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Atmospheric reentry refers to the return to an atmosphere previously left for space. Often the word "atmospheric" is dropped and the term reentry (or re-entry) is taken to mean atmospheric reentry in context.
Compared with landing on a planet without atmosphere, atmospheric entry has the advantage that no rocket is needed for deceleration. This gives a considerable reduction of the total delta-v needed for a spaceflight from the Earth, with return with soft landing, such as in the case of a manned spaceflight. Without this saving such a spaceflight would cost a delta-v of twice the 9.7 km/s for launch, is 19.4 km/s, which may even be impossible with current technology.
From a Low Earth Orbit a deorbit burn is needed, but this costs a delta-v of only ca. 80 m/s, depending on the altitude. From elsewhere a transfer orbit can be chosen that directly enters the atmosphere.
For a manned spacecraft and for objects of value the requirements are:
For expendable objects, preventing damage at the Earths surface is the objective, i.e. either burning up or evaporating in the atmosphere, or hitting deserted land or water. For example, even if the Hubble Space Telescope would no longer be needed, it would still be needed to carry out a mission to attach a de-orbit rocket, for either controlled reentry or moving it to a higher orbit.
Because a major difference between sub-orbital and orbital spaceflights is the greater speed of the latter, atmospheric reentry poses much more of a technical challenge with orbital flights than with suborbital flights. This article will focus on orbital reentry, though the same considerations apply with sub-orbital flights, only to a lesser extent. Also note that the below only really applies to flights where the vehicle needs to return to Earth intact. If the vehicle is, say, a satellite that is ultimately expendable, then there naturally is no need to worry about deceleration and non-destructive reentry.
The main challenge with reentry is deceleration from high orbital speeds. To avoid our orbital spacecraft performing a meteorA meteor is the visible path of a meteoroid that enters the Earth's (or another body's) atmosphere, commonly called a shooting star''. The visibility is due to the heat produced by the atmospheric entry. A very bright meteor, brighter than the apparent ma-style "landing", it has to slow down. An obvious way of slowing down is through atmospheric frictionIn physics, friction is the resistive force that occurs when two surfaces travel along each other when forced together. It causes physical deformation and heat buildup. The frictional force is a function of the force pressing the surfaces together and the and dragFor a solid object moving through a fluid, drag is the sum of all the aerodynamic or hydrodynamic forces in the direction of the external fluid flow. It therefore acts to oppose the motion of the object, and in a powered vehicle it is overcome by thrust. (ie. using wind resistance) . This is called aerobrakingAerobraking is a technique used by spacecraft in which it uses drag within a planetary atmosphere to reduce its velocity relative to the planet. Aerobraking has been used extensively over the decades by spacecraft orbiting Earth as a means to remove their. Atmospheric friction however can rapidly generate a destructive amount of heat. Many smaller meteoroids burn up through such friction and never reach the Earth's surface. So is there a better way?