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Orbiting Geophysical Observatory (OGO) Program of
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refers to the six
satellite A satellite or an artificial satellite is an object, typically a spacecraft, placed into orbit around a celestial body. They have a variety of uses, including communication relay, weather forecasting, navigation ( GPS), broadcasting, scient ...
s launched by the United States that were in use from September 1964 to 1972, designed to study the
Earth Earth is the third planet from the Sun and the only astronomical object known to Planetary habitability, harbor life. This is enabled by Earth being an ocean world, the only one in the Solar System sustaining liquid surface water. Almost all ...
's
magnetosphere In astronomy and planetary science, a magnetosphere is a region of space surrounding an astronomical object in which charged particles are affected by that object's magnetic field. It is created by a celestial body with an active interior Dynamo ...
. The satellites successfully studied the interactions between the
Earth Earth is the third planet from the Sun and the only astronomical object known to Planetary habitability, harbor life. This is enabled by Earth being an ocean world, the only one in the Solar System sustaining liquid surface water. Almost all ...
and the
Sun The Sun is the star at the centre of the Solar System. It is a massive, nearly perfect sphere of hot plasma, heated to incandescence by nuclear fusion reactions in its core, radiating the energy from its surface mainly as visible light a ...
, despite a number of technical problems. Each satellite had 20 to 25 instruments. The project manager for all 6 OGO projects was Wilfred Scull.


OGO satellites

All OGO satellites are built around a common parallelepiped-shaped platform (0.9 × 0.9 × 1.8 m). The satellite's orientation is maintained fixed in space ( 3-axis stabilized) so that one of the long faces (0.9 × 1.8 m) permanently points towards Earth. On this face, as well as on the opposite face, a surface of 0.6 m² is available for scientific experiments. The attitude control system is also responsible for keeping the solar panels continuously oriented perpendicularly to the solar rays. The cubic SOEP (Solar Oriented Experiment Package) receptacles, attached to the ends of the solar panels on both faces, can accommodate experiments on a surface of 0.1 m². At one end of the satellite's body, two OPEP-1 (Orbital Plane Experiment Package) and OPEP-2 experiment sets are mounted on an adjustable support that keeps them oriented in the direction of the satellite's forward movement. Two booms, 5.7 meters long (EP-5 and EP-6) and four booms, 1.8 meters long (EP-1 to EP-4), hold scientific experiments at their ends that must be kept away from the satellite's body to meet visibility or sensitivity constraints. Additionally, the satellite is equipped with several antennas for telecommunications, the most prominent being an adjustable
Yagi antenna Yagi may refer to: Places *Yagi, Kyoto, in Japan * Yagi (Kashihara), in Nara Prefecture, Japan * Yagi Ridge, a mountain ridge in British Columbia, Canada * Yagi-nishiguchi Station, in Kashihara, Nara, Japan * Kami-Yagi Station, a JR-West Kabe Line ...
. The scientific experiments may have their own antenna, like the one shown in the diagram extending 9 meters from the SOEP-1 experiment on the solar panel. The satellite typically has twelve appendages deployed in orbit in two sequences to avoid any interference. The attitude control system relies on horizon sensors, cold gas thrusters, and
reaction wheels A reaction wheel (RW) is an electric motor attached to a flywheel, which, when its rotation speed is changed, causes a counter-rotation proportionately through conservation of angular momentum. A reaction wheel can rotate only around its center ...
. It allows the satellite to be stabilized on 3 axes with an accuracy of 2° relative to the local vertical, 5° relative to the Sun's direction, and 5° relative to the forward movement axis. The thermal control system uses louvers that open and close to maintain a temperature of 10 to 24°C within the satellite's body and thermal resistors for scientific experiments mounted outside. Electrical power is provided by solar panels that produce 550 watts, of which 50 watts are available for scientific experiments. The energy is stored in two 28-volt nickel-cadmium batteries. The telecommunications system ensures data transfer at a rate between 1 and 64 kilobits per second. Scientific data can be transmitted in real-time or stored temporarily on one of two magnetic tape recorders with a recording speed of 1 to 4 kilobits per second and a reading speed of 64 to 128 kilobits per second. OGO 1, OGO 3, and OGO 5 were in
equatorial orbit A near-equatorial orbit is an orbit that lies close to the equatorial plane of the primary body orbited. Such an orbit has an inclination near 0°. On Earth, such orbits lie near the celestial equator, the great circle of the imaginary celestial s ...
s; OGO 2, OGO 4, and OGO 6 were in lower
polar orbit A polar orbit is one in which a satellite passes above or nearly above both poles of the body being orbited (usually a planet such as the Earth, but possibly another body such as the Moon or Sun) on each revolution. It has an inclination of abo ...
s.


