0
directly by the sun.
Wiki User
∙ 13y ago
Add your answer:
Earn +20 pts
Which atmospheric level is farthest from the lithosphere?
The thermosphere is.
What is the thermosphere composed of?
The Thermosphere contains the ionsphere and exosphere with nitrogen and other gases
What are the atmospheric layers?
From on top of us: Troposphere, Stratosphere, Mesosphere, Thermosphere, Exosphere.
Where is the atmospheric pressure the greatest?
Near the earth's surface.
What are the gases found in the thermosphere?
Oxygen-20%Nitrogen-80%Helium-1%
Which atmospheric level is farthest from the lithosphere?
The thermosphere is.
The Uppermost atmospheric layer?
The uppermost atmospheric layer is the THERMOSPHERE. here temperature again increases with altitude because many of the gases are absorbing solar radiation.
What is the atmospheric pressure in the thermosphere?
90
Two atmospheric layers that contain air as warm as 25c?
The thermosphere and the stratosphere are two atmospheric layers that can have warm air.
Which atmospheric level is farhtest from the lithosphere?
thermosphere
What are the gases in thermosphere?
Thermosphere contain the same gases as troposphere but in very low concentrations: oxygen, nitrogen argon.
What is the thermosphere composed of?
The Thermosphere contains the ionsphere and exosphere with nitrogen and other gases
Which Layer Contains All Atmospheric Storms?
The Thermosphere is the layer that contains all of the Atmospheric storms
What increases the temperature in the atmosphere?
the thermosphere is the hottest all of the atmospheric layers.
What are the atmospheric names?
the exosphere, the thermosphere, the troposphre, the mesosphere, the ionisphere and the stratosphere.
Causes atmospheric air to be rapidly heated?
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.
Does the thermosphere only contain a tiny fraction of the atmosphere's mass?
Yes the thermosphere only contains a tiny fraction of atmospheric mass.
