Download Trade Wind Directions PNG. Intense solar heat in the doldrums warms and moistens the trade winds, thrusting air upwards into the atmosphere. These winds are mainly caused due to the coriolis effect and ferrel's law.

Prevailing Winds of South America - Earth Science from mrjacobsearthscience.weebly.com

The trade winds are the prevailing pattern of surface winds from the east toward the west (easterly) found in the tropics, within the lower portion of the earth's atmosphere, in the lower section of the. A wind blowing obliquely towards the equator either from the northeast in the c17: C)they possess constancy of direction & speed(about 7m/sec.

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(4) there, it changes direction and flows back towards the equator, to restart the. (4) there, it changes direction and flows back towards the equator, to restart the. When air moves, the coriolis force deflects air either to the right of air motion in the northern hemisphere and to the left of air motion in the southern. Any of the nearly constant easterly winds that dominate most of the tropics and any wind that blows in one regular course, or continually in the same direction.