Thermospheric Density and Wind Determination from Satellite Dynamics

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 vel...

Πλήρης περιγραφή

Λεπτομέρειες βιβλιογραφικής εγγραφής
Κύριος συγγραφέας: Doornbos, Eelco (Συγγραφέας)
Συγγραφή απο Οργανισμό/Αρχή: SpringerLink (Online service)
Μορφή: Ηλεκτρονική πηγή Ηλ. βιβλίο
Γλώσσα:English
Έκδοση: Berlin, Heidelberg : Springer Berlin Heidelberg : Imprint: Springer, 2012.
Σειρά:Springer Theses,
Θέματα:
Διαθέσιμο Online:Full Text via HEAL-Link
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001 978-3-642-25129-0
003 DE-He213
005 20151029211909.0
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020 |a 9783642251290  |9 978-3-642-25129-0 
024 7 |a 10.1007/978-3-642-25129-0  |2 doi 
040 |d GrThAP 
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072 7 |a SCI042000  |2 bisacsh 
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100 1 |a Doornbos, Eelco.  |e author. 
245 1 0 |a Thermospheric Density and Wind Determination from Satellite Dynamics  |h [electronic resource] /  |c by Eelco Doornbos. 
264 1 |a Berlin, Heidelberg :  |b Springer Berlin Heidelberg :  |b Imprint: Springer,  |c 2012. 
300 |a XVI, 184 p.  |b online resource. 
336 |a text  |b txt  |2 rdacontent 
337 |a computer  |b c  |2 rdamedia 
338 |a online resource  |b cr  |2 rdacarrier 
347 |a text file  |b PDF  |2 rda 
490 1 |a Springer Theses,  |x 2190-5053 
505 0 |a Empirical modelling of the thermosphere -- Satellite dynamics and non-gravitational force modelling -- Producing density and crosswind from satellite dynamics observations -- Analysis and interpretation of density and wind data -- Empirical model calibration -- Conclusions and recommendations. 
520 |a 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. 
650 0 |a Earth sciences. 
650 0 |a Atmospheric sciences. 
650 0 |a Fluids. 
650 0 |a Aerospace engineering. 
650 0 |a Astronautics. 
650 1 4 |a Earth Sciences. 
650 2 4 |a Atmospheric Sciences. 
650 2 4 |a Aerospace Technology and Astronautics. 
650 2 4 |a Fluid- and Aerodynamics. 
710 2 |a SpringerLink (Online service) 
773 0 |t Springer eBooks 
776 0 8 |i Printed edition:  |z 9783642251283 
830 0 |a Springer Theses,  |x 2190-5053 
856 4 0 |u http://dx.doi.org/10.1007/978-3-642-25129-0  |z Full Text via HEAL-Link 
912 |a ZDB-2-EES 
950 |a Earth and Environmental Science (Springer-11646)