|Major Contractors||Lockheed Martin|
|Mission Type||Earth Observation|
|Launch||September 15, 1991 from Space Shuttle|
|Mission Duration||September 15, 1991–December 15, 2005|
|Semimajor Axis||600 lm|
|Orbital Period||95.9 minutes|
|Cryogenic Limb Array Etalon Spectrometer (CLAES)||Determines concentrations and distributions of gases in atmosphere|
|Improved Stratospheric and Mesospheric Sounder (ISAMS)||Creates a temperature profile of the middle atmosphere|
|Microwave Limb Sounder (MLS)||Create vertical profiles of atmospheric gases, temperature, pressure and cloud ice|
|Halogen Occultation Experiment (HALOE)||Profile the middle atmosphere composition and temperature|
|High Resolution Doppler Imager (HRDI)||Uses Doppler shift to determine horizontal winds|
|Wind Imaging Interferometer (WINDII)||Senses temperature and winds in the mesosphere and lower thermosphere|
|Solar Ultraviolet Spectral Irradiance Monitor (SUSIM)||Measures the absolute irradiance of the solar ultraviolet (UV) light|
|Solar/Stellar Irradiance Comparison Experiment (SOLSTICE)||(characteristics)|
|Particle Environment Monitor (PEM)||(characteristics)|
|Active Cavity Radiometer Irradiance Monitor (ACRIM II)||(characteristics)|
The 5900 kg (13,000 lb) satellite was launched during Space Shuttle mission STS-48 in 1991. The original mission life was to be three years. As of June 2005, six of the ten instruments were still operational. UARS orbits at an altitude of 375 miles with an orbital inclination of 57 degrees.
A final orbit lowering burn, followed by the "passivation" of the Satellite's systems was performed in early December, 2005.
CLAES is a spectrometer that determines the concentrations and distributions of nitrogen and chlorine compounds, ozone, water vapor and methane. It does this by inferring the amount of gases in the atmosphere by measuring the unique infrared signature of each gas.
In order to differentiate the relatively weak signature of trace gases from the background radiation in the atmosphere, CLAES had to have high resolution and sensitivity. To achieve this, the instrument combined a telescope with an infrared spectrometer. The whole instrument was cryogenically cooled to keep heat from the instrument from interfering with the readings. The cryogenics system consists of an inner tank of solid neon at −257 °C (−430 °F) and an outer tank of solid carbon dioxide at −150 °C (−238 °F). As the neon and carbon dioxide evaporated, they kept the instrument cool. The final cryogens evaporated from the instrument on May 5, 1993 and the instrument warmed up ending its useful life.
The instrument looked sideways out of the UARS platform to allow the instrument to look through the stratosphere and the lower mesosphere. CLAES produced a 19-month global database showing the vertical distributions of important ozone-layer gases in the stratosphere and their variation with time of day, season, latitude, and longitude.
ISAMS is an infrared radiometer for measuring thermal emission from the Earth’s limb (the line of the horizon as seen from UARS), on both sides of the spacecraft. It used the pressure-modulation technique to obtain high spectral resolution, and innovative stirling-cycle coolers to achieve high detector senstivity. The specific objectives of ISAMS were (i) To obtain measurements of atmospheric temperature as a function of pressure, from the tropopause to the mesopause, with good accuracy and spatial resolution, and hence to study the structure and dynamics of the region, (ii) To investigate the distribution and variability of water vapour in the middle atmosphere, to determine its role in the atmospheric general circulation, and its sources and sinks in the middle atmosphere, (iii) To measure the global distribution of oxides of nitrogen and hence to investigate their origins and their roles in catalytic cycles which control the amount of ozone in the stratospheric ozone layer. It also made extensive observations of volcanic aerosols and polar stratospheric clouds in the middle atmosphere. The instrument operated from September 1991–July 1992.
The MLS detects naturally occurring microwave thermal emissions from Earth’s limb to create vertical profiles of atmospheric gases, temperature, pressure and cloud ice. MLS looks 90° from the angle of UARS’ orbit.
Thermal radiation enters the instrument through a three-mirror antenna system. The antenna mechanically scans in the vertical plane through the atmospheric limb every 65.5 seconds. The scan covers a height range from the surface up to 90 km (55 miles). Upon entering the instrument, the signal from the antenna is separated into three signals for processing by different radiometers. The 63-GHz radiometer measures temperature and pressure. The 183-GHz radiometer measures water vapor and ozone. The 205-GHz radiometer measures ClO, ozone, sulfur dioxide, nitric acid and water vapor.
As of June 2005, the 63- and 205-GHz radiometers are operational. The 183-GHz radiometer failed after 19 months of operation.
HALOE uses solar occultation to measure simultaenous vertical profiles of Ozone (O3), Hydrogen Chloride (HCl), hydrogen fluoride (HF), Methane (CH4), Water Vapor (H2O), Nitric oxide (NO), Nitrogen Dioxide (NO2), Temperature, Aerosol Extinction, Aerosol composition and size distribution versus atmospheric pressure at the Earth’s limb. The measurements are done at eight different wavelengths of infrared across a 1.6 km (1.0 mile) wide field of view of Earth’s limb.
A vertical scan of the atmosphere is obtained by tracking the sun during occultation. The scan will measure the amount of solar energy absorbed by gases in the atmosphere.
In order to support scanning, the instrument comes in two parts, the optics unit on a two-axis gimbal and a fixed electronics unit. The optics unit contains a telescope that collects solar energy as well as the gas detectors. The electronics unit handles data, motor control and power for the instrument.
HRDI observes the emission and absorption lines of molecular oxygen above the limb of the Earth, uses the Doppler shift of the lines to determine horizontal winds and uses the line shapes and strengths to obtain information about temperature and atmospheric make-up.
The telescope uses a narrow field of view to prevent Doppler shift variation across the field of view from distorting the results. Input from the telescope is fed to the processor via a fiber optic cable.
The WINDII instrument measures wind, temperature and emission rate from airglow and aurora. The instrument looks at Earth’s limb from two different angles, 45 degrees and 135 degrees off the spacecraft’s angle of motion. This allows the instrument to read the same areas of the sky from two angles within a few minutes of the previous reading.
The instrument consists of an interferometer which feeds to a CCD camera. The two telescopes (45 degrees and 135 degrees) each have a one meter long baffle tube to reduce stray light during daytime viewing. The input from the telescopes is positioned side-by-side on the CCD so both views are imaged simultaneously.
SUSIM measures ultraviolet (UV) emissions from the sun. The observations are made both through vacuum and through occultations of the sun through the atmosphere. This allows a comparison of the amount of UV light that reaches the earth and the amount abosorbed by the upper atmosphere.
Because of the energy of UV, instrument degradation is a major issue. To help with this problem, the instrument contains two identical spectrometers. One will is used almost continuously during the daylight portion of UARS’ orbit. The second is used infrequently to verify the sensitivity of the first.
Global change in the upper atmosphere: the upper atmosphere is cooling and contracting as a result of rising greenhouse gas concentrations. These changes are Likely to affect the orbital lifetimes of satellites.(ATMOSPHERE)
Nov 24, 2006; Life on Earth is affected more directly by climate change near the surface than in the upper atmosphere. However, as the story of...