The coverage area of Meteosat at 0¿ longitude.
The METEOSAT Satellite.
DMSP in Earth orbit.
An early military weather satellite, first launched in 1962. It was built by RCA for the National Reconnaissance Office and used components from NASA's TIROS satellites, but had a superior design and was smaller than TIROS.
A military weather satellite of the mid-1960s from Program 417, predecessor to the modern Defense Meteorological Satellite Program, designed for the National Reconnaissance Office.
The international satellite-based search and rescue system makes use of equipment carried on U.S. polar-orbiting and geosynchronous meteorological satellites and on Russian satellites.
GOES coverage area.
Artist's conception of NIMBUS meteorological satellite system. In: Plan for a National Meteorological Satellite System, produced by the National Coordinating Committee for Aviation Meteorology, April 1961.
The first television picture from space, produced on TIROS 1, April 1, 1960.
Making adjustments to TIROS II satellite prior to launch. Small square objects are 9,260 solar cells. TIROS II was the first meteorological satellite to have infra-red sensors as well as television cameras. It was launched November 23, 1960 and weighed 280 pounds.
An early TIROS satellite - later models had cameras mounted on sides.
Tiros-1 was rocketed into space aboard a Thor-Able launch vehicle in the early hours of April 1, 1960, from Cape Canaveral, Florida.
GOES-8 image, February 24, 2002.
Beginning in the early 1960s, meteorological, or weather, satellite programs have been an important focus of government agencies. In the United States, the National Aeronautics and Space Administration (NASA), the National Oceanic and Atmospheric Administration (NOAA), and the Department of Defense (DoD) have all been involved with developing and operating weather satellites. In Europe, the European Space Agency (ESA) and EUMETSAT (European Organisation (the European spelling for “Organization”) for the Exploitation of Meteorological Satellites) operate the meteorological satellite system.
The world's first weather satellite, a polar-orbiting satellite, was launched from Cape Canaveral, Florida, on April 1, 1960. Named “TIROS” for Television Infrared Observation Satellite, this was NASA's first experimental step to determine if satellites could be useful in the study of the Earth and whether they could continue operating for an extended period of time. The series proved extremely successful, with one satellite operating for almost five years and several operating more than three years.
An operational system of meteorology satellites flying in low-Earth orbit (about 450-470 nautical miles [833-870 kilometers] altitude) began operating in 1970. These satellites were called the Improved TIROS Operational System (ITOS) at launch and NOAA once they were checked out and became operational. The primary objective of this series of sun-synchronous satellites was to provide improved infrared and visual observations of Earth cloud cover for use in analyzing weather and forecasting. Other objectives included measuring snow and ice and the sea surface, and gathering information on the vertical structure of temperature and moisture in the atmosphere on a regular daily basis. Six of the eight satellites in this series were launched and operated successfully, with one operating more than four years.
NASA's Nimbus satellites were flown from 1964 through 1978, as advanced research satellites that tested new sensing instruments and data-gathering techniques rather than as operational weather satellites. The Environmental Science Services Administration (former name for the National Weather Service), however, did become a routine user of Nimbus data. This data was valuable for its coverage of conditions over oceans and other areas where few other upper atmospheric measurements were made. Instruments on the Nimbus satellites included microwave radiometers, atmospheric sounders, ozone mappers, the Coastal Zone Color Scanner, and infrared radiometers and provided significant global data on sea-ice coverage, atmospheric temperature, atmospheric chemistry (i.e., ozone distribution), the amount of radiation in the Earth's atmosphere, and sea-surface temperature. The Total Ozone Mapping Spectrometer (TOMS) instrument aboard the final Nimbus, Nimbus-7, mapped the extent of the phenomenon known as the “ozone hole.”
The first series of TIROS satellites was followed by a series that began with the October 1978 launch of TIROS-N, an experimental spacecraft that served as a model for the operational follow-on series: NOAA-6 through NOAA-17. The technological improvements integrated into this series of satellites, the current ATN or Advanced TIROS series (the launch of NOAA-17 is planned for 2004), have provided higher resolution images, and more day and nighttime data for both local and global areas than the earlier series. Polar-orbiting satellites can collect data for almost the entire Earth, and when two operate simultaneously, as this system is designed, environmental data for any region of the Earth is collected at least twice every 12 hours. This series of satellites has experienced only one launch failure, and almost all of the satellites have greatly exceeded their two-year expected lifetime. NOAA-8, launched in March 1983, was the first to carry search and rescue transponders. This international humanitarian system, with 29 participating nations, allows aircraft, ships, and people in distress who carry transmitters or beacons to signal the satellite, which then transmits the signal to a terminal on the ground where rescue operations begin. As was true with the earlier satellites, NASA is responsible for development, launch, and checkout of the satellites. Once operational, NOAA operates them.
