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Radar can track storm systems, because precipitation reflects electromagnetic fields at certain frequencies. Radar can also render precise maps. Radar systems are widely used in air-traffic control, aircraft navigation, and marine navigation. High-power radar, using large dish antennas, has been used to measure distances to the moon, other planets, asteroids, and artificial satellites. From unmanned space probes, radar has been used to map Venus, whose surface is obscured at visible wavelengths by a thick layer of clouds. Radar has been employed by NASA (the U.S. National Aeronautics and Space Administration) to make highly detailed topographical maps of the earth's surface as well. Most radar systems determine position in two dimensions: azimuth (compass bearing) and radius (distance). The display is in polar coordinates. A rotating antenna transmits RF pulses at defined intervals. The delay between a transmitted pulse and the echo, or return pulse, determines the radial position of the plotted point(s) for each azimuth direction on the display. The greater the echo delay from a particular object in space, the farther from the display center its point appears. The maximum range of a UHF or microwave radar system depends on the height of the antenna above average terrain, the topography of the surface in the region, the atmospheric conditions in the region, and in some cases the level of radio background noise. Radar is known to the general public for its use by law enforcement in determining the speeds of motor vehicles. This type of radar does not display the exact position of an object, but determines its radial speed vector from the Doppler effect. A radar detector, which consists of a simple UHF/microwave broadband receiver, can be used in a car or truck to warn drivers of the presence of police radar. Radar detectors are illegal in some states. The Weather Service uses so-called Doppler radar to determine not only the positions and extent of storm systems, but wind patterns and velocities aloft. Doppler radar employs a combination of position-sensing and speed-sensing radar, making it possible to ascertain the locations and intensity of severe thunderstorms, hurricanes, and tornadoes. Radar has been used on the high-frequency (HF) radio bands, between approximately 5 MHz and 20 MHz, in an attempt to obtain early warning in the event of a nuclear assault via ballistic missiles. The ionosphere refracts HF waves, allowing much greater system range than is possible with radar at UHF or microwave frequencies. During the 1970s and early 1980s, the signals from these systems became infamous because of the interference they caused. Radio amateurs coined the term woodpecker to describe the sound of HF over-the-horizon radar pulses in communications receivers. 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Spatial samples are acquired every 275 meters. Over a period of 7 minutes, a 360 km wide swath of Earth comes into view at all 9 angles. Special attention has been paid to providing highly accurate absolute and relative calibration, using on-board hardware consisting of deployable solar diffuser plates and several types of photodiodes. To complement the on-board calibration effort, a validation program of in situ measurements are being conducted, involving field instruments, one of which is the PARABOLA III, which automatically scans the sky and ground at many angles, and a multi-angle aircraft camera (AirMISR). Global coverage with MISR is acquired about once every 9 days at the equator; the nominal lifetime of the mission is 6 years. MISR was built for NASA by the Jet Propulsion Laboratory in Pasadena, California, and is one of five instruments launched into polar orbit aboard NASA's Terra spacecraft in August 1999. The spacecraft flys in a sun-synchronous orbit, designed so that it crosses the equator every 98 minutes, always at 10:30 a.m. local time, as Earth rotates below. 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Radiometers","definition":["INFRARED RADIOMETERS are meters used to detect and measure radiant energy that is either electromagnetic or acoustic and that is also in the infrared part of the electromagnetic spectrum (visible spectrum at its red end); Infrared is electromagnetic wave frequencies below the visible range which have wavelengths longer than light but shorter than radio waves. 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The objective is to provide high-resolution multispectral imagery with high geo-location accuracy. The camera design employs a pushbroom imaging concept. Extensive use of existing state-of-the-art technologies is made regarding such items as: a) camera alignment procedures, b) telescope thermal control and mechanical assembly principles, c) video processing techniques. 