OGO 1

OGO 1 (OGO-A) was successfully launched from Cape Canaveral Air Force Station on September 5, 1964 and placed in an initial orbit of 281 × 149,385  km with an inclination of 31.2°. The purpose of the OGO 1 spacecraft, the first of a series of six Orbiting Geophysical Observatories, was to conduct diversified geophysical experiments to obtain a better understanding of the Earth as a planet and to develop and operate a standardized observatory-type satellite. OGO 1 consisted of a main body that was parallelepipedal in form, two solar panels, each with a solar-oriented experiment package (SOEP), two orbital plane experiment packages (OPEP) and six appendages EP-1 through EP-6 supporting the boom experiment packages. One face of the main body was designed to point toward the Earth (+Z axis), and the line connecting the two solar panels (X axis) was intended to be perpendicular to the Earth-Sun-spacecraft plane. The solar panels were able to rotate about the X axis. The OPEPs were mounted on and could rotate about an axis which was parallel to the Z axis and attached to the main body. Due to a boom deployment failure shortly after orbital injection, the spacecraft was put into a permanent spin mode of 5 rpm about the Z axis. This spin axis remained fixed with a declination of about -10 deg and
right ascension Right ascension (abbreviated RA; symbol ) is the angular distance of a particular point measured eastward along the celestial equator from the Sun at the equinox (celestial coordinates), March equinox to the (hour circle of the) point in questio ...
of about 40 deg at launch. The initial local time of apogee was 2100 h. OGO 1 carried 20 experiments. Twelve of these were particle studies and two were magnetic field studies. In addition, there was one experiment for each of the following types of studies: interplanetary dust, VLF, Lyman-alpha, gegenschein, atmospheric mass, and
radio astronomy Radio astronomy is a subfield of astronomy that studies Astronomical object, celestial objects using radio waves. It started in 1933, when Karl Jansky at Bell Telephone Laboratories reported radiation coming from the Milky Way. Subsequent observat ...
. Real-time data were transmitted at 1, 8, or 64 kbs depending on the distance of the spacecraft from the Earth. Playback data were tape recorded at 1 kbs and transmitted at 64 kbs. Two wideband transmitters, one feeding into an omnidirectional antenna and the other feeding into a directional antenna, were used to transmit data. A special-purpose telemetry system, feeding into either antenna, was also used to transmit wideband data in real time only. Tracking was accomplished by using radio beacons and a range and range-rate S-band transponder. Because of the boom deployment failure, the best operating mode for the data handling system was the use of one of the wideband transmitters and the directional antenna. All data received from the omnidirectional antenna were noisy. During September 1964, acceptable data were received over 70% of the orbital path. By June 1969, data acquisition was limited to 10% of the orbital path. The spacecraft was placed in a standby status November 25, 1969, and all support was terminated November 1, 1971. By April 1970 the spacecraft perigee had increased to 46,000 km and the inclination had increased to 58.8 deg.


