Geostationary orbit GudangMovies21 Rebahinxxi LK21
A geostationary orbit, also referred to as a geosynchronous equatorial orbit (GEO), is a circular geosynchronous orbit 35,786 km (22,236 mi) in altitude above Earth's equator, 42,164 km (26,199 mi) in radius from Earth's center, and following the direction of Earth's rotation.
An object in such an orbit has an orbital period equal to Earth's rotational period, one sidereal day, and so to ground observers it appears motionless, in a fixed position in the sky. The concept of a geostationary orbit was popularised by the science fiction writer Arthur C. Clarke in the 1940s as a way to revolutionise telecommunications, and the first satellite to be placed in this kind of orbit was launched in 1963.
Communications satellites are often placed in a geostationary orbit so that Earth-based satellite antennas do not have to rotate to track them but can be pointed permanently at the position in the sky where the satellites are located. Weather satellites are also placed in this orbit for real-time monitoring and data collection, and navigation satellites to provide a known calibration point and enhance GPS accuracy.
Geostationary satellites are launched via a temporary orbit, and then placed in a "slot" above a particular point on the Earth's surface. The satellite requires periodic station-keeping to maintain its position. Modern retired geostationary satellites are placed in a higher graveyard orbit to avoid collisions.
History
In 1929, Herman Potočnik described both geosynchronous orbits in general and the special case of the geostationary Earth orbit in particular as useful orbits for space stations. The first appearance of a geostationary orbit in popular literature was in October 1942, in the first Venus Equilateral story by George O. Smith, but Smith did not go into details. British science fiction author Arthur C. Clarke popularised and expanded the concept in a 1945 paper entitled Extra-Terrestrial Relays – Can Rocket Stations Give Worldwide Radio Coverage?, published in Wireless World magazine. Clarke acknowledged the connection in his introduction to The Complete Venus Equilateral. The orbit, which Clarke first described as useful for broadcast and relay communications satellites, is sometimes called the Clarke orbit. Similarly, the collection of artificial satellites in this orbit is known as the Clarke Belt.
In technical terminology the orbit is referred to as either a geostationary or geosynchronous equatorial orbit, with the terms used somewhat interchangeably.
The first geostationary satellite was designed by Harold Rosen while he was working at Hughes Aircraft in 1959. Inspired by Sputnik 1, he wanted to use a geostationary satellite to globalise communications. Telecommunications between the US and Europe was then possible between just 136 people at a time, and reliant on high frequency radios and an undersea cable.
Conventional wisdom at the time was that it would require too much rocket power to place a satellite in a geostationary orbit and it would not survive long enough to justify the expense, so early efforts were put towards constellations of satellites in low or medium Earth orbit. The first of these were the passive Echo balloon satellites in 1960, followed by Telstar 1 in 1962. Although these projects had difficulties with signal strength and tracking, issues that could be solved using geostationary orbits, the concept was seen as impractical, so Hughes often withheld funds and support.
By 1961, Rosen and his team had produced a cylindrical prototype with a diameter of 76 centimetres (30 in), height of 38 centimetres (15 in), weighing 11.3 kilograms (25 lb), light and small enough to be placed into orbit. It was spin stabilised with a dipole antenna producing a pancake shaped beam. In August 1961, they were contracted to begin building the real satellite. They lost Syncom 1 to electronics failure, but Syncom 2 was successfully placed into a geosynchronous orbit in 1963. Although its inclined orbit still required moving antennas, it was able to relay TV transmissions, and allowed for US President John F. Kennedy in Washington D.C., to phone Nigerian prime minister Abubakar Tafawa Balewa aboard the USNS Kingsport docked in Lagos on August 23, 1963.
The first satellite placed in a geostationary orbit was Syncom 3, which was launched by a Delta D rocket in 1964. With its increased bandwidth, this satellite was able to transmit live coverage of the Summer Olympics from Japan to America. Geostationary orbits have been in common use ever since, in particular for satellite television.
Today there are hundreds of geostationary satellites providing remote sensing and communications.
Although most populated land locations on the planet now have terrestrial communications facilities (microwave, fiber-optic), with telephone access covering 96% of the population and internet access 90%, some rural and remote areas in developed countries are still reliant on satellite communications.
Uses
Most commercial communications satellites, broadcast satellites and SBAS satellites operate in geostationary orbits.
