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Atmospheric drag provides a method of bleeding off energy from a spacecraft without using propulsion. Spacecraft thermal protection shields (TPS) insulate against resultant high stagnation point heating temperatures. Aeroassist maneuvers reduce spacecraft propellant requirements, launch weight and launch vehicle expense.


Aeroassist

Precise atmospheric density predictions are necessary for all of these techniques. Mathematical atmospheric models which produce these predictions are derived from observations of orbiting satellites. For example, Mars Global Surveyor (MGS) atmospheric reports were used for Mars Odyssey aerobraking.

Re-entry (Direct Entry) is the method employed by such missions as Apollo and the Space Shuttle to slow down and enter the atmosphere.

Aerobraking uses the atmosphere over long periods of time to slowly circularize elliptical orbits. Each revolution the spacecraft dips a little into the atmosphere until the final orbit is achieved. This process could take months.

Aerocapture very aggressively uses the atmosphere to slow spacecraft from interplanetary trajectories into a final orbit. Unlike aerobraking, penetration into the atmosphere is much deeper and lasts only minutes. If the flight path angle is too shallow, the spacecraft "bounces" off the atmosphere into space; if the flight path angle is too steep, the spacecraft will burn up. Despite its high propellant savings, aerocapture technology has not been demonstrated to date.

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