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: N. F. Arnold, T. B. Jones, T. R. Robinson, A. J. Stocker, J. A. Davies
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 1998
Subjects:
Q
Online Access:https://doi.org/10.1007/s00585-998-1392-z
https://doaj.org/article/02a6591397de46b387473766497cd765
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spelling ftdoajarticles:oai:doaj.org/article:02a6591397de46b387473766497cd765 2023-05-15T16:04:12+02:00 Validation of the CUTLASS HF radar gravity wave observing capability using EISCAT CP-1 data N. F. Arnold T. B. Jones T. R. Robinson A. J. Stocker J. A. Davies 1998-10-01T00:00:00Z https://doi.org/10.1007/s00585-998-1392-z https://doaj.org/article/02a6591397de46b387473766497cd765 EN eng Copernicus Publications https://www.ann-geophys.net/16/1392/1998/angeo-16-1392-1998.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.1007/s00585-998-1392-z 0992-7689 1432-0576 https://doaj.org/article/02a6591397de46b387473766497cd765 Annales Geophysicae, Vol 16, Pp 1392-1399 (1998) Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 article 1998 ftdoajarticles https://doi.org/10.1007/s00585-998-1392-z 2022-12-30T20:48:49Z 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) Article in Journal/Newspaper EISCAT Tromsø Directory of Open Access Journals: DOAJ Articles Tromsø Annales Geophysicae 16 10 1392 1399
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
spellingShingle Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
N. F. Arnold
T. B. Jones
T. R. Robinson
A. J. Stocker
J. A. Davies
Validation of the CUTLASS HF radar gravity wave observing capability using EISCAT CP-1 data
topic_facet Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
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 Article in Journal/Newspaper
author N. F. Arnold
T. B. Jones
T. R. Robinson
A. J. Stocker
J. A. Davies
author_facet N. F. Arnold
T. B. Jones
T. R. Robinson
A. J. Stocker
J. A. Davies
author_sort N. F. Arnold
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
publisher Copernicus Publications
publishDate 1998
url https://doi.org/10.1007/s00585-998-1392-z
https://doaj.org/article/02a6591397de46b387473766497cd765
geographic Tromsø
geographic_facet Tromsø
genre EISCAT
Tromsø
genre_facet EISCAT
Tromsø
op_source Annales Geophysicae, Vol 16, Pp 1392-1399 (1998)
op_relation https://www.ann-geophys.net/16/1392/1998/angeo-16-1392-1998.pdf
https://doaj.org/toc/0992-7689
https://doaj.org/toc/1432-0576
doi:10.1007/s00585-998-1392-z
0992-7689
1432-0576
https://doaj.org/article/02a6591397de46b387473766497cd765
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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