49) 50) 51) 52) 53) The industrial team consists of the following partners: • Thales Alenia Space, France: Instrument, telescope, detection unit, telescope structure & thermal control, video electronics, video power supply, harness • Thales Alenia Space España: Instrument service module • Sener: Shutter, detection unit structure & thermal control • E2V (Chelmsford, UK): Pan & MS CCD imaging detectors • SESO (Société Européenne de Systèmes Optiques), France: telescope mirror manufacturing • EADS Sodern: FPA (Focal Plane Assembly) • Sagem: Spectral filters. Equipment Technology Implementation Panchromatic detector CCD detector array with TDI (Time Delay Integration) mode of operation and anti-blooming structure High resolution imaging without satellite slowing. No light spreading due to blooming. Very long multispectral stripe filters Assembly of a single substrate with 4 stripe filters over the detector window Separate the different spectral bands in the FOV. Minimize chromatic aberrations Highly integrated detection unit Integrated focal plane and video electronics. Highly integrated ASIC technology Compact detection function integrated in the camera Telescope Carbon / carbon structure and light-weighted Zerodur optics Low mass/high thermal stability, highly polished mirror surfaces Optical assembly: The instrument employs a Korsch all-reflective 4 mirrors telescope design with TMA (Three Mirror Anastigmatic) optics. An additional plane mirror (MR) is used to enhance the instrument compactness. The imaging geometry optimization features a primary mirror size of 650 mm diameter, which suits well to the detectors performance and the orbit characteristics. The instrument architecture chosen is organized around a central plane structure supporting the primary mirror, the tertiary mirror, the plane mirror (MR), and a central cylinder that supports the secondary mirror. The optical assembly consists of an on-axis part (M1 + M2 collector mirrors) and an off-axis part (M3 + MR mirrors) feeding the different focal planes. The optics system of the instrument uses state-of-the-art techniques such as SiC-100 (silicon carbide) material for the mirrors and the telescope structure, specific detectors, and a modular video chain design. EADS Sodern is responsible for the development of the FPA. The FPA is offering a wide variety of new technologies for the imaging function. The size of the observed image is close to 400 mm and is analyzed in 30,000 samples in Pan and 7,500 in MS.. The focal plane assembly consists of two symmetrical arrangements of Pan and MS detectors. The beam splitter is made of a set of mirrors. The spectral selection is made by optical filters placed very close in front of the detectors. Pan filters and MS stripe line filters are space-qualified multi-layer coatings deposited on glass substrates. Each filter is composed of a high-pass filter and a low-pass filter. An absorbing material deposited between the MS filters isolates each band from the others to avoid interband straylight. Attitude sensors (star tracker heads and gyroscope heads) are placed on this central instrument structure to improve the performance. A dedicated supporting truss structure ensures the instrument interface with respect to the bus. The detector thermal radiator has its own supporting structure. The instrument design employs carbon material for the structure (the carbide characteristics are: very low coefficient of thermal expansion, very low density, resulting in a light telescope, and a simple thermal control) and Zerodur material for the mirrors. The instrument focus mechanism is placed onto the tertiary mirror. This position offers an optimum between mechanism and accuracy. The instrument includes also an internal shutter to protect it from sun radiation in non-operational phases such as launch, attitude acquisition, or safe modes. The shutter is placed behind the primary mirror to protect only the tertiary mirror and the detection cavity. Spectral bands Pan: 480-820 nm; TDI is only used for Pan data MS bands in nm B0= 450-530 (blue), B1= 510-590 (green), B2= 620-700 (red), B3= 775-915 (NIR) Optical system 65 cm aperture diameter, focal length of 12.905 m, f/20, TMA optics Spatial resolution, GSD 0.7 m for Pan, 2.8 m for MS bands Swath width, FOR 20 km at nadir, 60º (FOR=Field of Regard); Each satellite will be able to collect imagery anywhere within an 800 km wide ground strip, covering 200 km in 11 s or 800 km in 25 s, including stabilization time. SNR > 147 (Pan), > 130 (MS) MTF in Pan band 0.07 at Nyquist frequency fe/2 (1/2 x 0.7 m-1) Note: “fe” is the sampling frequency (fréquence d'échantillonnage) Detectors Pan array assembly: 5 x 6000 (30,000 pixels cross-track) pixel size: 13 µm MS array assembly: 5 x 1500 (7500 pixels in cross-track) pixel size: 52 µm TDI detector data rate 290 Mpixel/s (total) or about 700 Mbit/s per detector; or 3.5 Mbit/s (max) Data quantization 12 bit per pixel (correlated dual sampling) Image location accuracy 1 m (with ground control points), 20 m without GCP (99.7%), 10 m (90%) Image location accuracy <0.9 pixel Pan over 12 s with a time linear error model (with GCPs) Line-of-sight frequency <0.1 pixel (dynamic stability) Source data rate, downlink 4.5 Gbit/s (max), 465 Mbit/s in 3 x 155 Mbit/s X-band channels Data compression Wavelet compression algorithm with an average compression factor of 4 Instrument mass, power ~ 195 kg (< 14 service electronics), ~ 400 W Instrument size L < 1594 mm W < 980 mm H < 2235 mm Pointing agility of S/C Roll of 60º within 