Compare the density of gases in the thermosphere to the density at sea level.
The atmosphere is 10 times denser at sea level.
The atmosphere is 10 million times denser at sea level
.
The atmosphere is 1000 times denser at sea level.
The atmosphere is 100 times denser at sea level.
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We will examine how air temperature, number density, and pressure change in the vertical, i.e., as one moves up and down in Earth's atmosphere. The average vertical structure of temperature, density, and pressure in Earth's atmosphere described below is often called the "static structure" as it does not consider large scale movements of air like wind currents. It is like describing how the average properties of ocean water (e.g., water temperature and salinity) change in moving from the ocean bottom to the top of the water without considering ocean currents.
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