The Coriolis effect explains this phenomenon clearly. Pressure belts and wind belts differ in patterns depending on certain atmospheric factors like temperature.
The bands of high pressure are called subtropical high-pressure belts, while the bands of low pressure are known as the intertropical convergence zone (ITCZ) or the equatorial low-pressure belt. These belts play a significant role in global atmospheric circulation.
High atmospheric pressure generally suppresses the development of rain clouds. The earth has belts of high pressure, usually between latitudes of 25 - 35 degrees north or south, where many of the earth's deserts are located.
Prevailing winds Easterlies
High pressure belts found at 30 degree latitudes are called subtropical high-pressure belts. These belts are generated by the sinking air from the Hadley Cell circulation at these latitudes, resulting in stable atmospheric conditions and clear skies. Subtropical high-pressure systems are associated with arid climates and are often responsible for the formation of deserts.
The convection cells radiate heat.
Locate the pressure belts on earth
It is the temperature which controls the pressure belts and ,therefore, as the sun moves from one tropic to another, the pressure belts also do the same.This phenomenon is called as shifting of pressure belts.
The pressure belts are located at different latitudes rather than longitudes. Some of the main pressure belts include the equatorial low-pressure belt near the equator, the subtropical high-pressure belts around 30 degrees north and south latitudes, and the subpolar low-pressure belts near the poles.
The seven pressure belts that impact global wind patterns are the Intertropical Convergence Zone (ITCZ), subtropical high-pressure belts (located at around 30 degrees N and S), subpolar low-pressure belts (located at around 60 degrees N and S), and the polar high-pressure belts (located at the poles). These pressure belts are key drivers of global atmospheric circulation and influence the direction and strength of winds around the world.
Its caused by the combination of pressure belts and the Coriolis effect.
An atmospheric belt refers to a region of consistent wind patterns and weather conditions near the Earth's surface, such as the Trade Winds. An atmospheric zone, on the other hand, refers to a broad area of the atmosphere with specific characteristics, such as the Troposphere or Stratosphere. Atmospheric belts are localized features within atmospheric zones.