1. Large-scale circulation consisting of warm air that rises near the equator and moves poleward in the upper troposphere creating a low-pressure belt at the equator
2. As it rises to the top of the troposphere, the air cools to the same temperature as its surroundings and begins to flow toward the north and south poles
3. The cooled air descends gently again to reach the Earth's surface at around 30 degrees North and 30 degrees South, creating a zone of high subtropical atmospheric pressure
4. The air thus compressed and heated prevents the formation of clouds, resulting in clear skies, high temperature at the Earth's surface, permanent dry weather, and the formation of large tropical deserts
On the earth's surface, regular winds blow from the northeast in the northern hemisphere and from the southeast in the hemisphere between the Tropics and the equator, known as the trade winds
Cold air descending at the poles causes high pressure in the polar regions, leading to surface air migrating towards the mid-latitude low-pressure belts
Imaginaryforce, wind don't blow in a straight line due to the rotation of the Earth.
Jetstreams
High altitude winds connectingcells
Hot desert exist at the tropics because the dry air (cold/heavy) descends & absorbs all clouds. This air masses are part of the Hadley convection cell.
Arid climate can be found at the pôles because there is not much evaporation/moisture in air, it is cold.