Validation of the CUTLASS HF radar gravity wave observing capability using EISCAT CP-1 data

Quasi-periodic fluctuations in the returned ground-scatter power from the SuperDARN HF radars have been linked to the passage of medium-scale gravity waves. We have applied a technique that extracts the first radar range returns from the F-region to study the spatial extent and characteristics of th...

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Published in:Annales Geophysicae
Main Authors: Arnold, N. F., Jones, T. B., Robinson, T. R., Stocker, A. J., Davies, J. A.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.1007/s00585-998-1392-z
https://angeo.copernicus.org/articles/16/1392/1998/
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spelling ftcopernicus:oai:publications.copernicus.org:angeo34234 2023-05-15T16:04:10+02:00 Validation of the CUTLASS HF radar gravity wave observing capability using EISCAT CP-1 data Arnold, N. F. Jones, T. B. Robinson, T. R. Stocker, A. J. Davies, J. A. 2018-09-27 application/pdf https://doi.org/10.1007/s00585-998-1392-z https://angeo.copernicus.org/articles/16/1392/1998/ eng eng doi:10.1007/s00585-998-1392-z https://angeo.copernicus.org/articles/16/1392/1998/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.1007/s00585-998-1392-z 2020-07-20T16:28:05Z Quasi-periodic fluctuations in the returned ground-scatter power from the SuperDARN HF radars have been linked to the passage of medium-scale gravity waves. We have applied a technique that extracts the first radar range returns from the F-region to study the spatial extent and characteristics of these waves in the CUTLASS field-of-view. Some ray tracing was carried out to test the applicability of this method. The EISCAT radar facility at Tromsø is well within the CUTLASS field-of-view for these waves and provides a unique opportunity to assess independently the ability of the HF radars to derive gravity wave information. Results from 1st March, 1995, where the EISCAT UHF radar was operating in its CP-1 mode, demonstrate that the radars were in good agreement, especially if one selects the electron density variations measured by EISCAT at around 235 km. CUTLASS and EISCAT gravity wave observations complement each other; the former extends the spatial field of view considerably, whilst the latter provides detailed vertical information about a range of ionospheric parameters. Key words. Ionosphere (ionosphere – atmosphere interactions) · Meteorology and atmospheric dynamics (thermospheric dynamics) · Radio science (ionospheric propagations) Text EISCAT Tromsø Copernicus Publications: E-Journals Tromsø Annales Geophysicae 16 10 1392 1399
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Quasi-periodic fluctuations in the returned ground-scatter power from the SuperDARN HF radars have been linked to the passage of medium-scale gravity waves. We have applied a technique that extracts the first radar range returns from the F-region to study the spatial extent and characteristics of these waves in the CUTLASS field-of-view. Some ray tracing was carried out to test the applicability of this method. The EISCAT radar facility at Tromsø is well within the CUTLASS field-of-view for these waves and provides a unique opportunity to assess independently the ability of the HF radars to derive gravity wave information. Results from 1st March, 1995, where the EISCAT UHF radar was operating in its CP-1 mode, demonstrate that the radars were in good agreement, especially if one selects the electron density variations measured by EISCAT at around 235 km. CUTLASS and EISCAT gravity wave observations complement each other; the former extends the spatial field of view considerably, whilst the latter provides detailed vertical information about a range of ionospheric parameters. Key words. Ionosphere (ionosphere – atmosphere interactions) · Meteorology and atmospheric dynamics (thermospheric dynamics) · Radio science (ionospheric propagations)
format Text
author Arnold, N. F.
Jones, T. B.
Robinson, T. R.
Stocker, A. J.
Davies, J. A.
spellingShingle Arnold, N. F.
Jones, T. B.
Robinson, T. R.
Stocker, A. J.
Davies, J. A.
Validation of the CUTLASS HF radar gravity wave observing capability using EISCAT CP-1 data
author_facet Arnold, N. F.
Jones, T. B.
Robinson, T. R.
Stocker, A. J.
Davies, J. A.
author_sort Arnold, N. F.
title Validation of the CUTLASS HF radar gravity wave observing capability using EISCAT CP-1 data
title_short Validation of the CUTLASS HF radar gravity wave observing capability using EISCAT CP-1 data
title_full Validation of the CUTLASS HF radar gravity wave observing capability using EISCAT CP-1 data
title_fullStr Validation of the CUTLASS HF radar gravity wave observing capability using EISCAT CP-1 data
title_full_unstemmed Validation of the CUTLASS HF radar gravity wave observing capability using EISCAT CP-1 data
title_sort validation of the cutlass hf radar gravity wave observing capability using eiscat cp-1 data
publishDate 2018
url https://doi.org/10.1007/s00585-998-1392-z
https://angeo.copernicus.org/articles/16/1392/1998/
geographic Tromsø
geographic_facet Tromsø
genre EISCAT
Tromsø
genre_facet EISCAT
Tromsø
op_source eISSN: 1432-0576
op_relation doi:10.1007/s00585-998-1392-z
https://angeo.copernicus.org/articles/16/1392/1998/
op_doi https://doi.org/10.1007/s00585-998-1392-z
container_title Annales Geophysicae
container_volume 16
container_issue 10
container_start_page 1392
op_container_end_page 1399
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