directly by the sun.
The exosphere is the atmospheric level that is farthest from the lithosphere. It extends from the top of the thermosphere upwards and gradually transitions into outer space.
No, the thermosphere is actually heated by the sun's intense radiation. The air in the thermosphere is very sparse, so it can be heated to extremely high temperatures due to the absorption of solar energy.
Oxygen-20%Nitrogen-80%Helium-1%
The heterosphere is divided into several distinct regions based on the distribution of gases by molecular weight. These regions include the exosphere, thermosphere, and mesosphere. The exosphere is the outermost layer, containing mainly light gases like hydrogen and helium, while the thermosphere contains heavier gases like oxygen and nitrogen. The mesosphere sits below the thermosphere and holds various gases, with decreasing concentrations as altitude increases.
troposphere stratosphere mesosphere thermosphere
The uppermost atmospheric layer is the THERMOSPHERE. here temperature again increases with altitude because many of the gases are absorbing solar radiation.
The exosphere is the atmospheric level that is farthest from the lithosphere. It extends from the top of the thermosphere upwards and gradually transitions into outer space.
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No, the moon is not in the thermosphere. The moon is located in the vacuum of space, beyond Earth's atmosphere and atmospheric layers like the thermosphere.
thermosphere
No, the thermosphere is actually heated by the sun's intense radiation. The air in the thermosphere is very sparse, so it can be heated to extremely high temperatures due to the absorption of solar energy.
Oxygen-20%Nitrogen-80%Helium-1%
Thermosphere contain the same gases as troposphere but in very low concentrations: oxygen, nitrogen argon.
There are a few causes that lead to atmospheric air to be rapidly heated. Having a fire burning will lead to rapidly heated atmospheric air.
the thermosphere is the hottest all of the atmospheric layers.
In the thermosphere, ultraviolet (UV) and X-ray radiation from the Sun is absorbed by the sparse gases present, leading to the ionization of these gases. This absorption process significantly increases the temperature of the thermosphere, which can reach up to 2,500 °C (4,500 °F) or higher. The ionization also contributes to the formation of the ionosphere, which plays a crucial role in radio communication and atmospheric phenomena like the auroras. However, the density of the gases is so low that the heat is not felt as it would be at lower altitudes.
troposphere stratosphere mesosphere thermosphere