Explanation:

The general distribution of winds throughout the lower atmosphere is known as planetary winds. Confined within some latitudinal belts, these winds blow rather regularly throughout the year and are basically controlled by the latitudinal pressure belts. The main planetary winds are (i) the North-east and the South-east Trade winds (ii) the Temperate Westerlies and (iii) the Polar Easterlies, which blow from the polar high pressure area to the temperate low pre sure area.

Earth’s rotation and not its revolution is connected with planetary wind system. Earth’s rotation is responsible for generation of coriolis force, which impact the direction (and not speed) of planetary winds. This is the reason why we have south-west and north-east monsoon and not south and north monsoon.
Once air has been set in motion by the pressure gradient force, it undergoes an apparent deflection from its path, as seen by an observer on the earth. This apparent deflection is called the “Coriolis force” and is a result of the earth’s rotation.

As air moves from high to low pressure in the northern hemisphere, it is deflected to the right by the Coriolis force. In the southern hemisphere, air moving from high to low pressure is deflected to the left by the Coriolis force.