25 s; Pitch of 60º within 25 s."],"obsolete":false,"matchType":"prefLabel","ontologyType":"ONTOLOGY","@id":"https://terra-vocabulary.org/ncl/FAIR-Incubator/earthsciencesensors/c_a044a00a","@type":"http://www.w3.org/2002/07/owl#Class","links":{"self":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_a044a00a","ontology":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS","children":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_a044a00a/children","parents":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_a044a00a/parents","descendants":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_a044a00a/descendants","ancestors":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_a044a00a/ancestors","instances":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_a044a00a/instances","tree":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_a044a00a/tree","notes":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_a044a00a/notes","mappings":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_a044a00a/mappings","ui":"http://earthportal.eu/ontologies/TERRA_VOCABS_ESS?p=classes&conceptid=https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_a044a00a","@context":{"self":"http://www.w3.org/2002/07/owl#Class","ontology":"http://data.bioontology.org/metadata/Ontology","children":"http://www.w3.org/2002/07/owl#Class","parents":"http://www.w3.org/2002/07/owl#Class","descendants":"http://www.w3.org/2002/07/owl#Class","ancestors":"http://www.w3.org/2002/07/owl#Class","instances":"http://data.bioontology.org/metadata/Instance","tree":"http://www.w3.org/2002/07/owl#Class","notes":"http://data.bioontology.org/metadata/Note","mappings":"http://data.bioontology.org/metadata/Mapping","ui":"http://www.w3.org/2002/07/owl#Class"}},"@context":{"@vocab":"http://data.bioontology.org/metadata/","prefLabel":"http://www.w3.org/2004/02/skos/core#prefLabel","definition":"http://www.w3.org/2004/02/skos/core#definition","obsolete":"http://www.w3.org/2002/07/owl#deprecated","@language":"en"}},{"prefLabel":"SEVIRI","definition":["This radiometer is the main instrument on board the Meteosat Second Generation (MSG). MSG is a cooperation program of ESA (European Space Agency) and EUMETSAT (European Organisation for the Exploitation of Meteorological Satellites). This multi-wavelength camera, called SEVIRI, provides images of the Earth disc with cloud, land, ocean, snow and other information made visible by day and by night. It takes one full resolution image every 15 minutes, thus illustrating the weather in motion. Its operating principle is based on collecting the Earth&#039;s radiation by means of a telescope and focusing it on detectors sensitive to 12 different bands of the electromagnetic spectrum. This is followed by the electronic processing of the signals provided by the detectors. The infrared channels require low detector temperature and hence a large passive cooler. The instrument&#039;s overall mass is 270 kg and its power consumption is nominally less than 123 W during operations."],"obsolete":false,"matchType":"prefLabel","ontologyType":"ONTOLOGY","@id":"https://terra-vocabulary.org/ncl/FAIR-Incubator/earthsciencesensors/c_0e364531","@type":"http://www.w3.org/2002/07/owl#Class","links":{"self":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0e364531","ontology":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS","children":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0e364531/children","parents":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0e364531/parents","descendants":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0e364531/descendants","ancestors":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0e364531/ancestors","instances":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0e364531/instances","tree":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0e364531/tree","notes":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0e364531/notes","mappings":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0e364531/mappings","ui":"http://earthportal.eu/ontologies/TERRA_VOCABS_ESS?p=classes&conceptid=https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0e364531","@context":{"self":"http://www.w3.org/2002/07/owl#Class","ontology":"http://data.bioontology.org/metadata/Ontology","children":"http://www.w3.org/2002/07/owl#Class","parents":"http://www.w3.org/2002/07/owl#Class","descendants":"http://www.w3.org/2002/07/owl#Class","ancestors":"http://www.w3.org/2002/07/owl#Class","instances":"http://data.bioontology.org/metadata/Instance","tree":"http://www.w3.org/2002/07/owl#Class","notes":"http://data.bioontology.org/metadata/Note","mappings":"http://data.bioontology.org/metadata/Mapping","ui":"http://www.w3.org/2002/07/owl#Class"}},"@context":{"@vocab":"http://data.bioontology.org/metadata/","prefLabel":"http://www.w3.org/2004/02/skos/core#prefLabel","definition":"http://www.w3.org/2004/02/skos/core#definition","obsolete":"http://www.w3.org/2002/07/owl#deprecated","@language":"en"}},{"prefLabel":"TSX-1","definition":["Synthetic Aperture Radar (SAR) The primary payload is a Synthetic Aperture Radar (SAR) with an active antenna that allows for the utilization of different imaging modes