Assessing the contamination of SuperDARN global convection maps by non-F-region backscatter

Global convection mapping using line-of-sight Doppler velocity data from the Super Dual Auroral Radar Network (SuperDARN) is now an accepted method of imaging high-latitude ionospheric convection. This mapping process requires that the flow measured by the radars is defined solely by the con...

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Main Authors: G. Chisham, M. Pinnock
Format: Article
Language:English
Published: Copernicus Publications 2002-01-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/20/13/2002/angeo-20-13-2002.pdf
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spelling doaj-1d5b3786e092434780e5cddafd8b688f2020-11-24T22:02:44ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762002-01-0120132810.5194/angeo-20-13-2002Assessing the contamination of SuperDARN global convection maps by non-F-region backscatterG. Chisham0G. Chisham1M. Pinnock2M. Pinnock3Correspondence to: G. Chisham (G.Chisham@bas.ac.uk)British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge, CB3 0ET, UKCorrespondence to: G. Chisham (G.Chisham@bas.ac.uk)British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge, CB3 0ET, UKGlobal convection mapping using line-of-sight Doppler velocity data from the Super Dual Auroral Radar Network (SuperDARN) is now an accepted method of imaging high-latitude ionospheric convection. This mapping process requires that the flow measured by the radars is defined solely by the convection electric field. This is generally only true of radar backscatter from the ionospheric F-region. We investigate the extent to which the E-region and ground backscatter in the SuperDARN data set may be misidentified as F-region backscatter, and assess the contamination of global convection maps which results from the addition of this non-F-region backscatter. We present examples which highlight the importance of identifying this contamination, especially with regard to the mesoscale structure in the convection maps.<br><br><b>Key words. </b>Ionosphere (plasma convection) – Radio science (radio wave propagation; instruments and techniques)https://www.ann-geophys.net/20/13/2002/angeo-20-13-2002.pdf
collection DOAJ
language English
format Article
sources DOAJ
author G. Chisham
G. Chisham
M. Pinnock
M. Pinnock
spellingShingle G. Chisham
G. Chisham
M. Pinnock
M. Pinnock
Assessing the contamination of SuperDARN global convection maps by non-F-region backscatter
Annales Geophysicae
author_facet G. Chisham
G. Chisham
M. Pinnock
M. Pinnock
author_sort G. Chisham
title Assessing the contamination of SuperDARN global convection maps by non-F-region backscatter
title_short Assessing the contamination of SuperDARN global convection maps by non-F-region backscatter
title_full Assessing the contamination of SuperDARN global convection maps by non-F-region backscatter
title_fullStr Assessing the contamination of SuperDARN global convection maps by non-F-region backscatter
title_full_unstemmed Assessing the contamination of SuperDARN global convection maps by non-F-region backscatter
title_sort assessing the contamination of superdarn global convection maps by non-f-region backscatter
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2002-01-01
description Global convection mapping using line-of-sight Doppler velocity data from the Super Dual Auroral Radar Network (SuperDARN) is now an accepted method of imaging high-latitude ionospheric convection. This mapping process requires that the flow measured by the radars is defined solely by the convection electric field. This is generally only true of radar backscatter from the ionospheric F-region. We investigate the extent to which the E-region and ground backscatter in the SuperDARN data set may be misidentified as F-region backscatter, and assess the contamination of global convection maps which results from the addition of this non-F-region backscatter. We present examples which highlight the importance of identifying this contamination, especially with regard to the mesoscale structure in the convection maps.<br><br><b>Key words. </b>Ionosphere (plasma convection) – Radio science (radio wave propagation; instruments and techniques)
url https://www.ann-geophys.net/20/13/2002/angeo-20-13-2002.pdf
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