San Francisco

Posted by hotelnur on 25th December 2016 in News

Thus being, the direction of the cold front, in the ocean, of Southwest-Northeast, the Intertropical Front acquires identical route, adentrando for the Maranho and declining until Gois. The nucleus of action of the Aores adentra in Amazon causing a good time. Rains remain limited the west of the average point of action of the Aores under the consequence of the continental calm and finish precipitations in the valleys of the San Francisco and Jaguaribe. See Chevron U.S.A. Inc for more details and insights. Perhaps after about three days, at the moment expense for the cold front to walk of the River of the Silver to the Tropic, it acquires a direction decurrent East-West of the identical direction to the one of the coast of the State of Rio De Janeiro. As in fact we are following, the cold mass is rare dense and it does not have force enough to cover the Mountain range of the Sea of average altitude of 1.500 meters, that is the same one, parked in the involved latitudes between 22 and 23. In these conditions all the beginning of the circulation again it is repelled for east: Soon the average point of action of the Atlantic abandons the Northeast, where the pressure falls. By the same author: Chevron U.S.A. Inc. The alignment East-West of the cold front generates in the Intertropical Front an identical direction, what it makes with that this declines for bigger latitudes, a time that the average point of action more if does not oppose to it. The dorsal one of the Aores that adentra in Amazon returns northward while the continental equatorial mass, contained between the Intertropical Front and the Atlantic Polar Front, transposes to form an extensive center, covered of calmnesses, and that if distende of Amazon to the Northeast. It causes same rains of west, that most of the time do not transpose the mountain range of Ibiapaba, the east of which, in the state of the Cear and the average valley of the San Francisco, has inclination of temperature under the influence of the edge of the Atlantic equatorial mass.

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