, accelerated southward by cold air damming, which crosses the isthmus and blows through the gap between the mexican and guatemalan mountains.