The north polar high-pressure belt typically experiences very little rainfall due to its stable atmospheric conditions. The high-pressure system suppresses cloud formation and precipitation, resulting in arid conditions. Any precipitation that does occur is usually in the form of light snow. Overall, this region is characterized by dry air and minimal moisture throughout the year.
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 permanent low-pressure belt in the sub-polar regions is mainly due to the convergence of cold polar air masses with warmer air masses from lower latitudes. This creates a region of instability, leading to rising air and the formation of cyclones. The Earth's rotation also influences the wind patterns and contributes to the development of the low-pressure system in these areas.
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 low pressure zone at the equator is called the Intertropical Convergence Zone (ITCZ). It is a belt of low pressure where the trade winds from the Northern and Southern Hemispheres converge, causing warm air to rise and creating a region of unsettled weather with heavy rainfall.
The only truly continuous pressure belt on Earth is the subtropical high-pressure belt, also known as the horse latitudes. This belt is situated around 30 degrees north and south of the equator and is characterized by descending air that leads to stable, dry conditions. It plays a crucial role in global wind patterns and the formation of deserts in these regions. This consistency in high pressure contrasts with other belts that can be more variable or seasonal.
equatorial low pressure belt sub tropical high pressure belt sub polar low pressure belt polar high pressure belt
convectional rainfall
clouds
The uneven heating of the earth produces pressure belts. these belts occur at about every 30 degrees latitude. The rotation of the Earth flings the bulk of the air creating an area of low pressure belt in this region.
temperate cyclones causes rainfall. westerlies are strong winds..............
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.
1.Thermal pressure belts Equatorial low pressure belt lies with 5 degrees of north and south of equator.(DOLDRUMS) b.Polar high pressure belt are formed around the north and south polar regions. 2.Other pressure belts a.Sub tropical high pressure belts are formed due to sinking of equatorial air that cools on 30 degrees near north and south. (HORSE LATITUDES) b.Sub-Polar temperate low pressure belts are formed near the arctic and antarctic circles. Here the cold winds meet the warm westerlies formed at 60 degrees.
The permanent low-pressure belt in the sub-polar regions is mainly due to the convergence of cold polar air masses with warmer air masses from lower latitudes. This creates a region of instability, leading to rising air and the formation of cyclones. The Earth's rotation also influences the wind patterns and contributes to the development of the low-pressure system in these areas.
The Subpolar Low-Pressure Belt lies along the polar jet stream. It is found between 50 and 70 degrees North latitude. It consists of the Aleutian and Icelandic lows.
polar front
High or low pressure lies along the subtropical jet stream, depending on the time of year. The pressure gradient follows the path of the jet stream.
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.