Now the molecules of the heated air have room to move around more freely, and continue to do so as long as the heat gives them extra kinetic energy. The higher the hot air floats, the more room there is for its molecules to move about, and so it continually expands, its energy pushing it out and up. Here the air runs into a balancing problem due to the laws of thermodynamics. The energy from all of its molecules can be used to propel the molecules out at greater distances so it can expand more, or the energy can be used to keep the air hot, but it cannot do both at the same time.
Warm air rises at the equator and cold air sinks at the poles. Warm air expands and cool air contracts and compresses.
it gets warmer as it rises
yes the cool denser air sink while the warm less dense rises
Warm air rises because it is less dense than cold air. This creates air currents and convection that lead to the mixing of air masses in the atmosphere.
When warm air contacts cold air, the warm air typically rises above the cold air. This occurs because warm air is less dense than cold air. As the warm air rises, it can lead to the formation of clouds and precipitation, depending on the moisture content and other atmospheric conditions.
Warm air rises,and then sinks when the air is cold.
It's the other way round - when air becomes warm, it rises.
Warm air rises at the equator and cold air sinks at the poles. Warm air expands and cool air contracts and compresses.
it gets warmer as it rises
it gets warmer as it rises
it gets warmer as it rises
it gets warmer as it rises
Lol, no it doesn't, ..it gets colder as it rises.
Yes! Warm air is less dense, which is why warm air rises. Cold air is more dense so that's why it sinks.
yes the cool denser air sink while the warm less dense rises
Warm air rises because it is less dense than cold air. This creates air currents and convection that lead to the mixing of air masses in the atmosphere.
When warm air contacts cold air, the warm air typically rises above the cold air. This occurs because warm air is less dense than cold air. As the warm air rises, it can lead to the formation of clouds and precipitation, depending on the moisture content and other atmospheric conditions.