and can be used in a very flexible manner. With radar instruments various frequency ranges of the radar spectrum can be observed, the so-called bands. TerraSAR-X is operated in the X-band, which is lying at a frequency around 9.65 GHz, corresponding to a wavelength of about 3 centimeters. The technology of the active, phase-con-trolled antenna enables a high flexibility and mission efficiency. While in case of passive systems the whole radar antenna or even the satellite must be rotated in order to align the antenna onto the tar-get area, the active antenna of TerraSAR-X can steer its radar pulses in a certain direction. The antenna is 4.80 meters long and80 centimeters wide. The satellite is designed in a way that it can be installed, together with its antenna at its full size, on the launch vehicle. In this way a complex unfolding mechanism can be avoided. The TerraSAR-X radar can operate in two polarizations, H (horizontal) and V (vertical)and consists of 12 antenna panels, each equipped with 32 slotted waveguide radiators. Each of these waveguides is fitted with a transmit/receive module (TRM), so that the whole antenna consists of 384 TRMs. This allows the control of the radar beam by 0.75° in the flight direction and 20° perpendicular to the flight direction. The data received are stored in a mass storage system with a 256 Gbit capacity before they are transmitted via a 300 Mbit per second X-band system to the ground station. The active antenna enables different imaging methods to be used with very fast switching between them: - In the Spotlight Mode the radar image records an area of 5 to 10 by 10 kilo-meters size. In this manner a maximum resolution of up to one meter is achieved. - In the Stripmap Mode the satellite images a strip of 30 kilometers width and a maximum length of 1,500 kilo-meters. The resolution is 3 meters. - In the ScanSAR mode a strip of 100 kilometers width and 1,500 kilometers maximum length is scanned with a resolution of 18 meters. The elements of the SAR instrument are designed fully redundant, which means that two fully functional sets of electronic boxes exist. This allows to utilize a new concept that envisages the simultaneous activation of both chains. This experimental operating scenario is called “Dual Receive Antenna“ (DRA) mode, in which the antenna is electrically separated into two halves, and the data received are independently recorded and evaluated. In this way it is possible to apply interesting new techniques such as Along Track Interferometry, fully polarimetric data recording, or an increase in geometric resolution. Along Track Interferometry allows, amongst other things, the detection of moving objects such as, for example, cars or ships. This application is of particular interest both for traffic re-search, and also for the investigation of ocean currents, for example."],"obsolete":false,"matchType":"prefLabel","ontologyType":"ONTOLOGY","@id":"https://terra-vocabulary.org/ncl/FAIR-Incubator/earthsciencesensors/c_0109745c","@type":"http://www.w3.org/2002/07/owl#Class","links":{"self":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0109745c","ontology":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS","children":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0109745c/children","parents":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0109745c/parents","descendants":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0109745c/descendants","ancestors":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0109745c/ancestors","instances":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0109745c/instances","tree":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0109745c/tree","notes":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0109745c/notes","mappings":"https://data.earthportal.eu/ontologies/TERRA_VOCABS_ESS/classes/https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0109745c/mappings","ui":"http://earthportal.eu/ontologies/TERRA_VOCABS_ESS?p=classes&conceptid=https%3A%2F%2Fterra-vocabulary.org%2Fncl%2FFAIR-Incubator%2Fearthsciencesensors%2Fc_0109745c","@context":{"self":"http://www.w3.org/2002/07/owl#Class","ontology":"http://data.bioontology.org/metadata/Ontology","children":"http://www.w3.org/2002/07/owl#Class","parents":"http://www.w3.org/2002/07/owl#Class","descendants":"http://www.w3.org/2002/07/owl#Class","ancestors":"http://www.w3.org/2002/07/owl#Class","instances":"http://data.bioontology.org/metadata/Instance","tree":"http://www.w3.org/2002/07/owl#Class","notes":"http://data.bioontology.org/metadata/Note","mappings":"http://data.bioontology.org/metadata/Mapping","ui":"http://www.w3.org/2002/07/owl#Class"}},"@context":{"@vocab":"http://data.bioontology.org/metadata/","prefLabel":"http://www.w3.org/2004/02/skos/core#prefLabel","definition":"http://www.w3.org/2004/02/skos/core#definition","obsolete":"http://www.w3.org/2002/07/owl#deprecated","@language":"en"}},{"prefLabel":"Aerosol Collectors","definition":["Aerosol collectors are devices used to measure aerosols usually deposited directly onto films or sensitive detectors. Collectors can measure varying sizes of aerosols depending on the application. Some aerosol collectors are