Yes, air rises at the equator primarily due to its low density, which is a result of higher temperatures. The intense solar heating at the equator warms the air, causing it to expand and become less dense. This rising warm air creates lower pressure at the surface, leading to more air being drawn in from surrounding areas, contributing to the characteristic convection and the formation of tropical rainforests and weather patterns.
As you rise up through the layers of the atmosphere, both the density and pressure decrease. This is because there are fewer air molecules at higher altitudes, leading to lower density and pressure.
low pressure
yes
The reason the tropopause is lower above the poles than the equator is... The time it takes air to cool. The surface air-temperature at the equator is much higher than at the poles, meaning that the air rises further to reach the equilibrium required at the tropopause. Likewise, the air at the poles is cooler, and does not require as much room to rise.
It gets bigger because as it gets higher, the density of the atmosphere will rise when the density inside the balloon stays the same. Then because of pressure, it will get bigger and eventually pop.
As you rise up through the layers of the atmosphere, both the density and pressure decrease. This is because there are fewer air molecules at higher altitudes, leading to lower density and pressure.
low pressure
yes
Warm air rises because it is less dense than cold air, leading to lower pressure at the surface. This process is known as convection, where warm air expands and becomes buoyant, causing it to rise through the atmosphere.
The reason the tropopause is lower above the poles than the equator is... The time it takes air to cool. The surface air-temperature at the equator is much higher than at the poles, meaning that the air rises further to reach the equilibrium required at the tropopause. Likewise, the air at the poles is cooler, and does not require as much room to rise.
It gets bigger because as it gets higher, the density of the atmosphere will rise when the density inside the balloon stays the same. Then because of pressure, it will get bigger and eventually pop.
solar radiation throughout the year. As a result, air at the equator is heated, causing it to rise and creating low pressure. This warm air then moves towards the poles, where it cools, becomes denser, and sinks back towards the surface.
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.
When altitude rises, the air pressure and density both decrease. When temperature rises that means that more air is pushing down on it. So this means that the air pressure and density rise when temperature rises.
When altitude rises, the air pressure and density both decrease. When temperature rises that means that more air is pushing down on it. So this means that the air pressure and density rise when temperature rises.
Probably because it is warmer and hence lighter.
As you rise upwards in the atmosphere, air pressure decreases. This occurs because the density of air molecules diminishes with altitude, leading to fewer molecules exerting pressure. Consequently, higher elevations experience lower air pressure compared to sea level. This decrease in pressure can also affect breathing and the boiling point of liquids.