= Communications
=
Geostationary communication satellites are useful because they are visible from a large area of the earth's surface, extending 81° away in latitude and 77° in longitude. They appear stationary in the sky, which eliminates the need for ground stations to have movable antennas. This means that Earth-based observers can erect small, cheap and stationary antennas that are always directed at the desired satellite.: 537 However, latency becomes significant as it takes about 240 ms for a signal to pass from a ground based transmitter on the equator to the satellite and back again.: 538 This delay presents problems for latency-sensitive applications such as voice communication, so geostationary communication satellites are primarily used for unidirectional entertainment and applications where low latency alternatives are not available.
Geostationary satellites are directly overhead at the equator and appear lower in the sky to an observer nearer the poles. As the observer's latitude increases, communication becomes more difficult due to factors such as atmospheric refraction, Earth's thermal emission, line-of-sight obstructions, and signal reflections from the ground or nearby structures. At latitudes above about 81°, geostationary satellites are below the horizon and cannot be seen at all. Because of this, some Russian communication satellites have used elliptical Molniya and Tundra orbits, which have excellent visibility at high latitudes.
= Meteorology
=
A worldwide network of operational geostationary meteorological satellites is used to provide visible and infrared images of Earth's surface and atmosphere for weather observation, oceanography, and atmospheric tracking. As of 2019 there are 19 satellites in either operation or stand-by. These satellite systems include:
the United States' GOES series, operated by NOAA
the Meteosat series, launched by the European Space Agency and operated by the European Weather Satellite Organization, EUMETSAT
the Republic of Korea COMS-1 and GK-2A multi mission satellites.
the Russian Elektro-L satellites
the Japanese Himawari series
Chinese Fengyun series
India's INSAT series
These satellites typically capture images in the visual and infrared spectrum with a spatial resolution between 0.5 and 4 square kilometres. The coverage is typically 70°, and in some cases less.
Geostationary satellite imagery has been used for tracking volcanic ash, measuring cloud top temperatures and water vapour, oceanography, measuring land temperature and vegetation coverage, facilitating cyclone path prediction, and providing real time cloud coverage and other tracking data. Some information has been incorporated into meteorological prediction models, but due to their wide field of view, full-time monitoring and lower resolution, geostationary weather satellite images are primarily used for short-term and real-time forecasting.
= Navigation
=
Geostationary satellites can be used to augment GNSS systems by relaying clock, ephemeris and ionospheric error corrections (calculated from ground stations of a known position) and providing an additional reference signal. This improves position accuracy from approximately 5m to 1m or less.
Past and current navigation systems that use geostationary satellites include:
The Wide Area Augmentation System (WAAS), operated by the United States Federal Aviation Administration (FAA);
The European Geostationary Navigation Overlay Service (EGNOS), operated by the ESSP (on behalf of EU's GSA);
The Multi-functional Satellite Augmentation System (MSAS), operated by Japan's Ministry of Land, Infrastructure and Transport Japan Civil Aviation Bureau (JCAB);
The GPS Aided Geo Augmented Navigation (GAGAN) system being operated by India.
The commercial StarFire navigation system, operated by John Deere and C-Nav Positioning Solutions (Oceaneering);
The commercial Starfix DGPS System and OmniSTAR system, operated by Fugro.
Implementation
= Launch
=
Geostationary satellites are launched to the east into a prograde orbit that matches the rotation rate of the equator. The smallest inclination that a satellite can be launched into is that of the launch site's latitude, so launching the satellite from close to the equator limits the amount of inclination change needed later. Additionally, launching from close to the equator allows the speed of the Earth's rotation to give the satellite a boost. A launch site should have water or deserts to the east, so any failed rockets do not fall on a populated area.
Most launch vehicles place geostationary satellites directly into a geostationary transfer orbit (GTO), an elliptical orbit with an apogee at GEO height and a low perigee. On-board satellite propulsion is then used to raise the perigee, circularise and reach GEO.
= Orbit allocation
=
Satellites in geostationary orbit must all occupy a single ring above the equator. The requirement to space these satellites apart, to avoid harmful radio-frequency interference during operations, means that there are a limited number of orbital slots available, and thus only a limited number of satellites can be operated in geostationary orbit. This has led to conflict between different countries wishing access to the same orbital slots (countries near the same longitude but differing latitudes) and radio frequencies. These disputes are addressed through the International Telecommunication Union's allocation mechanism under the Radio Regulations. In the 1976 Bogota Declaration, eight countries located on the Earth's equator claimed sovereignty over the geostationary orbits above their territory, but the claims gained no international recognition.