ground-based, while others are aircraft-based or even placed on 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Video cameras are used primarily in two modes. The first, characteristic of much early television, is what might be called a live broadcast, where the camera feeds real time images directly to a screen for immediate observation. A few cameras still serve live television production, but most live connections are for security, military/tactical, and industrial operations where surreptitious or remote viewing is required. The second is to have the images recorded to a storage device for archiving or further processing; for many years, videotape was the primary format used for this purpose, but optical disc media, hard disk, and flash memory are all increasingly used. 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The CPR was developed jointly by NASA/JPL and the Canadian Space Agency (CSA). The overall design of the CPR is simple, well understood, and has strong heritage from many cloud radars already in operation in ground-based and airborne applications. Most of the design parameters and subsystem configurations are nearly identical to those for the Airborne Cloud Radar, which has been flying on the NASA DC-8 aircraft since 1998. The design of the CPR is driven by the science objectives. The original requirements on CPR were: sensitivity defined by a minimum detectable reflectivity factor of -30 dBZ, along-track sampling of 2 km, a dynamic range of 70 dB, 500 m vertical resolution and calibration accuracy of 1.5 dB. The minimum detectable reflectivity factor requirement was reduced to -26 dBZ when the mission was changed to put CloudSat into a higher orbit for formation flying. 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Thermal Infrared Sensor (TIRS) will measure land surface temperature in two thermal bands with a new technology that applies quantum physics to detect heat. TIRS was added to the satellite mission when it became clear that state water resource managers rely on the highly accurate measurements of Earth's thermal energy obtained by LDCM's predecessors, Landsat 5 and Landsat 7, to track how land and water are being used. With nearly 80 percent of the fresh water in the Western U.S. being used to irrigate crops, TIRS will become an invaluable tool for managing water consumption. TIRS uses Quantum Well Infrared Photodetectors (QWIPs) to detect long wavelengths of light emitted by the Earth whose intensity depends on surface temperature. These wavelengths, called thermal infrared, are well beyond the range of human vision. QWIPs are a new, lower-cost alternative to conventional infrared technology and were developed at NASA's Goddard Space Flight Center in Greenbelt, Md. The QWIPs TIRS uses are sensitive to two thermal infrared wavelength bands, helping it separate the temperature of the Earth's surface from that of the atmosphere. 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It is a fixed, nadir-viewing imager with a single spectral channel covering the 620-670 nm region, selected to match band 1 of the MODIS (MODerate resolution Imaging Spectroradiometer) instrument on Aqua. 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Several versions of the NAOMI instrument have already been developed with a GSD from 1.5 m to 2.5 m, and swath widths from 10 km up to 60 km. All of them are based on the same telescope concept implementing one or several focal planes units in the same camera, and even two cameras in the same instrument as for the SPOT-6 & SPOT-7 program. NAOMI instruments can be embarked on small platforms (Myriade class) or larger platforms (Astrosat-250). The IEU (Instrument Electronics Unit) can accommodate internal mass memory functions or can be coupled with high capacities mass memories like CORECI equipment also developed by Astrium SAS. The main building blocks of the instrument are: • A highly stable, light and compact telescope built in SiC material, with a simple thermal control. • A focal plane, embedding TDI (Time Delay Integration) detector, a PAN CCD and four XS (multispectral) detectors equipped with strip filters and coupled with front end electronics. 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It takes benefit of all the heritage and skills acquired in CCD architecture definition and in operating with the ultimate conditions of speed and performances. The result of this customization offers an unrivalled level of integration and performances. All the stringent constraints of dynamic range optimization and power consumption reduction have been mastered with less than 1 watt detector dissipation. The Front-End Electronics Module (F2EM) encompasses all the functions to be implemented close to the detectors. Mounted inside the FPA (Focal Plane Assembly), it provides the detectors with all the necessary biasing and clocking signals and performs preamplification and transmission of the video signal to the MEV. The MEV (Module Electronique Video) is the backend part of the NAOMI detection electronics. The MEV provides the F2EM with the primary power supplies and clocks necessary to front-end operation. 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