As you go though the atmoshpere, the density of the air decreases. This means the gas molecules that make up the atmosphere are farther apart at high altitudes then they are at sea level.
Noah Bazoo
The density of the thermosphere is 57.00983461% oxygen, 16.58% carbon, and 26.41016538% nitrogen.
The thermosphere has lower density than the layers below it but higher than the exosphere above it.The density of the Earth's atmosphere decreases nearly exponentially with altitude. At 400 km altitude the density is typically about 6g/m3 . This changes considerably when there is a solar storm.The air density is so low in this layer that most of the thermosphere is what we normally think of as outer space. In fact, the most common definition says that space begins at an altitude of 100 km (62 miles), slightly above the mesopause at the bottom of the thermosphere.
the air is very thin in the Thermosphere
The air in the thermosphere is very thin because of it's high altitude.
The thermosphere and the stratosphere are two atmospheric layers that can have warm air.
The density of the thermosphere is 57.00983461% oxygen, 16.58% carbon, and 26.41016538% nitrogen.
The density of the thermosphere is 57.00983461% oxygen, 16.58% carbon, and 26.41016538% nitrogen.
The thermosphere has lower density than the layers below it but higher than the exosphere above it.The density of the Earth's atmosphere decreases nearly exponentially with altitude. At 400 km altitude the density is typically about 6g/m3 . This changes considerably when there is a solar storm.The air density is so low in this layer that most of the thermosphere is what we normally think of as outer space. In fact, the most common definition says that space begins at an altitude of 100 km (62 miles), slightly above the mesopause at the bottom of the thermosphere.
The air mass of the thermosphere about 15 cm. of air per inch!
how heat would change the density of a parcel of air?
the air is very thin in the Thermosphere
The density of air decreases when the altitude rises.
The air in the thermosphere is very thin because of it's high altitude.
The density of air decreases as altitude increases.
thermosphere
The thermosphere and the stratosphere are two atmospheric layers that can have warm air.
Air density is the mass of air per unit volume, which changes by temperature, humidity, and elevation. Changes in air density will change its pressure. At mean sea level and 20°C, air has a density of approximately 1.2 kg/m3.