Low Earth orbit
A
low Earth orbit (LEO) is an
orbit around Earth between the atmosphere and the
Van Allen radiation belt. The boundaries are not firmly defined but are typically around
200 -
1200 km (124 - 726 miles) above the
Earth's surface. Above this are
intermediate circular orbit (ICO) and, far above,
geostationary orbit. Orbits lower than this are not stable and will decay rapidly because of atmospheric drag. Orbits higher than this are subject to early electronic failure because of intense radiation and charge accumulation. Orbits with a high inclination angle are usually called
polar orbits, the properties of this and the sun-synchronous orbit being more significant than their altitude.
Objects in low earth orbit encounter atmospheric gases in the
thermosphere (approximately 80-500 km up) or
exosphere (approximately 500 km and up), depending on orbit height.
Most
manned spaceflights have been in LEO, including all
Space Shuttle and various
space station missions; the only exceptions have been suborbital test flights such as the early
Project Mercury missions and the flights of the
X-15 rocket plane (which was not intended to reach LEO), and the
Project Apollo missions to the Moon (which went beyond LEO).
Most artificial
satellites are placed in LEO, where they travel at about 27,400 km/h (8 km/s), making one revolution in about 90 minutes. The primary exception are
communication satellites that require geostationary orbit. However, it requires less energy to place a satellite into a LEO and the satellite needs less powerful transmitters for data transfer, so LEO is still used for many communication applications. Because these orbits are not geostationary, a network of satellites is required to provide continuous coverage. Lower orbits also aid
remote sensing satellites because of the added detail that can be gained. Remote sensing satellites can also take advantage of sun synchronous LEO orbits at an altitude of about 800km and near polar inclination. ENVISAT is one example of an earth observation satellite that makes use of this special type of LEO.
The LEO environment is becoming congested, not least with
space debris. The
North American Aerospace Defense Command (NORAD), part of the
United States Strategic Command (formerly the
United States Space Command), tracks more than 8,000 objects larger than 10cm in LEO.
Although
gravity in LEO is not much less than on the surface of the Earth (it reduces 1% every 30 km), people and objects in orbit experience
weightlessness.
Atmospheric and gravity drag associated with launch typically add 1,500-2,000 m/s to the
delta-V required to reach normal LEO orbital velocity of 7,800 m/s.
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Atmospheric reentry*
Medium Earth Orbit (MEO or ICO)
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Geosynchronous Orbit (GEO)
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Geostationary Orbit (GSO)
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Geostationary Transfer Orbit (GTO)
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International Space Station*
Lunar Transfer Orbit (LTO)
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Moon*
Polar Orbit*
specific orbital energy examples*
Satellite phone*
Weather satellite