Abstract

Djiostrovah wind and its effect in the transfer of energy in the atmosphere arise Djiostrovah wind in the upper parts of the troposphere up to (3000 - 9000) m above sea level within the mid-latitudes from 30 to 60 in both hemispheres is determined by wind direction with the movement prevailing in Western of these offers. And speed over 20 knots and increasing speed to rise made ​​up swirling air large and because of the different speed of the speed of the wind down of which result in energy (momentum) to seep into the earth's surface and are affected by wind Djiostrovah strong deviation from the Earth's rotation around itself (power Creols) Vtnhrv wind Djiostrovah in offers a high pressure areas over the poles Allowatye where the reverse direction clockwise in the Northern Hemisphere with clockwise in the southern hemisphere, either in this world offers Vtnhrv about pressure areas over the Allowatye Madarien. Thus, they lead to bring Arctic air to bring the world and offers tropical air to the mid-latitudes and higher

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