Tabulations of some of the most frequently required information on individual Tiros satellites.
Tiros satellites characteristics including ESSA I
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Tiros satellites characteristics including ESSA I
Basic information on tiros satellite
Radiation data measured by Tiros IV satellite for determination of global distribution of atmospheric water vapor
Radiation data measured by Tiros IV satellite for determination of global distribution of atmospheric water vapor
Calibration of five channel tiros satellite radiometer
TIROS weather satellite launch - flight plan, configuration, vidicon television system, polar synchronous orbit, stabilization and control, and Delta launch vehicle
Surface features of southern Africa based on interpreted photographs taken by TIROS SATELLITES
Atmospheric properties based upon evaluation of infrared radiation data from TIROS III SATELLITE
Tiros VII measurements of 15 micron radiation emitted by carbon dioxide from which global maps of stratospheric temperatures are obtained
A procedure is described which works effectively to detect and locate emergency locating transmitters (ELTs) and emergency position indicating radio beacons (EPIRBs) in a multisignal environment. Using data generated from several manufactured ELTs with diverse superimposed Doppler curves, as many as 9 simultaneous ELTs can be detected and located at a variety of signal strengths. It is noted that average position errors of 10 km are attainable today at signal power to noise spectral density ratios as low as 17 dB-Hz.
TIROS satellite test data on spacecraft, launch vehicle, ground control, and data system
Cloud pattern classification, discrimination, and interpretation from photographs obtained by meteorological satellite - Tiros satellite
TIROS II contains instrumentation for measuring infrared and reflected solar radiation from the earth and its atmosphere. A medium resolution scanning radiometer and a low resolution non-scanning radiometer are employed. The satellite's spin provides the scan line of the medium resolution radiometer which is then advanced by the orbital motion. The spatial resolution is about 40 miles square when the earth directly beneath the satellite is viewed. The five channels employ bolometer detectors and filters to limit the spectral responses to five bands: 6 to 6.5 microns, 8 to 12 microns, 0.2 to 6 microns, 8 to 30 microns, and 0.55 to 0.75 microns. These five bands study, respectively: radiation in the water vapor absorption band; day and nighttime cloud cover; albedo; thermal radiation; and visual maps for comparison with satellite vidicon pictures. The low resolution non-scanning radiometer measures the earth's black-body temperature and albedo. Its field when viewing directly below is a circle of 450 miles diameter, covering part of each frame from the wide-field television camera. This radiometer consists of two thermistors, each in the apex of a reflective cone which provides optical gain. One thermistor is black and responds to both thermal and reflected solar radiation. The second responds to thermal but reflects solar radiation. The design, calibration, performance, and data reduction for both systems are discussed herein.
TIROS II, III, IV, and VII meteorological satellite radiation data availability
Tiros & nimbus meteorological satellite systems - data acquisition & recording