Cargando…

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...

Descripción completa

Detalles Bibliográficos
Clasificación:Libro Electrónico
Autor principal: Doornbos, Eelco (Autor)
Autor Corporativo: SpringerLink (Online service)
Formato: Electrónico eBook
Idioma:Inglés
Publicado: Berlin, Heidelberg : Springer Berlin Heidelberg : Imprint: Springer, 2012.
Edición:1st ed. 2012.
Colección:Springer Theses, Recognizing Outstanding Ph.D. Research,
Temas:
Acceso en línea:Texto Completo

MARC

LEADER 00000nam a22000005i 4500
001 978-3-642-25129-0
003 DE-He213
005 20220114235348.0
007 cr nn 008mamaa
008 120117s2012 gw | s |||| 0|eng d
020 |a 9783642251290  |9 978-3-642-25129-0 
024 7 |a 10.1007/978-3-642-25129-0  |2 doi 
050 4 |a QC851-999 
072 7 |a RBP  |2 bicssc 
072 7 |a SCI042000  |2 bisacsh 
072 7 |a RBP  |2 thema 
082 0 4 |a 551.5  |2 23 
100 1 |a Doornbos, Eelco.  |e author.  |4 aut  |4 http://id.loc.gov/vocabulary/relators/aut 
245 1 0 |a Thermospheric Density and Wind Determination from Satellite Dynamics  |h [electronic resource] /  |c by Eelco Doornbos. 
250 |a 1st ed. 2012. 
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, Recognizing Outstanding Ph.D. Research,  |x 2190-5061 
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 Atmospheric science. 
650 0 |a Aerospace engineering. 
650 0 |a Astronautics. 
650 0 |a Continuum mechanics. 
650 1 4 |a Atmospheric Science. 
650 2 4 |a Aerospace Technology and Astronautics. 
650 2 4 |a Continuum Mechanics. 
710 2 |a SpringerLink (Online service) 
773 0 |t Springer Nature eBook 
776 0 8 |i Printed edition:  |z 9783642442643 
776 0 8 |i Printed edition:  |z 9783642251306 
776 0 8 |i Printed edition:  |z 9783642251283 
830 0 |a Springer Theses, Recognizing Outstanding Ph.D. Research,  |x 2190-5061 
856 4 0 |u https://doi.uam.elogim.com/10.1007/978-3-642-25129-0  |z Texto Completo 
912 |a ZDB-2-EES 
912 |a ZDB-2-SXEE 
950 |a Earth and Environmental Science (SpringerNature-11646) 
950 |a Earth and Environmental Science (R0) (SpringerNature-43711)