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Hot evening atmosphere will persist – Noticieros Televisa

During the early hours of Wednesday, minimum temperatures of – 5 to 0 degrees Celsius are expected in mountainous areas of Chihuahua and Durango, as well as from 0 to 5 degrees Celsius in high places of Baja California, State of Mexico, Hidalgo, Puebla, Sonora and Tlaxcala, in addition to conditions parto frost in Chihuahua, Durango, State of Mexico, Hidalgo and Puebla.

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And anticyclonic system in the middle levels of the atmosphere will keep hot evening atmosphere to very hot in most of the Mexican Republic, with maximum temperatures of 40 to 45 degrees in Campeche, Chiapas, Coahuila, Guerrero, southern Jalisco, Michoacán, Morelos, Nuevo León, Oaxaca, San Luis Potosí, Tabasco, Tamaulipas, Veracruz and Yucatan; 35 to 40 degrees in Baja California, Chihuahua, Colima, Durango, southwest of the State of Mexico, Guanajuato, north of Hidalgo, Nayarit, north and southwest of Puebla, north of Querétaro, Quintana Roo, Sinaloa, Sonora, north and south of Zacatecas, as well as 30 to 35 degrees Celsius in AguAscalientes, Baja California Sur, Mexico City and Tlaxcala.

is forecast gusty wind from 60 to 70 km/h and dust storms in Chihuahua, Coahuila, Nuevo León and Tamaulipas, and from 50 to 60 km/h in Aguascalientes, Baja California, Durango, Jalisco, San Luis Potosí and Zacatecas.

Also, strong punctual rains are expected in areas of Chiapas and Nuevo León; intervals of showers in localities of Coahuila, Guanajuato, Oaxaca, San Luis Potosí, Tamaulipas and Zacatecas and isolated rains in regions of Aguascalientes, Durango, Jalisco, Michoacán, Puebla and Quintana Roo. The forecast rains may be accompanied by electrical discharges and conditions for the fall of hail of different sizes.

The meteorological conditions described above will be caused by a dry line over the north of the Mexican territory that will continue in interaction with a low pressure channel over the interior of the Mexican Republic; the current of maximum winds, instability at high levels of the atmosphere, in addition to a second low pressure channel extended in the southeast of the Mexican territory, in combination with the entry of moisture from the Pacific Ocean and the Caribbean Sea.

With information from Conagua

KAH

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