OGO-1 reentry

The University of Arizona's
Catalina Sky Survey Catalina Sky Survey (CSS; obs. code: 703) is an astronomical survey to discover comets and asteroids. It is conducted at the Steward Observatory's Catalina Station, located near Tucson, Arizona, in the United States. CSS focuses on the searc ...
(CSS), funded by NASA’s Planetary Defense Coordination Office (PDCO), detected an object late in the evening of 25 August 2020 which appeared to be on an impact trajectory with Earth. Two
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middle school students also observed the object. Maui Waena Intermediate School eighth-graders Holden Suzuki and Wilson Chau, with mentor outreach astronomer J.D. Armstrong of the
University of Hawaii A university () is an educational institution, institution of tertiary education and research which awards academic degrees in several Discipline (academia), academic disciplines. ''University'' is derived from the Latin phrase , which roughly ...
Institute for Astronomy (IfA), used data from the Las Cumbres Observatory (LCO) Faulkes Telescope North on Haleakala to track OGO-1. The University of Hawaii's
Asteroid Terrestrial-impact Last Alert System The Asteroid Terrestrial-impact Last Alert System (ATLAS) is a robotic astronomical survey and early warning system optimized for detecting smaller near-Earth objects a few weeks to days before they Impact event, impact Earth. Funded by NASA, an ...
(ATLAS), also funded by PDCO, independently observed the object. Further observations were conducted by CSS to confirm the object’s trajectory. Precision orbit calculations were conducted by the Center for
Near-Earth Object A near-Earth object (NEO) is any small Solar System body orbiting the Sun whose closest approach to the Sun ( perihelion) is less than 1.3 times the Earth–Sun distance (astronomical unit, AU). This definition applies to the object's orbit a ...
(NEO) Studies (CNEOS) at NASA’s
Jet Propulsion Laboratory The Jet Propulsion Laboratory (JPL) is a Federally funded research and development centers, federally funded research and development center (FFRDC) in La Cañada Flintridge, California, Crescenta Valley, United States. Founded in 1936 by Cali ...
, and compared to data from the
European Space Agency The European Space Agency (ESA) is a 23-member International organization, international organization devoted to space exploration. With its headquarters in Paris and a staff of around 2,547 people globally as of 2023, ESA was founded in 1975 ...
's NEO Coordination Center. The object was confirmed to be not an
asteroid An asteroid is a minor planet—an object larger than a meteoroid that is neither a planet nor an identified comet—that orbits within the Solar System#Inner Solar System, inner Solar System or is co-orbital with Jupiter (Trojan asteroids). As ...
, but in fact Orbiting Geophysical Observatory-1 (OGO-1). OGO-1 reentered Earth's atmosphere and disintegrated on Saturday evening, 29 August 2020 over Southern
French Polynesia French Polynesia ( ; ; ) is an overseas collectivity of France and its sole #Governance, overseas country. It comprises 121 geographically dispersed islands and atolls stretching over more than in the Pacific Ocean, South Pacific Ocean. The t ...
.


OGO 2

OGO 2 (OGO-C) carried about twenty scientific experiments with the objective of performing observations of polar auroras, atmospheric luminescence, energized particles, variations affecting the magnetic field and the properties of the ionosphere. These observations were to be carried out particularly in the regions overlooking the poles. The satellite was placed in a low polar orbit (414 × 1,510  km with an inclination of 87.4°) on October 14, 1965 by a Thor-Agena D launch vehicle from Vandenberg Air Force Base. Shortly after launch, the attitude control system exhausted the gas it had available to control the satellite's orientation and the satellite entered a slow rotation. Five of the experiments could no longer operate under these conditions and six others provided degraded results. On April 1966, both accumulators fail and observations are consequently limited to the illuminated portions of the orbit. By December 1966, there are only 8 operational experiments left, of which only 5 provide undegraded results. On November 1, 1967, the satellite was put into standby mode. Due to power problems, the data collected up to that time only covered a total period of 306 days. An instrument was briefly reactivated for two weeks in February 1968, and operations were definitely stopped on November 1, 1971.


