The density of the atmosphere is proportional to the heat it's containing; so, it's density 100km over the tropics isn't quite the same as it's density 100km over the poles. However, over the course of a year, depending on your location, the atmosphere will receive more direct sunlight and heat up, causing it's density to fall, then cool off, causing it's density to increase.
In other words:-Atmospheric drag is reduced as altitude and
temperature increase.
Because the density of the air is reduced at higher altitude and
temperature.
Hope my explanation will help you.
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