in equitorial low pressure belt , low pressure is due to
1) intense heating
2) rate of rotation of earth is max. at equator . this results in max centrifugal force at equator which pushes the air away from the surface and causes low pressure condition.
Equatorial Low
The equatorial belt of low pressure and heavy rainfall is called the Intertropical Convergence Zone (ITCZ). This zone is characterized by the convergence of trade winds from both hemispheres, leading to upward motion, cloud formation, and precipitation.
The equator is an intensely heated throughout the year . Due to the intense heating the air in this region becomes warm and light and it rises above creating a partial vacuum .(As you know vacuum leads to decrease in air pressure) As a result a region of permanent low pressure is created called the equatorial low pressure belt.
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.
due to high temperature north west India becomes a seat of low pressure .this condition attracts the south east trade winds from southern hemisphere and while crossing the equator the winds change their direction to south west
clouds
Equatorial Low
convectional rainfall
The equatorial breeze is called the Trade Winds. These winds blow from the subtropical high pressure to the equatorial low pressure, creating a distinct pattern of air circulation near the equator.
equatorial low pressure belt sub tropical high pressure belt sub polar low pressure belt polar high pressure belt
Equatorial Low
The low pressure wind belt located in the equatorial regions is called the Intertropical Convergence Zone (ITCZ). This area is known for its rising warm, moist air that creates a belt of low pressure and convergence of trade winds.
The four major air pressure zones are the Polar High, Subtropical High, Equatorial Low, and Subpolar Low. These zones are characterized by their distinct atmospheric pressures and play a significant role in shaping global weather patterns.
The pressure zone associated with abundant precipitation and warm temperatures is the equatorial low-pressure zone, also known as the Intertropical Convergence Zone (ITCZ). This area experiences rising warm, moist air leading to frequent rainfall.
The equatorial belt of low pressure and heavy rainfall is called the Intertropical Convergence Zone (ITCZ). This zone is characterized by the convergence of trade winds from both hemispheres, leading to upward motion, cloud formation, and precipitation.
The equator is an intensely heated throughout the year . Due to the intense heating the air in this region becomes warm and light and it rises above creating a partial vacuum .(As you know vacuum leads to decrease in air pressure) As a result a region of permanent low pressure is created called the equatorial low pressure belt.
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.