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Atmospheric drag is proportional to density. How does the magnitude of atmospheric drag change over a solar cycle at 100 km altitude? 1.

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Answer #1

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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