Solution:Geostrophic WindThe winds in the upper atmosphere, free from frictional effect of the surface and are controlled by the pressure gradient and the Coriolis force.
An air parcel initially at rest will move from high pressure to low pressure because of the Pressure Gradient Force (PGF).
However, as that air parcel begins to move, it is deflected by the Coriolis force to the right in the northern hemisphere (to the left in the southern hemisphere).
As the wind gains speed, the deflection increases until the Coriolis force equals the pressure gradient force (2-3 km above the ground, friction is low and winds travel at greater speeds).
At this point, the wind will be blowing parallel to the isobars (perpendicular to Pressure Gradient Force). When this happens, the wind is referred to as geostrophic wind.
Since these winds are geostrophic, i.e., they flow at great speeds due to low friction and are subjected to greater Coriolis force.
So they deflect greatly giving rise to three distinct cells called Hadley cell, Ferrel Cell and Polar cell.