Simultaneous HF measurements of E- and F-region Doppler velocities at large flow angles

Data collected by the CUTLASS Finland HF radar are used to illustrate the significant difference between the cosine component of the plasma convection in the F-region and the Doppler velocity of the E-region coherent echoes observed at large flow angles. We show that the E-region velocity is ~5...

Full description

Bibliographic Details
Main Authors: R. A. Makarevitch, F. Honary, A. V. Koustov
Format: Article
Language:English
Published: Copernicus Publications 2004-04-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/22/1177/2004/angeo-22-1177-2004.pdf
id doaj-da45dbd05f2040ef9dceb097e1826417
record_format Article
spelling doaj-da45dbd05f2040ef9dceb097e18264172020-11-24T21:30:08ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762004-04-01221177118510.5194/angeo-22-1177-2004Simultaneous HF measurements of E- and F-region Doppler velocities at large flow anglesR. A. Makarevitch0F. Honary1A. V. Koustov2Department of Communication Systems, Lancaster University, Lancaster, LA1 4YR, UKDepartment of Communication Systems, Lancaster University, Lancaster, LA1 4YR, UKInstitute of Space and Atmospheric Sciences, University of Saskatchewan, 116 Science Place, Saskatoon, SK, S7N 5E2, CanadaData collected by the CUTLASS Finland HF radar are used to illustrate the significant difference between the cosine component of the plasma convection in the F-region and the Doppler velocity of the E-region coherent echoes observed at large flow angles. We show that the E-region velocity is ~5 times smaller in magnitude and rotated by ~30° clockwise with respect to convection in the F-region. Also, measurements at flow angles larger than 90° exhibit a completely new feature: Doppler velocity increase with the expected aspect angle and spatial anticorrelation with the backscatter power. By considering DMSP drift-meter measurements we argue that the difference between F- and E-region velocities cannot be interpreted in terms of the convection change with latitude. The observed features in the velocity of the E-region echoes can be explained by taking into account the ion drift contribution to the irregularity phase velocity as predicted by the linear fluid theory.<br><br> <b>Key words.</b> Ionosphere (auroral ionosphere; ionospheric irregularities; plasma convection)https://www.ann-geophys.net/22/1177/2004/angeo-22-1177-2004.pdf
collection DOAJ
language English
format Article
sources DOAJ
author R. A. Makarevitch
F. Honary
A. V. Koustov
spellingShingle R. A. Makarevitch
F. Honary
A. V. Koustov
Simultaneous HF measurements of E- and F-region Doppler velocities at large flow angles
Annales Geophysicae
author_facet R. A. Makarevitch
F. Honary
A. V. Koustov
author_sort R. A. Makarevitch
title Simultaneous HF measurements of E- and F-region Doppler velocities at large flow angles
title_short Simultaneous HF measurements of E- and F-region Doppler velocities at large flow angles
title_full Simultaneous HF measurements of E- and F-region Doppler velocities at large flow angles
title_fullStr Simultaneous HF measurements of E- and F-region Doppler velocities at large flow angles
title_full_unstemmed Simultaneous HF measurements of E- and F-region Doppler velocities at large flow angles
title_sort simultaneous hf measurements of e- and f-region doppler velocities at large flow angles
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2004-04-01
description Data collected by the CUTLASS Finland HF radar are used to illustrate the significant difference between the cosine component of the plasma convection in the F-region and the Doppler velocity of the E-region coherent echoes observed at large flow angles. We show that the E-region velocity is ~5 times smaller in magnitude and rotated by ~30° clockwise with respect to convection in the F-region. Also, measurements at flow angles larger than 90° exhibit a completely new feature: Doppler velocity increase with the expected aspect angle and spatial anticorrelation with the backscatter power. By considering DMSP drift-meter measurements we argue that the difference between F- and E-region velocities cannot be interpreted in terms of the convection change with latitude. The observed features in the velocity of the E-region echoes can be explained by taking into account the ion drift contribution to the irregularity phase velocity as predicted by the linear fluid theory.<br><br> <b>Key words.</b> Ionosphere (auroral ionosphere; ionospheric irregularities; plasma convection)
url https://www.ann-geophys.net/22/1177/2004/angeo-22-1177-2004.pdf
work_keys_str_mv AT ramakarevitch simultaneoushfmeasurementsofeandfregiondopplervelocitiesatlargeflowangles
AT fhonary simultaneoushfmeasurementsofeandfregiondopplervelocitiesatlargeflowangles
AT avkoustov simultaneoushfmeasurementsofeandfregiondopplervelocitiesatlargeflowangles
_version_ 1725963738855505920