OGO 3

OGO 3 (OGO-B) was launched on June 7, 1966 and placed in an orbit of 295 × 122,219  km and 31° inclination. The 21 experiments, forming the largest set of scientific instruments ever placed in orbit, all returned quality data. They were mostly identical to those flown on OGO 1. These included 4 experiments for the study of cosmic radiation, 4 devoted to plasma, two to trapped radiation, two to the Earth's magnetic field, one to the ionosphere, 3 to the study of optical radiation and radio emissions and one to micrometeorites. The instrument responsible for detecting positrons and gamma-ray bursts, which had not worked on board OGO 1, provided satisfactory results in a modified version. The satellite remained stabilized on 3 axes for 46 days. At the end of this period on July 23, 1966, a failure of one of the equipment responsible for attitude control forces the operators to stabilize the satellite by putting it into rotation (with rotation period between 90 and 125 seconds). From June 1969, data collection can only be done over 50% of the orbit. Regular data collection ends on December 1, 1969, and the mission ends on February 29, 1972.


OGO 4

The OGO 4 (OGO-D) satellite was launched on July 28, 1967 by a Thor-Agena D launcher from Vandenberg Air Force Base and placed in a polar orbit of 416 × 900  km with a declination of 86°. The objectives were the same as those of OGO 2. The satellite encounters problems with the attitude control system shortly after launch, but manages to correct them and for 18 months the satellite is stabilized on 3 axes. By mid January 1969 the magnetic tape recording system fails and the operators are no longer able to maintain the satellite's orientation. The satellite is rotated to stabilize it around its vertical axis with a slight precession and an initial period of 202 seconds. In this new configuration, 7 of the experiments are stopped because they can no longer provide viable results. On October 27, 1969, the satellite was put on standby. An experiment in receiving low-frequency waves was reactivated several times between 1970 and 1971, but operations were definitively stopped on September 27, 1971.


OGO 5

OGO 5 (OGO-E) was launched on March 4, 1969. The satellite was primarily dedicated to Earth observation, with an initial orbit of 272 × 148,228  km with an inclination of 31.1°. The attitude control system suffered a failure on August 6, 1971 and the satellite is put on standby on October 8, 1971. Three experiments were reactivated between June 1 and July 13, 1972, with operations stopping on July 14, 1972.


Non-Earth observations

In 1970 OGO-5 used its ultraviolet photometer to observe comets Encke, Tago-Sato-Kosaka (1969 IX) and Bennett (1970 II).


OGO 6

The OGO 6 (OGO-F) satellite was launched on June 5, 1969 by a Thor-Agena D launcher from Vandenberg Air Force Base and placed in a polar orbit of 413 × 1,077  km with an inclination of 82°. The satellite carried 26 scientific experiments whose objective was to observe the relationships between different characteristics of the upper atmosphere during a period of high solar activity. On June 22, 1969, a fault in a solar panel results in the creation of a negative potential of 20 volts when the solar panels are exposed to the Sun, affecting the results of seven experiments. On October 1969, a row of photovoltaic cells fails without noticeable consequences. One of the two magnetic tape recorders suffered a failure in August 1970. In September 1970, following the degradation of energy production and equipment only 14 scientific experiments are still operating normally while 3 are partially operating and 9 are stopped. But the end of June 1971, power generation problems worsen and the satellite is put on standby. A radio experiment developed by a Japanese laboratory is activated between October 10, 1971 and March 1972. Operations are completely stopped on July 14, 1972.


Notes


References

* * * {{cite news, agency=
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Spartanburg Herald-Journal The ''Spartanburg Herald-Journal'' is a daily newspaper, the primary newspaper for Spartanburg, South Carolina, United States. History The origins of the paper lie with ''The Spartan'', a weekly paper reportedly first printed in about 1842� ...
, title=U.S. to Launch Giant Satellite, page=B8, url=https://news.google.com/newspapers?id=WHwsAAAAIBAJ&sjid=XcwEAAAAIBAJ&pg=7427,4348828&dq=orbiting+geophysical+observatory&hl=en, date=August 30, 1964, access-date=December 6, 2010
Biography of Wilfred Scull, OGO project manager
Satellites orbiting Earth Satellites formerly orbiting Earth