= Statite proposal
=
A statite is a hypothetical satellite that uses radiation pressure from the sun against a solar sail to modify its orbit.
It would hold its location over the dark side of the Earth at a latitude of approximately 30 degrees. A statite is stationary relative to the Earth and Sun system rather than compared to surface of the Earth, and could ease congestion in the geostationary ring.
Retired satellites
Geostationary satellites require some station keeping to keep their position, and once they run out of thruster fuel they are generally retired. The transponders and other onboard systems often outlive the thruster fuel and by allowing the satellite to move naturally into an inclined geosynchronous orbit some satellites can remain in use, or else be elevated to a graveyard orbit. This process is becoming increasingly regulated and satellites must have a 90% chance of moving over 200 km above the geostationary belt at end of life.
= Space debris
=
Space debris at geostationary orbits typically has a lower collision speed than at low Earth orbit (LEO) since all GEO satellites orbit in the same plane, altitude and speed; however, the presence of satellites in eccentric orbits allows for collisions at up to 4 km/s (14,400 km/h; 8,900 mph). Although a collision is comparatively unlikely, GEO satellites have a limited ability to avoid any debris.
At geosynchronous altitude, objects less than 10 cm in diameter cannot be seen from the Earth, making it difficult to assess their prevalence.
Despite efforts to reduce risk, spacecraft collisions have occurred. The European Space Agency telecom satellite Olympus-1 was struck by a meteoroid on August 11, 1993, and eventually moved to a graveyard orbit, and in 2006 the Russian Express-AM11 communications satellite was struck by an unknown object and rendered inoperable, although its engineers had enough contact time with the satellite to send it into a graveyard orbit. In 2017, both AMC-9 and Telkom-1 broke apart from an unknown cause.
Properties
A typical geostationary orbit has the following properties:
Inclination: 0°
Period: 1436 minutes (one sidereal day): 121
Eccentricity: 0
Argument of perigee: undefined
Semi-major axis: 42,164 km
= Inclination
=
An inclination of zero ensures that the orbit remains over the equator at all times, making it stationary with respect to latitude from the point of view of a ground observer (and in the Earth-centered Earth-fixed reference frame).: 122
= Period
=
The orbital period is equal to exactly one sidereal day. This means that the satellite will return to the same point above the Earth's surface every (sidereal) day, regardless of other orbital properties. For a geostationary orbit in particular, it ensures that it holds the same longitude over time.: 121 This orbital period, T, is directly related to the semi-major axis of the orbit through the formula:
T
=
2
π
a
3
μ
{\displaystyle T=2\pi {\sqrt {a^{3} \over \mu }}}
where:
a is the length of the orbit's semi-major axis
μ is the standard gravitational parameter of the central body: 137
= Eccentricity
=
The eccentricity is zero, which produces a circular orbit. This ensures that the satellite does not move closer or further away from the Earth, which would cause it to track backwards and forwards across the sky.: 122
Stability
A geostationary orbit can be achieved only at an altitude very close to 35,786 kilometres (22,236 miles) and directly above the equator. This equates to an orbital speed of 3.07 kilometres per second (1.91 miles per second) and an orbital period of 1,436 minutes, one sidereal day. This ensures that the satellite will match the Earth's rotational period and has a stationary footprint on the ground. All geostationary satellites have to be located on this ring.
A combination of lunar gravity, solar gravity, and the flattening of the Earth at its poles causes a precession motion of the orbital plane of any geostationary object, with an orbital period of about 53 years and an initial inclination gradient of about 0.85° per year, achieving a maximal inclination of 15° after 26.5 years.: 156 To correct for this perturbation, regular orbital stationkeeping maneuvers are necessary, amounting to a delta-v of approximately 50 m/s per year.
A second effect to be taken into account is the longitudinal drift, caused by the asymmetry of the Earth – the equator is slightly elliptical (equatorial eccentricity).: 156 There are two stable equilibrium points sometimes called "gravitational wells" (at 75.3°E and 108°W) and two corresponding unstable points (at 165.3°E and 14.7°W). Any geostationary object placed between the equilibrium points would (without any action) be slowly accelerated towards the stable equilibrium position, causing a periodic longitude variation. The correction of this effect requires station-keeping maneuvers with a maximal delta-v of about 2 m/s per year, depending on the desired longitude.
