Flow angle dependence for the asymmetry of broad 50-MHz coherent echoes at large magnetic aspect angles
The skewness of broad Type 2-like spectra has been studied using data collected by two orthogonal CW 50-MHz radio links with co-located scattering volumes. Geometrical aspect angles of observations were about 10Ã. One short event was considered. For this event, the electron flow direction was chang...
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Veröffentlicht in: | Annales geophysicae (1988) 1997-01, Vol.15 (6), p.760-766 |
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creator | Kustov, A. V. Sofko, G. J. Koehler, J. A. Uspensky, M. V. |
description | The skewness of broad Type 2-like spectra has been studied using data collected by two orthogonal CW 50-MHz radio links with co-located scattering volumes. Geometrical aspect angles of observations were about 10Ã. One short event was considered. For this event, the electron flow direction was changing periodically (period about 9 minutes) presumably due to the passage of a magnetospheric MHD wave through the ionosphere. It was found that for the radar observations along the electrojet flow, the skewness had the same sign as the mean Doppler shift with average absolute values in between 0.5-1.0. For observations perpendicular to the electrojet flow, spectra were more symmetrical (average skewness was around 0) and the sign of the skewness was sometimes opposite to the sign of the mean Doppler shift. These observations are interpreted in terms of contribution from both the Farley-Buneman and gradient-drift instabilities to the resultant spectrum. Differences with radar observations at small aspect angles are discussed. |
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V. ; Sofko, G. J. ; Koehler, J. A. ; Uspensky, M. V.</creator><creatorcontrib>Kustov, A. V. ; Sofko, G. J. ; Koehler, J. A. ; Uspensky, M. V.</creatorcontrib><description>The skewness of broad Type 2-like spectra has been studied using data collected by two orthogonal CW 50-MHz radio links with co-located scattering volumes. Geometrical aspect angles of observations were about 10Ã. One short event was considered. For this event, the electron flow direction was changing periodically (period about 9 minutes) presumably due to the passage of a magnetospheric MHD wave through the ionosphere. It was found that for the radar observations along the electrojet flow, the skewness had the same sign as the mean Doppler shift with average absolute values in between 0.5-1.0. For observations perpendicular to the electrojet flow, spectra were more symmetrical (average skewness was around 0) and the sign of the skewness was sometimes opposite to the sign of the mean Doppler shift. These observations are interpreted in terms of contribution from both the Farley-Buneman and gradient-drift instabilities to the resultant spectrum. 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For observations perpendicular to the electrojet flow, spectra were more symmetrical (average skewness was around 0) and the sign of the skewness was sometimes opposite to the sign of the mean Doppler shift. These observations are interpreted in terms of contribution from both the Farley-Buneman and gradient-drift instabilities to the resultant spectrum. Differences with radar observations at small aspect angles are discussed.</description><subject>Earth Sciences</subject><subject>Ocean, Atmosphere</subject><subject>Sciences of the Universe</subject><issn>0992-7689</issn><issn>1432-0576</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1997</creationdate><recordtype>article</recordtype><recordid>eNpVUcGKFDEQbUTBcfXoPSfBQ6-VpJN0jsPiOsKIFz2HmnSlp6W7MyZZZfz6zdIiSEG94vHeo-A1zVsOtxzAfMgAqld1QWfls2bHOylaUEY_b3ZgrWiN7u3L5lXOPwBAc9vvmvF-jr8ZruNMbKALrQOtnliIiZUzMczXZaGSriwGdkoRB6ag_XL4w3w8U6K1MPLnSJlhYTOmkdiC40pl8tV7IV-27Py6eRFwzvTmL9403-8_frs7tMevnz7f7Y-tF1qXVpAHHYwgiVr5-nOPhkuvJXSneqoTWduFfjDWBoneSo1DGCp4NMLyQd4077fcM87ukqYF09VFnNxhf3RPHIDkWpj-F6_ad5v2kuLPB8rFLVP2NM-4UnzIjvdcKiNEFd5uwhFnctMaYkno6wy0TD6uFKbK77ueKwtCQTW0m8GnmHOi8O8VDu6pK_dfV_IRF7yFTQ</recordid><startdate>19970101</startdate><enddate>19970101</enddate><creator>Kustov, A. V.</creator><creator>Sofko, G. J.</creator><creator>Koehler, J. 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V.</creatorcontrib><creatorcontrib>Sofko, G. J.</creatorcontrib><creatorcontrib>Koehler, J. A.</creatorcontrib><creatorcontrib>Uspensky, M. V.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Hyper Article en Ligne (HAL)</collection><collection>Hyper Article en Ligne (HAL) (Open Access)</collection><jtitle>Annales geophysicae (1988)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kustov, A. V.</au><au>Sofko, G. J.</au><au>Koehler, J. A.</au><au>Uspensky, M. 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It was found that for the radar observations along the electrojet flow, the skewness had the same sign as the mean Doppler shift with average absolute values in between 0.5-1.0. For observations perpendicular to the electrojet flow, spectra were more symmetrical (average skewness was around 0) and the sign of the skewness was sometimes opposite to the sign of the mean Doppler shift. These observations are interpreted in terms of contribution from both the Farley-Buneman and gradient-drift instabilities to the resultant spectrum. Differences with radar observations at small aspect angles are discussed.</abstract><pub>Copernicus GmbH</pub><doi>10.1007/s005850050493</doi><tpages>7</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Earth Sciences Ocean, Atmosphere Sciences of the Universe |
title | Flow angle dependence for the asymmetry of broad 50-MHz coherent echoes at large magnetic aspect angles |
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