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 convection...
Ausführliche Beschreibung
Autor*in: |
G. Chisham [verfasserIn] M. Pinnock [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2002 |
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Übergeordnetes Werk: |
In: Annales Geophysicae - Copernicus Publications, 2002, 20(2002), Seite 13-28 |
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Übergeordnetes Werk: |
volume:20 ; year:2002 ; pages:13-28 |
Links: |
Link aufrufen |
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DOI / URN: |
10.5194/angeo-20-13-2002 |
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Katalog-ID: |
DOAJ078241596 |
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10.5194/angeo-20-13-2002 doi (DE-627)DOAJ078241596 (DE-599)DOAJ1d5b3786e092434780e5cddafd8b688f DE-627 ger DE-627 rakwb eng QC1-999 QC801-809 G. Chisham verfasserin aut Assessing the contamination of SuperDARN global convection maps by non-F-region backscatter 2002 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier 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) Science Q Physics Geophysics. Cosmic physics G. Chisham verfasserin aut M. Pinnock verfasserin aut M. Pinnock verfasserin aut In Annales Geophysicae Copernicus Publications, 2002 20(2002), Seite 13-28 (DE-627)25338981X (DE-600)1458425-6 14320576 nnns volume:20 year:2002 pages:13-28 https://doi.org/10.5194/angeo-20-13-2002 kostenfrei https://doaj.org/article/1d5b3786e092434780e5cddafd8b688f kostenfrei https://www.ann-geophys.net/20/13/2002/angeo-20-13-2002.pdf kostenfrei https://doaj.org/toc/0992-7689 Journal toc kostenfrei https://doaj.org/toc/1432-0576 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_2048 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 20 2002 13-28 |
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10.5194/angeo-20-13-2002 doi (DE-627)DOAJ078241596 (DE-599)DOAJ1d5b3786e092434780e5cddafd8b688f DE-627 ger DE-627 rakwb eng QC1-999 QC801-809 G. Chisham verfasserin aut Assessing the contamination of SuperDARN global convection maps by non-F-region backscatter 2002 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier 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) Science Q Physics Geophysics. Cosmic physics G. Chisham verfasserin aut M. Pinnock verfasserin aut M. Pinnock verfasserin aut In Annales Geophysicae Copernicus Publications, 2002 20(2002), Seite 13-28 (DE-627)25338981X (DE-600)1458425-6 14320576 nnns volume:20 year:2002 pages:13-28 https://doi.org/10.5194/angeo-20-13-2002 kostenfrei https://doaj.org/article/1d5b3786e092434780e5cddafd8b688f kostenfrei https://www.ann-geophys.net/20/13/2002/angeo-20-13-2002.pdf kostenfrei https://doaj.org/toc/0992-7689 Journal toc kostenfrei https://doaj.org/toc/1432-0576 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_2048 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 20 2002 13-28 |
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10.5194/angeo-20-13-2002 doi (DE-627)DOAJ078241596 (DE-599)DOAJ1d5b3786e092434780e5cddafd8b688f DE-627 ger DE-627 rakwb eng QC1-999 QC801-809 G. Chisham verfasserin aut Assessing the contamination of SuperDARN global convection maps by non-F-region backscatter 2002 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier 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) Science Q Physics Geophysics. Cosmic physics G. Chisham verfasserin aut M. Pinnock verfasserin aut M. Pinnock verfasserin aut In Annales Geophysicae Copernicus Publications, 2002 20(2002), Seite 13-28 (DE-627)25338981X (DE-600)1458425-6 14320576 nnns volume:20 year:2002 pages:13-28 https://doi.org/10.5194/angeo-20-13-2002 kostenfrei https://doaj.org/article/1d5b3786e092434780e5cddafd8b688f kostenfrei https://www.ann-geophys.net/20/13/2002/angeo-20-13-2002.pdf kostenfrei https://doaj.org/toc/0992-7689 Journal toc kostenfrei https://doaj.org/toc/1432-0576 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_2048 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 20 2002 13-28 |
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10.5194/angeo-20-13-2002 doi (DE-627)DOAJ078241596 (DE-599)DOAJ1d5b3786e092434780e5cddafd8b688f DE-627 ger DE-627 rakwb eng QC1-999 QC801-809 G. Chisham verfasserin aut Assessing the contamination of SuperDARN global convection maps by non-F-region backscatter 2002 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier 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) Science Q Physics Geophysics. Cosmic physics G. Chisham verfasserin aut M. Pinnock verfasserin aut M. Pinnock verfasserin aut In Annales Geophysicae Copernicus Publications, 2002 20(2002), Seite 13-28 (DE-627)25338981X (DE-600)1458425-6 14320576 nnns volume:20 year:2002 pages:13-28 https://doi.org/10.5194/angeo-20-13-2002 kostenfrei https://doaj.org/article/1d5b3786e092434780e5cddafd8b688f kostenfrei https://www.ann-geophys.net/20/13/2002/angeo-20-13-2002.pdf kostenfrei https://doaj.org/toc/0992-7689 Journal toc kostenfrei https://doaj.org/toc/1432-0576 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_2048 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 20 2002 13-28 |
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Assessing the contamination of SuperDARN global convection maps by non-F-region backscatter |
abstract |
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) |
abstractGer |
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) |
abstract_unstemmed |
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) |
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Assessing the contamination of SuperDARN global convection maps by non-F-region backscatter |
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