Solar wind and radiation pressure also exert small forces on satellites: over time, these cause them to slowly drift away from their prescribed orbits.
In the absence of servicing missions from the Earth or a renewable propulsion method, the consumption of thruster propellant for station-keeping places a limitation on the lifetime of the satellite. Hall-effect thrusters, which are currently in use, have the potential to prolong the service life of a satellite by providing high-efficiency electric propulsion.
Derivation
For circular orbits around a body, the centripetal force required to maintain the orbit (Fc) is equal to the gravitational force acting on the satellite (Fg):
F
c
=
F
g
{\displaystyle F_{\text{c}}=F_{\text{g}}}
From Isaac Newton's universal law of gravitation,
F
g
=
G
M
E
m
s
r
2
{\displaystyle F_{\text{g}}=G{\frac {M_{\text{E}}m_{\text{s}}}{r^{2}}}}
,
where Fg is the gravitational force acting between two objects, ME is the mass of the Earth, 5.9736×1024 kg, ms is the mass of the satellite, r is the distance between the centers of their masses, and G is the gravitational constant, (6.67428±0.00067)×10−11 m3 kg−1 s−2.
The magnitude of the acceleration, a, of a body moving in a circle is given by:
a
=
v
2
r
{\displaystyle a={\frac {v^{2}}{r}}}
where v is the magnitude of the velocity (i.e. the speed) of the satellite. From Newton's second law of motion, the centripetal force Fc is given by:
F
c
=
m
s
v
2
r
{\displaystyle F_{\text{c}}=m_{\text{s}}{\frac {v^{2}}{r}}}
.
As Fc = Fg,
m
s
v
2
r
=
G
M
E
m
s
r
2
{\displaystyle m_{\text{s}}{\frac {v^{2}}{r}}=G{\frac {M_{\text{E}}m_{\text{s}}}{r^{2}}}}
,
so that
v
2
=
G
M
E
r
{\displaystyle v^{2}=G{\frac {M_{\text{E}}}{r}}}
Replacing v with the equation for the speed of an object moving around a circle produces:
(
2
π
r
T
)
2
=
G
M
E
r
{\displaystyle \left({\frac {2\pi r}{T}}\right)^{2}=G{\frac {M_{\text{E}}}{r}}}
where T is the orbital period (i.e. one sidereal day), and is equal to 86164.09054 s. This gives an equation for r:
r
=
G
M
E
T
2
4
π
2
3
{\displaystyle r={\sqrt[{3}]{\frac {GM_{\text{E}}T^{2}}{4\pi ^{2}}}}}
The product GME is known with much greater precision than either factor alone; it is known as the geocentric gravitational constant μ = 398600.4418±0.0008 km3 s−2. Hence
r
=
μ
T
2
4
π
2
3
{\displaystyle r={\sqrt[{3}]{\frac {\mu T^{2}}{4\pi ^{2}}}}}
The resulting orbital radius is 42,164 kilometres (26,199 miles). Subtracting the Earth's equatorial radius, 6,378 kilometres (3,963 miles), gives the altitude of 35,786 kilometres (22,236 miles).
The orbital speed is calculated by multiplying the angular speed by the orbital radius:
v
=
ω
r
≈
3074.6
m/s
{\displaystyle v=\omega r\quad \approx 3074.6~{\text{m/s}}}
In other planets
By the same method, we can determine the orbital altitude for any similar pair of bodies, including the areostationary orbit of an object in relation to Mars, if it is assumed that it is spherical (which it is not entirely). The gravitational constant GM (μ) for Mars has the value of 42830 km3 s−2, its equatorial radius is 3389.50 km and the known rotational period (T) of the planet is 1.02595676 Earth days (88642.66 s). Using these values, Mars' orbital altitude is equal to 17039 km.
See also
List of orbits
List of satellites in geosynchronous orbit
Orbital station-keeping
Space elevator, which ultimately reaches to and beyond a geostationary orbit
Explanatory notes
References
This article incorporates public domain material from Federal Standard 1037C. General Services Administration. Archived from the original on January 22, 2022. (in support of MIL-STD-188).
External links
How to get a satellite to geostationary orbit
Orbital Mechanics (Rocket and Space Technology)
List of satellites in geostationary orbit
Clarke Belt Snapshot Calculator
3D Real Time Satellite Tracking
Geostationary satellite orbit overview
Daily animation of the Earth, made by geostationary satellite 'Electro L' photos Satellite shoots 48 images of the planet every day.
