The influence of ground track constraints upon orbit requirements for sun synchronous satellites
Equations derived for analyzing ground track of sun synchronous satellite and applied to Earth Resources Satellite
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Equations derived for analyzing ground track of sun synchronous satellite and applied to Earth Resources Satellite
Energy dissipation associated with physical librations of large synchronous satellites may be important for maintaining internal fluid layers. Depending on the depth and viscosity of the fluid layer, viscous heating from librations may exceeed that from tides.
Orbital regression of synchronous satellites due to combined gravitational effects of sun, moon, and oblate earth
Low cost TV ground receiving systems for signals transmitted from synchronous satellites, describing reception techniques, manufacturing and performance characteristics
The AQUA, SNPP, and NOAA 18-20 PM sun-synchronous satellites were designed with similar local time, local solarzenith angles, and overlapping temporal coverage. Although the satellites are expected to have fixed local equator-crossing time, during the satellite lifetime, the equator-crossing times of these satellites drift. For NOAA 18-19, the driftin equator-crossing time is significant (few hours) and no correction has been done over the lifetime. For SNPP andAQUA, correction in the orbital inclination angle was periodically performed to maintain the equator-crossing timearound the designed value. The impact of systematic drift of the local observation time during the satellite life cycle canbe significant and should be accounted for when using multi-year time series of satellite products in long-termenvironmental studies. In this paper, the equator-crossing time drift of AQUA, SNPP, and NOAA 18-20, the correctionof SNPP and AQUA equator-crossing time via orbital inclination angle change, and the consequent local solar zenithangle variation are evaluated. The impact of such drift on low-latitude mean brightness temperature trend derived fromthe similar ~11 μm thermal emissive channel of AQUA MODIS CH31, SNPP Visible Infrared Imaging RadiometerSuite (VIIRS) CH15 and NOAA 18-19 HIRS CH08 are analyzed. The drift in the mean brightness temperature measuredby these sensors is combined as a function of local time and analyzed using diurnal cycle analysis. The mean brightnesstemperature drift for SNPP VIIRS is reconciled within the context of much larger temperature drift of NOAA 18-19.
Satellite drift maxima from synchronous inclined circular orbit due to perturbations
Design, fabrication, and testing of antenna for ATS F and G synchronous satellites
Scintillation, polarization, and multipath effects on VHF propagation between synchronous satellites and aircraft - telecommunication systems
Solar phenomena effect on VHF communications between synchronous satellite relay and earth ground stations
Gravitational red shift measurement using synchronous satellite, argon laser and Fabry- Perot interferometer
Bidirectional reflectance of earth atmosphere and cloud formation above equatorial Pacific observed by synchronous satellite as function of angular dependence
Sea surface slope distribution and wind velocity determination by sun glitter photography from synchronous satellite
Solar flare and sunspot effects on VHF communications between synchronous satellite relay and ground stations
Laser propagation experiments between stabilized synchronous satellites and ground stations at visible and near-infrared wavelengths
An apparent early recovery of the main phase of geomagnetic storms at the distance of the synchronous satellite is examined in terms of changing electric current distributions in the magnetosphere during magnetic storms. It is suggested that a rapid recession of the edge of the plasma sheet (after the advance toward the earth during an early epoch of the main phase) is partly responsible for the early recovery. Relevant plasma sheet variations during geomagnetic storms are found to be in agreement with the inferred variations.
Satellite orbit adjustment, stationkeeping and attitude control of typical earth- and sun- synchronous satellites by electric propulsion systems
Spin phase synchronization of cartwheel satellite in polar orbit
Zenith and azimuthal angles of measurement dependence on reflection properties of earth atmosphere determined from synchronous satellite data