Thermospheric Winds and Their Influence on the Ionosphere: (Review)
Gespeichert in:
1. Verfasser: | |
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Format: | Elektronisch E-Book |
Sprache: | English |
Veröffentlicht: |
Berlin, Heidelberg
Springer Berlin Heidelberg
1974
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Schriftenreihe: | Mitteilungen aus dem Max-Planck-Institut für Aeronomie
53 |
Schlagworte: | |
Online-Zugang: | Volltext |
Beschreibung: | It is well known that thermospheric winds play an important role in the dynamics of the upper atmo sphere and are of major importance for the behaviour of the ionosphere. The methods of calculating these winds are discussed briefly. Comparisons of the calculated winds with observational data are carried out. Some main effects of the winds on the dynamical behaviour of the ionized as well as neutral part of the upper atmosphere are discussed. 2. Calculation of thermospheric winds The system of equations describing the dynamical behaviour of the thermosphere and the ionosphere consists of: b a neutral atmosphere ionosphere continuity equations continuity equations for different ion species and electrons equations of motion (winds) equations of motion for the different constituents (ambi polar diffusion, wind induced drifts, ~ x ~ -drifts) energy balance equations energy balance equations Due to collisions between charged and neutral particles there is an interaction between the ionized and neutral gas. Both sets of equations are coupled, therefore, by the respective drag terms. Because of the complexity of the mathematics involved in solving all equations simultaneously, different approaches have been made to solve parts of this system of differential equations under additional assumptions and restrictions. There are two general approaches: a. ) Solution of the equation of motion of the neutral atmosphere together with the ionospheric continuity equations and equations of motion of the ions |
Beschreibung: | 1 Online-Ressource (27 p) |
ISBN: | 9783642660405 9783540070702 |
DOI: | 10.1007/978-3-642-66040-5 |
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245 | 1 | 0 | |a Thermospheric Winds and Their Influence on the Ionosphere |b (Review) |c by R. Rüster |
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490 | 0 | |a Mitteilungen aus dem Max-Planck-Institut für Aeronomie |v 53 | |
500 | |a It is well known that thermospheric winds play an important role in the dynamics of the upper atmo sphere and are of major importance for the behaviour of the ionosphere. The methods of calculating these winds are discussed briefly. Comparisons of the calculated winds with observational data are carried out. Some main effects of the winds on the dynamical behaviour of the ionized as well as neutral part of the upper atmosphere are discussed. 2. Calculation of thermospheric winds The system of equations describing the dynamical behaviour of the thermosphere and the ionosphere consists of: b a neutral atmosphere ionosphere continuity equations continuity equations for different ion species and electrons equations of motion (winds) equations of motion for the different constituents (ambi polar diffusion, wind induced drifts, ~ x ~ -drifts) energy balance equations energy balance equations Due to collisions between charged and neutral particles there is an interaction between the ionized and neutral gas. Both sets of equations are coupled, therefore, by the respective drag terms. Because of the complexity of the mathematics involved in solving all equations simultaneously, different approaches have been made to solve parts of this system of differential equations under additional assumptions and restrictions. There are two general approaches: a. ) Solution of the equation of motion of the neutral atmosphere together with the ionospheric continuity equations and equations of motion of the ions | ||
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Datensatz im Suchindex
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any_adam_object | |
author | Rüster, R. |
author_facet | Rüster, R. |
author_role | aut |
author_sort | Rüster, R. |
author_variant | r r rr |
building | Verbundindex |
bvnumber | BV042413385 |
classification_tum | PHY 000 |
collection | ZDB-2-PHA ZDB-2-BAE |
