- Also called:
- artificial satellite
- Related Topics:
- space debris
- Molniya
- scientific satellite
- Geosat
- Syncom 2
Earth satellite
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What is an instrument on an Earth satellite?
An instrument on an Earth satellite can be either an in situ measurement tool, which requires direct contact with the subject of interest, or a remote sensor, located at a distance from what it observes. Remote sensors can be passive, receiving naturally emitted information, or active, emitting energy and recording its reflection.
Satellites use various instruments to monitor weather, measure temperature, cloud cover, moisture, and surface properties such as ice and soil moisture. For example, Landsat satellites use multispectral scanners to gather data in green, red, and infrared spectral bands, which are then used to create false-color images for geological and environmental analysis.
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Why do Earth satellites need instruments?
Earth satellites need instruments to gather data and send it back to Earth, which allows scientists to gain new information about the universe that would be unobtainable otherwise. These instruments allow satellites to collect data about Earth’s surface and atmosphere and make astronomical observations.
For example, weather satellites use instruments to transmit photographs of cloud patterns and measurements of other meteorological conditions, which helps with weather forecasting. Also, the first scientific discovery from instruments orbiting in space was the Van Allen radiation belts, which Explorer 1 discovered in 1958.
8 Britannica Sources- technology of photography: Satellite and space photography
- Earth exploration: Remote sensing
- NISAR: Polarimetry and interferometry
- Earth satellite
- satellite communication: How satellites work
- space exploration: Solar and space physics
- weather forecasting: Meteorological measurements from satellites and aircraft
- undersea exploration: Navigation
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What kinds of measurements can satellite instruments make?
Satellite instruments use both active and passive remote sensors to monitor the atmosphere.
Examples of measurements:
* Temperature, pressure, and wind velocity Radiosondes, attached to helium balloons, measure these.
* Ocean salinity The Aquarius/SAC-D mission used a radiometer and a scatterometer to measure changes in the ocean’s brightness (in radio waves), which are associated with the ocean’s salt content.
* Magnetic fields Magnetometers measure the strength and direction of magnetic fields on or near Earth and in space.
* Precipitation intensity, wind speed, and direction Doppler radars measure the backscattering of electromagnetic microwave radiation and can estimate wind speed and direction.
* Lightning occurrences Ground-based detectors measure the time, location, flash polarity, and stroke count of lightning strikes.7 Britannica SourcesCreated from Britannica articles using AI. AI can make mistakes, so verify using Britannica articles. -
How do instruments on satellites collect and send data back to Earth?
Satellites use instruments for both in situ measurements, which require direct contact with the subject of interest, and remote sensing observations, where the sensors are located at a distance. Remote sensors can be passive, receiving naturally emitted information, or active, emitting energy and recording its reflection.
Data collection involves measuring various parameters, and the data is transmitted back to Earth using a communications system that includes antennas and transponders. The tracking telemetry and control (TT&C) system maintains a two-way link between the satellite and ground stations, enabling the monitoring of the satellite's position, temperature, and other parameters.
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What is the difference between passive and active satellite instruments?
Active and passive satellite instruments differ in how they gather data. Active sensors, like synthetic aperture radars (SARs), emit their own radiation, which bounces off the Earth's surface and returns to the sensor. This allows them to operate independently of external light sources, such as the Sun, and penetrate clouds. Passive sensors, on the other hand, measure electromagnetic radiation that is naturally emitted or reflected from the Earth's surface.
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How do satellite instruments help us monitor weather and climate on Earth?
Satellite instruments are essential for monitoring Earth's weather and climate by providing global quantitative data on temperature, cloud cover, moisture, and surface properties.
Meteorological satellites come in two primary types:
* Polar orbiters These satellites orbit Earth at low altitudes, offering high-resolution data and covering the entire planet every 24 hours.
* Geostationary orbiters Positioned over the Equator, these satellites provide a continuous view of a wide area, which is invaluable for tracking rapid changes in weather phenomena like thunderstorms and hurricanes.These satellites use both passive and active remote sensing technologies to gather data. They measure wind speed and direction from cloud movement, and they calculate temperature and moisture profiles using infrared data. This comprehensive monitoring helps improve weather forecasting and climate models.
7 Britannica Sources- tropical cyclone: Use of satellites and aircraft
- Earth sciences: Probes, satellites, and data transmission
- global warming: Theoretical climate models
- atmosphere: Measurement systems
- undersea exploration: Acoustic and satellite sensing
- weather forecasting: Meteorological measurements from satellites and aircraft
- hydrologic sciences: The accumulation of ice
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Earth satellite, artificial object launched into a temporary or permanent orbit around Earth. Spacecraft of this type may be either crewed or uncrewed, the latter being the most common.
The idea of an artificial satellite in orbital flight was first suggested by Sir Isaac Newton in his book Philosophiae Naturalis Principia Mathematica (1687). He pointed out that a cannonball shot at a sufficient velocity from atop a mountain in a direction parallel to the horizon would go all the way around Earth before falling. Although the object would tend to fall toward Earth’s surface because of gravitational force, its momentum would cause it to descend along a curved path. Greater velocity would put it into a stable orbit, like that of the Moon, or direct it away from Earth altogether.
On October 4, 1957, nearly three centuries after Newton had proposed his theory, the Soviet Union launched the first Earth satellite, Sputnik 1. Sputnik circled Earth every 96 minutes, and its simple radio signal was heard by scientists and radio operators across the world. The United States orbited its first satellite, Explorer 1, three months later (January 31, 1958). Explorer, though much smaller than Sputnik, was instrumented to detect radiation and discovered the innermost of the two Van Allen radiation belts, a zone of electrically charged solar particles that surrounds Earth.
Since these initial efforts, more than 5,000 Earth satellites have been orbited by more than 70 different nations. As of 2017, more than 2,000 satellites are in orbit, the majority being from Russia or the United States. The satellites vary widely in size and design, ranging from small “picosatellites” of less than a kilogram to the International Space Station, a space laboratory that is home to six astronauts and has a mass of more than 400 tons. They are equally diverse in function. Scientific satellites are chiefly used to collect data about Earth’s surface and atmosphere and to make astronomical observations. Weather satellites transmit photographs of cloud patterns and measurements of other meteorological conditions that aid in weather forecasting, while communications satellites relay telephone calls, radio and television programs, and data communications between distant parts of the world. Navigation satellites enable the crews of oceangoing vessels and airplanes to determine the position of their craft in all kinds of weather. Some satellites have distinctly military applications, such as reconnaissance and surveillance.
Satellites can be placed in any number of different orbits. The particular path selected is largely determined by the function of the spacecraft. Most weather and reconnaissance satellites, for example, are fired into a polar orbit in which Earth’s polar axis is a line on the orbital plane. Because Earth rotates under polar-orbiting satellites, they pass over its entire surface within a given time period, providing full global coverage. Communications satellites, on the other hand, are generally placed into an equatorial orbit, which enables them to circle the most densely populated regions of Earth from west to east. Moreover, communications satellites comprising a network or system are nearly always launched to a distance of 22,300 miles (35,890 km) above Earth. At this altitude, the motion of a satellite becomes synchronized with Earth’s rotation, causing the craft to remain fixed over a single location. If properly positioned, three communications satellites travelling in such a geosynchronous orbit can relay signals between stations around the world. (See also spacecraft; space exploration.)


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