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.
High pressure belts form as a result of air cooling and descending at specific latitudes in the Earth's atmosphere. As the air sinks, it becomes warmer and denser, creating an area of high pressure at the surface. These high pressure belts are typically found around 30 degrees north and south of the equator, known as the subtropical highs.
The Intertropical Coverance Zone. Or to abbreviate, ITCZ.
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
The convection cells radiate heat.
The convection cells radiate heat.
The convection cells radiate heat.
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.
High pressure belts form as a result of air cooling and descending at specific latitudes in the Earth's atmosphere. As the air sinks, it becomes warmer and denser, creating an area of high pressure at the surface. These high pressure belts are typically found around 30 degrees north and south of the equator, known as the subtropical highs.
Pressure belts form in the atmosphere due to differences in solar heating at different latitudes. Warm air rises at the equator, creating a low-pressure area, while cooler air sinks at the poles, creating high-pressure areas. This creates a system of alternating high and low pressure belts that help drive global wind patterns.
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.
Pressure belts are formed in the atmosphere due to the unequal heating of the Earth's surface. The sun's rays are more concentrated near the equator and spread out towards the poles, which creates temperature differences and leads to variations in air pressure. This results in the formation of different pressure belts like the equatorial low-pressure belt and the subtropical high-pressure belts.
The Intertropical Coverance Zone. Or to abbreviate, ITCZ.
A pressure belt refers to a region of high or low pressure that encircles the Earth, influencing weather patterns and wind circulation. The most well-known pressure belt is the Equatorial Low, associated with the Intertropical Convergence Zone where winds converge. Pressure belts play a crucial role in shaping global climate and weather systems.
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
The convection cells radiate heat.
Air is rising at low pressure belts. As air rises, it cools and forms clouds, leading to the possibility of precipitation. This rising motion at low pressure belts is associated with unsettled weather conditions.