Self-consistent modelling of the daytime electron density profile in the ionospheric F region
A theoretical self-consistent method for the description of daytime N e (h) profiles in the ionospheric F region measured by EISCAT is proposed. It is based on the use of a theoretical F-region model and measured electron density, N e (h) , electron, T e (h) , and ion temperature, T i (h) , and fiel...
Published in: | Annales Geophysicae |
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ftcopernicus:oai:publications.copernicus.org:angeo33951 2023-05-15T16:04:32+02:00 Self-consistent modelling of the daytime electron density profile in the ionospheric F region Mikhailov, A. Schlegel, K. 2018-09-27 application/pdf https://doi.org/10.1007/s00585-997-0314-9 https://angeo.copernicus.org/articles/15/314/1997/ eng eng doi:10.1007/s00585-997-0314-9 https://angeo.copernicus.org/articles/15/314/1997/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.1007/s00585-997-0314-9 2020-07-20T16:28:09Z A theoretical self-consistent method for the description of daytime N e (h) profiles in the ionospheric F region measured by EISCAT is proposed. It is based on the use of a theoretical F-region model and measured electron density, N e (h) , electron, T e (h) , and ion temperature, T i (h) , and field-aligned plasma drift V l (h) profiles. The method describes the observed N e (h) profile with high accuracy for quiet and disturbed conditions. Two versions of the method are considered: in the first the exospheric temperature T ex is derived from a procedure minimizing [log( N e (h) obs / N e (h) cal ] 2 , in the second T ex is deduced from the ion energy conservation in the F region. The method allows us to infer from the incoherent-scatter observations: concentrations of atomic oxygen, [O], molecular oxygen, [O 2 ], molecular nitrogen, [N 2 ] the vertical plasma drift, W , the exospheric temperature. T ex , and the shape parameter S in the neutral temperature profile. The ratio ([O + ]/ N e ) calculated by the theoretical model is used to correct T e (h), T i (h) and N e (h) profiles routinely measured with EISCAT which are known to depend strongly on the actual applied ion-composition model. Such a correction is especially important for geomagnetically disturbed periods when the F region is strongly enriched with molecular ions. We conclude that four of the six thermospheric parameters, namely [O], [N 2 ], W and T ex can be confidently inferred from the EISCAT observations, while the other two derived parameters, [O 2 ] ans S are less reliable. The method can be used for the analysis of long-term (seasonal, solar cycle) as well as for day-to-day variations of the thermospheric parameters and the F-region ion composition using daytime incoherent-scatter observations. Text EISCAT Copernicus Publications: E-Journals Annales Geophysicae 15 3 314 326 |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
A theoretical self-consistent method for the description of daytime N e (h) profiles in the ionospheric F region measured by EISCAT is proposed. It is based on the use of a theoretical F-region model and measured electron density, N e (h) , electron, T e (h) , and ion temperature, T i (h) , and field-aligned plasma drift V l (h) profiles. The method describes the observed N e (h) profile with high accuracy for quiet and disturbed conditions. Two versions of the method are considered: in the first the exospheric temperature T ex is derived from a procedure minimizing [log( N e (h) obs / N e (h) cal ] 2 , in the second T ex is deduced from the ion energy conservation in the F region. The method allows us to infer from the incoherent-scatter observations: concentrations of atomic oxygen, [O], molecular oxygen, [O 2 ], molecular nitrogen, [N 2 ] the vertical plasma drift, W , the exospheric temperature. T ex , and the shape parameter S in the neutral temperature profile. The ratio ([O + ]/ N e ) calculated by the theoretical model is used to correct T e (h), T i (h) and N e (h) profiles routinely measured with EISCAT which are known to depend strongly on the actual applied ion-composition model. Such a correction is especially important for geomagnetically disturbed periods when the F region is strongly enriched with molecular ions. We conclude that four of the six thermospheric parameters, namely [O], [N 2 ], W and T ex can be confidently inferred from the EISCAT observations, while the other two derived parameters, [O 2 ] ans S are less reliable. The method can be used for the analysis of long-term (seasonal, solar cycle) as well as for day-to-day variations of the thermospheric parameters and the F-region ion composition using daytime incoherent-scatter observations. |
format |
Text |
author |
Mikhailov, A. Schlegel, K. |
spellingShingle |
Mikhailov, A. Schlegel, K. Self-consistent modelling of the daytime electron density profile in the ionospheric F region |
author_facet |
Mikhailov, A. Schlegel, K. |
author_sort |
Mikhailov, A. |
title |
Self-consistent modelling of the daytime electron density profile in the ionospheric F region |
title_short |
Self-consistent modelling of the daytime electron density profile in the ionospheric F region |
title_full |
Self-consistent modelling of the daytime electron density profile in the ionospheric F region |
title_fullStr |
Self-consistent modelling of the daytime electron density profile in the ionospheric F region |
title_full_unstemmed |
Self-consistent modelling of the daytime electron density profile in the ionospheric F region |
title_sort |
self-consistent modelling of the daytime electron density profile in the ionospheric f region |
publishDate |
2018 |
url |
https://doi.org/10.1007/s00585-997-0314-9 https://angeo.copernicus.org/articles/15/314/1997/ |
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EISCAT |
genre_facet |
EISCAT |
op_source |
eISSN: 1432-0576 |
op_relation |
doi:10.1007/s00585-997-0314-9 https://angeo.copernicus.org/articles/15/314/1997/ |
op_doi |
https://doi.org/10.1007/s00585-997-0314-9 |
container_title |
Annales Geophysicae |
container_volume |
15 |
container_issue |
3 |
container_start_page |
314 |
op_container_end_page |
326 |
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1766400126114332672 |