Orbital Mechanics for Engineering Students
Kata Kunci Pencarian:
geostationary orbitgeostationary orbit (geo)geostationary orbit picturesgeostationary orbit imagegeostationary orbit is at a height ofgeostationary orbit distancegeostationary orbit slotsgeostationary orbit altitudegeostationary orbit definitiongeostationary orbit radius
Geostationary Orbit - Assignment Point
Geostationary Orbit - Assignment Point
Geostationary Earth Orbit
Geostationary orbit - Simple English Wikipedia, the free encyclopedia
Saving geostationary orbit - ROOM Space Journal
Geostationary orbit | Wikiwand | Geostationary orbit, Earth orbit, Orbit
Geostationary Orbit Polar Orbit
Geostationary orbit | The Planetary Society
Geostationary orbit | The Planetary Society
Geostationary Orbit – Geospatial Education Platform
ESA - Geostationary orbit
Geostationary Orbit Diagram Photograph by Science Photo Library - Pixels
Search Resultsgeostationary orbit
Daftar Isi
Dec 11, 2015 · 1 siderial day = 21,549.425 s (this is the period for geosync orbit, I don't think KSP worried about orbital precession) Using Keplers 3rd law, equitorial geostationary orbit r = 3,463,334 m or an altitude of 2,863.334 km circular with an orbital velocity of 1,009.81 m/s I'm confused how the Third Law was applied. Explain/elaborate/correct:
Feb 19, 2016 · A geostationary orbit, geostationary Earth orbit or geosynchronous equatorial orbit (GEO) is a circular orbit 35,786 kilometres (22,236 mi) above the Earth's equator and following the direction of the Earth's rotation.
Geostationary Orbit question :: Kerbal Space Program General …
Apr 9, 2013 · Geosynchronous orbit of Eve is at an altitude of 10,373.195 km above Eve. Geosynchronousorbit of Duna is at an altitude of 2,862.702 km above Duna. Geosynchronous orbit of Kerbal is at an altitude of 2,868.4 km above Kerbin. Geosynchronous orbit of Jool is at an altitude of about 7,000? km above Jool.
Geostationary orbits :: Juno: New Origins General Discussions
May 3, 2023 · On the one hand. On the other: Just sit down where you are since you are already in a geostationary orbit around the moon. After replying to this post I actually took the time to look up whether a geostationary orbit was possible around our actual moon. From what I read my initial feeling was correct.
Help with geostationary orbit :: Kerbal Space Program General …
Apr 29, 2018 · Since you're at Kerbin, you can target the Mun for the perfect equitorial orbit. Just doing the math, you would need a period of 5 hours, 59 minutes, 9.4 seconds or 21549.4 seconds. The standard gravitational parameter of Kerbin is 3.5316*10^12
i need exact "set orbit" values for geostationary orbit over ksc
Oct 30, 2017 · You would need to get your ship into a circular 2863333.5 meter orbit for it to be geostationary. For getting it exactly over KSC, you're going to have to either play with the orbit setter a bit or phase shift it manually.
Sep 24, 2016 · The Incline or Angle of your Orbit relative to a Default Equatorial Orbit. Inclination is measured in 180 Degrees. Positive Values for the Northern Hemisphere: (1 to 180) Negative Values for the Southern Hemisphere: (-1 to -180) Direction of Orbit is Relative to the selected Inclination Value used, as shown in picture.
Laythe Geostationary Orbit :: Kerbal Space Program General …
Jun 23, 2017 · Seriously now, you can find any planet's geostationary orbit height from the centre of the body with the formula ∛(GM/w²) where: - G is the gravitational constant of (6.67428 ± 0.00067)×10−¹¹ m³⋅kg−¹⋅s−² - M is the planet's mass-w is the body's angular speed
What is a keostationary orbit :: Kerbal Space Program General …
Feb 1, 2018 · A perfect kerbostationary orbit is only possible at exactly the equator, at an exact distance fromthe center of a perfectly spherical planet. Off by even a millimeter and its not perfect. The game allows for a quite large irregulaty int he orbit …
Good height for initial orbit/satellites :: Kerbal Space Program ...
Oct 18, 2013 · What's a good height for initial orbit after takeoff but before transferring to other moons/planets? Also, when do you start turning (I usually turn east after takeoff to get a nice orbit before transferring to the moon or wherever). On another note, when making a geostationary orbit, what heights do you use? Geostationary orbit is when you're far enough away from the …