ctrlnum | (OCoLC)863893157 (DE-599)BVBBV042413385 |
dewey-full | 550 |
dewey-hundreds | 500 - Natural sciences and mathematics |
dewey-ones | 550 - Earth sciences |
dewey-raw | 550 |
dewey-search | 550 |
dewey-sort | 3550 |
dewey-tens | 550 - Earth sciences |
discipline | Geologie / Paläontologie Physik |
doi_str_mv | 10.1007/978-3-642-66040-5 |
format | Electronic eBook |
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id | DE-604.BV042413385 |
illustrated | Not Illustrated |
indexdate | 2024-07-10T01:20:52Z |
institution | BVB |
isbn | 9783642660405 9783540070702 |
language | English |
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publishDate | 1974 |
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publisher | Springer Berlin Heidelberg |
record_format | marc |
series2 | Mitteilungen aus dem Max-Planck-Institut für Aeronomie |
spelling | Rüster, R. Verfasser aut Thermospheric Winds and Their Influence on the Ionosphere (Review) by R. Rüster Berlin, Heidelberg Springer Berlin Heidelberg 1974 1 Online-Ressource (27 p) txt rdacontent c rdamedia cr rdacarrier Mitteilungen aus dem Max-Planck-Institut für Aeronomie 53 It is well known that thermospheric winds play an important role in the dynamics of the upper atmo sphere and are of major importance for the behaviour of the ionosphere. The methods of calculating these winds are discussed briefly. Comparisons of the calculated winds with observational data are carried out. Some main effects of the winds on the dynamical behaviour of the ionized as well as neutral part of the upper atmosphere are discussed. 2. Calculation of thermospheric winds The system of equations describing the dynamical behaviour of the thermosphere and the ionosphere consists of: b a neutral atmosphere ionosphere continuity equations continuity equations for different ion species and electrons equations of motion (winds) equations of motion for the different constituents (ambi polar diffusion, wind induced drifts, ~ x ~ -drifts) energy balance equations energy balance equations Due to collisions between charged and neutral particles there is an interaction between the ionized and neutral gas. Both sets of equations are coupled, therefore, by the respective drag terms. Because of the complexity of the mathematics involved in solving all equations simultaneously, different approaches have been made to solve parts of this system of differential equations under additional assumptions and restrictions. There are two general approaches: a. ) Solution of the equation of motion of the neutral atmosphere together with the ionospheric continuity equations and equations of motion of the ions Geography Physics Earth Sciences Earth Sciences, general Physics, general Geografie Geowissenschaften Ionosphäre (DE-588)4130409-3 gnd rswk-swf Ionosphäre (DE-588)4130409-3 s 1\p DE-604 https://doi.org/10.1007/978-3-642-66040-5 Verlag Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
spellingShingle | Rüster, R. Thermospheric Winds and Their Influence on the Ionosphere (Review) Geography Physics Earth Sciences Earth Sciences, general Physics, general Geografie Geowissenschaften Ionosphäre (DE-588)4130409-3 gnd |
subject_GND | (DE-588)4130409-3 |
title | Thermospheric Winds and Their Influence on the Ionosphere (Review) |
title_auth | Thermospheric Winds and Their Influence on the Ionosphere (Review) |
title_exact_search | Thermospheric Winds and Their Influence on the Ionosphere (Review) |
title_full | Thermospheric Winds and Their Influence on the Ionosphere (Review) by R. Rüster |
title_fullStr | Thermospheric Winds and Their Influence on the Ionosphere (Review) by R. Rüster |
title_full_unstemmed | Thermospheric Winds and Their Influence on the Ionosphere (Review) by R. Rüster |
title_short | Thermospheric Winds and Their Influence on the Ionosphere |
title_sort | thermospheric winds and their influence on the ionosphere review |
title_sub | (Review) |
topic | Geography Physics Earth Sciences Earth Sciences, general Physics, general Geografie Geowissenschaften Ionosphäre (DE-588)4130409-3 gnd |
topic_facet | Geography Physics Earth Sciences Earth Sciences, general Physics, general Geografie Geowissenschaften Ionosphäre |
url | https://doi.org/10.1007/978-3-642-66040-5 |
work_keys_str_mv | AT rusterr thermosphericwindsandtheirinfluenceontheionospherereview |