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The Earth's atmosphere is often portrayed as a thin and finite blanket covering our planet, separate from the emptiness of outer space. In reality, the transition is gradual and a tiny fraction of the atmophere gases is still present at the altitude of low orbiting satellites. The very high velocities of these satellites ensure that their orbital motion can still be considerably affected by air density and wind. This influence can be measured using accelerometers and satellite tracking techniques. The opening chapters of this thesis provide an excellent introduction to the various disciplines that are involved in the interpretation of these observations: orbital mechanics, satellite aerodynamics and upper atmospheric physics. A subsequent chapter, at the heart of this work, covers advances in the algorithms used for processing satellite accelerometry and Two-Line Element (TLE) orbit data. The closing chapters provide an elaborate analysis of the resulting density and wind products, which are generating many opportunities for further research, to improve the modelling and understanding of the thermosphere system and its interactions with the lower atmosphere, the ionosphere-magnetosphere system and the Sun.
Artificial satellites -- Dynamics. --- Artificial satellites -- Orbits. --- Astronautics. --- Geography. --- Satellites. --- Thermospheric winds. --- Artificial satellites --- Thermospheric winds --- Satellites --- Mechanical Engineering --- Earth & Environmental Sciences --- Engineering & Applied Sciences --- Meteorology & Climatology --- Aeronautics Engineering & Astronautics --- Dynamics --- Orbits --- Thermosphere. --- Moons --- Natural satellites --- Planetary satellites --- Planets --- Thermosphere --- Winds --- Earth sciences. --- Atmospheric sciences. --- Fluids. --- Aerospace engineering. --- Earth Sciences. --- Atmospheric Sciences. --- Aerospace Technology and Astronautics. --- Fluid- and Aerodynamics. --- Atmosphere, Upper --- Upper atmosphere --- Space sciences --- Aeronautics --- Astrodynamics --- Space flight --- Space vehicles --- Hydraulics --- Mechanics --- Physics --- Hydrostatics --- Permeability --- Aeronautical engineering --- Astronautics --- Engineering --- Atmospheric sciences --- Earth sciences --- Atmosphere
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Space research --- Astrophysics --- Fluid mechanics --- vloeistofstroming --- astrofysica --- aerodynamica --- astronauten --- ruimtevaart
Choose an application
The Earth's atmosphere is often portrayed as a thin and finite blanket covering our planet, separate from the emptiness of outer space. In reality, the transition is gradual and a tiny fraction of the atmophere gases is still present at the altitude of low orbiting satellites. The very high velocities of these satellites ensure that their orbital motion can still be considerably affected by air density and wind. This influence can be measured using accelerometers and satellite tracking techniques. The opening chapters of this thesis provide an excellent introduction to the various disciplines that are involved in the interpretation of these observations: orbital mechanics, satellite aerodynamics and upper atmospheric physics. A subsequent chapter, at the heart of this work, covers advances in the algorithms used for processing satellite accelerometry and Two-Line Element (TLE) orbit data. The closing chapters provide an elaborate analysis of the resulting density and wind products, which are generating many opportunities for further research, to improve the modelling and understanding of the thermosphere system and its interactions with the lower atmosphere, the ionosphere-magnetosphere system and the Sun.
Space research --- Astrophysics --- Fluid mechanics --- vloeistofstroming --- astrofysica --- aerodynamica --- astronauten --- ruimtevaart
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