The role of electric field and neutral wind in the generation of polar cap sporadic E

This paper investigates the roles of electric field and neutral wind in the generation of sporadic-E layers within the polar cap. Two Es layers above Svalbard, observed by the EISCAT Svalbard Radar (ESR), were chosen for investigation. The radar experiment contains four beam directions, and this was...

Full description

Bibliographic Details
Published in:Annales Geophysicae
Main Authors: Nygrén, T., Voiculescu, M., Aikio, A. T.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/angeo-26-3757-2008
https://angeo.copernicus.org/articles/26/3757/2008/
id ftcopernicus:oai:publications.copernicus.org:angeo36608
record_format openpolar
spelling ftcopernicus:oai:publications.copernicus.org:angeo36608 2023-05-15T16:04:43+02:00 The role of electric field and neutral wind in the generation of polar cap sporadic E Nygrén, T. Voiculescu, M. Aikio, A. T. 2018-09-27 application/pdf https://doi.org/10.5194/angeo-26-3757-2008 https://angeo.copernicus.org/articles/26/3757/2008/ eng eng doi:10.5194/angeo-26-3757-2008 https://angeo.copernicus.org/articles/26/3757/2008/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.5194/angeo-26-3757-2008 2020-07-20T16:26:47Z This paper investigates the roles of electric field and neutral wind in the generation of sporadic-E layers within the polar cap. Two Es layers above Svalbard, observed by the EISCAT Svalbard Radar (ESR), were chosen for investigation. The radar experiment contains four beam directions, and this was used for determining the electric field. The neutral wind was obtained from the HWM93 model. Formation of Es layers was calculated by integrating the continuity equation under the action of driving forces due to neutral wind and electric field. A flat height profile of metal ions was assumed in the beginning. The calculation gives the time variation of the layer, which can be compared with observations. In one case the electric field was shown to be the main driving agent in layer generation. In the other case the electric field was weak and the layer was produced mainly by the neutral wind, but the electric field had influence on the height of the layer. A fairly good agreement between the variations of the observed and calculated layer altitudes was obtained and some agreement between the intensity variations was also found. Text EISCAT Svalbard Copernicus Publications: E-Journals Svalbard Annales Geophysicae 26 12 3757 3763
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description This paper investigates the roles of electric field and neutral wind in the generation of sporadic-E layers within the polar cap. Two Es layers above Svalbard, observed by the EISCAT Svalbard Radar (ESR), were chosen for investigation. The radar experiment contains four beam directions, and this was used for determining the electric field. The neutral wind was obtained from the HWM93 model. Formation of Es layers was calculated by integrating the continuity equation under the action of driving forces due to neutral wind and electric field. A flat height profile of metal ions was assumed in the beginning. The calculation gives the time variation of the layer, which can be compared with observations. In one case the electric field was shown to be the main driving agent in layer generation. In the other case the electric field was weak and the layer was produced mainly by the neutral wind, but the electric field had influence on the height of the layer. A fairly good agreement between the variations of the observed and calculated layer altitudes was obtained and some agreement between the intensity variations was also found.
format Text
author Nygrén, T.
Voiculescu, M.
Aikio, A. T.
spellingShingle Nygrén, T.
Voiculescu, M.
Aikio, A. T.
The role of electric field and neutral wind in the generation of polar cap sporadic E
author_facet Nygrén, T.
Voiculescu, M.
Aikio, A. T.
author_sort Nygrén, T.
title The role of electric field and neutral wind in the generation of polar cap sporadic E
title_short The role of electric field and neutral wind in the generation of polar cap sporadic E
title_full The role of electric field and neutral wind in the generation of polar cap sporadic E
title_fullStr The role of electric field and neutral wind in the generation of polar cap sporadic E
title_full_unstemmed The role of electric field and neutral wind in the generation of polar cap sporadic E
title_sort role of electric field and neutral wind in the generation of polar cap sporadic e
publishDate 2018
url https://doi.org/10.5194/angeo-26-3757-2008
https://angeo.copernicus.org/articles/26/3757/2008/
geographic Svalbard
geographic_facet Svalbard
genre EISCAT
Svalbard
genre_facet EISCAT
Svalbard
op_source eISSN: 1432-0576
op_relation doi:10.5194/angeo-26-3757-2008
https://angeo.copernicus.org/articles/26/3757/2008/
op_doi https://doi.org/10.5194/angeo-26-3757-2008
container_title Annales Geophysicae
container_volume 26
container_issue 12
container_start_page 3757
op_container_end_page 3763
_version_ 1766400342840311808