Geosynchronous weather satellites provide a different type of coverage. Flying in orbit some 22,400 miles (35,790 kilometers) above the equator, a pair of satellites provides the continuous day and nighttime monitoring of almost an entire hemisphere necessary for intensive data analysis. NASA launched the first geosynchronous meteorological satellite (SMS-1) on May 17, 1974, from Cape Canaveral Florida. GOES-1, launched on October 16, 1975, was the first of the Geostationary Operational Environmental Satellites (GOES). It formed part of a two-satellite constellation that viewed nearly 60 percent of the Earth's surface. Twelve more GOES have been launched since, with only one launch failure. GOES-7, launched in 1987, inaugurated the use of geosynchronous satellites for international search and rescue efforts. The search and rescue system became operational with GOES-8, which was launched in 1994.
GOES-8 was the first satellite to use three-axis stabilization rather than spin stabilization, which resulted in significant improvements in gathering weather imagery and atmospheric data. It also was the first to carry separate instruments that captured images and that atmospheric data at the same time. These instruments, called Imager and Sounder, have been the primary instruments aboard the satellites. They enable researchers to gather data continuously without having to alternate between using two operating modes on a single instrument. The newest GOES can also use the Global Positioning System for search and rescue operations to locate distress signals precisely, resulting in much better response time for providing rescue assistance. GOES-12, launched on July 23, 2001, was also the first to carry a solar x-ray imager, an instrument that points toward the sun rather than the Earth and observes the sun's x-ray emissions, providing early detection and location of solar flares. As with the polar-orbiting satellites, NASA manages development, launch, and checkout of these satellites and then turns them over to NOAA for operation.
NOAA also currently operates the Defense Meteorological Satellite Program (DMSP), a near-polar-orbiting series of satellites initiated by the Defense Department in the mid-1960s and the responsibility of the U.S. Air Force. Each DMSP satellite, orbiting at approximately 516 miles (830 kilometers) above the Earth, crosses any point on the Earth up to twice a day. They see such environmental features as clouds, bodies of water, snow, fire, and pollution in the visual and infrared spectra. Scanning radiometers record information that can help determine cloud type and height, land and surface water temperatures, water currents, ocean surface features, ice, and snow. Communicated to terminals on the ground, the data is processed, interpreted by meteorologists, and used in planning and conducting U.S. military operations worldwide.
The earliest DMSP satellites were 90-pound (41-kilogram) spin-stabilized satellites equipped with shutter-style TV cameras. The photos obtained were relayed to Earth and received by two stations at retired Nike missile sites in Washington and Maine. The photos were then sent to Air Force Global Weather Central at Offutt Air Force Base, Nebraska, where technicians would transform the electronic signals into Polaroid photographs and piece the photos together to form a mosaic that represented the weather observed from the orbiting satellite. Meteorologists then provided flight crews and commanders with current observations for their missions. These older spacecraft encountered problems with gaps in the photos and errors in storm location caused by the inability of the satellites to point accurately toward their target.
Better spacecraft technology in the 1970s resulted in improved optics, signal processing, and larger payloads. Gaps in the photos were eliminated, and meteorological data could be gathered near the horizon, allowing meteorologists to see “around the bend.” Further advancements allowed data to be collected in partial moonlight, and infrared processing enabled night viewing. The late 1970s and early 1980s, saw improvements in attitude control (the direction in which the spacecraft pointed) and increased onboard processing through the use of multiple onboard computers. With the enhanced equipment on board, DMSP satellites currently weigh more than 1,400 pounds (635 kilograms).
On May 5, 1994, President Bill Clinton decided to merge America's military and civil polar-orbiting operational meteorological satellite systems into a single, national system that could satisfy both civil and national security requirements for space-based environmental data. Called the National Polar-orbiting Operational Environmental Satellite System (NPOESS), it is estimated that the first converged satellite will be available for launch toward the end of the first decade of the 21st century.
The European meteorological satellite system is called Meteosat. First proposed by the French national space agency Centre National d'Etudes Spatiales (CNES), in 1969, eight member nations of the European Space Research Organization (ESRO), the predecessor to ESA, decided in 1972 to finance the effort. On November 23, 1977, Meteosat-1 was launched from Cape Canaveral, Florida. Meteosat-2 followed in June 1981, launched from Kourou, French Guyana, as were all later Meteosat satellites. The most recent satellite, Meteosat-7, was launched in 1997. Currently, EUMETSAT and ESA are cooperating on the production of a completely new system to take over and significantly improve the operational service by 2003. This will be accomplished through the Meteosat Second Generation group of satellites. (EUMETSAT, Europe's meteorological satellite organization, is an intergovernmental organization created through an international convention agreed to by 17 European member states.)
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