Simultaneous VHF radar backscatter and ionosonde observations of low-latitude E region
The first results of simultaneous observations made on the low-latitude field-aligned irregularities (FAI) using the MST radar located at Gadanki (13.5° N, 79.2° E, dip 12.5°) and the E<sub>s</sub> parameters using an ionosonde at a nearby station Sriharikota (...
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Copernicus Publications
2005-03-01
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doaj-d18c4d4a3ee74988ade149cab3b9c0942020-11-25T01:04:29ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762005-03-012377377910.5194/angeo-23-773-2005Simultaneous VHF radar backscatter and ionosonde observations of low-latitude E regionA. K. Patra0S. Sripathi1P. B. Rao2K. S. V. Subbarao3National MST Radar Facility, Tirupati, IndiaNational MST Radar Facility, Tirupati, IndiaNational Remote Sensing Agency, Hyderabad, IndiaSpace Physics Laboratory, VSSC, Trivandrum, IndiaThe first results of simultaneous observations made on the low-latitude field-aligned irregularities (FAI) using the MST radar located at Gadanki (13.5° N, 79.2° E, dip 12.5°) and the E<sub>s</sub> parameters using an ionosonde at a nearby station Sriharikota (13.7° N, 80.1° E, dip 12.6°) are presented. The observations show that while the height of the most intense radar echoes is below the virtual height of E<sub>s</sub> (h'E<sub>s</sub>) during daytime, it is found to be either below or above during nighttime. The strength of the FAI is better correlated with the top penetration frequency (f<sub>t</sub>E<sub>s</sub>) and the blanketing frequency (f<sub>b</sub>E<sub>s</sub>) during the night (r=0.4 in both cases) as compared to the day (r=0.35 and -0.04, respectively). Furthermore, the signal strength of FAI is reasonably correlated with (f<sub>t</sub>E<sub>s</sub>-f<sub>b</sub>E<sub>s</sub>) during daytime (r=0.59) while very poorly correlated during nighttime (r=0.18). While the radar observations in general appear to have characteristics close to that of mid-latitudes, the relationship of these with the E<sub>s</sub> parameters are poorer than that of mid-latitudes. The observations reported here, nevertheless, are quite consistent with the expectations based on the gradient drift instability mechanism.https://www.ann-geophys.net/23/773/2005/angeo-23-773-2005.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
A. K. Patra S. Sripathi P. B. Rao K. S. V. Subbarao |
spellingShingle |
A. K. Patra S. Sripathi P. B. Rao K. S. V. Subbarao Simultaneous VHF radar backscatter and ionosonde observations of low-latitude E region Annales Geophysicae |
author_facet |
A. K. Patra S. Sripathi P. B. Rao K. S. V. Subbarao |
author_sort |
A. K. Patra |
title |
Simultaneous VHF radar backscatter and ionosonde observations of low-latitude E region |
title_short |
Simultaneous VHF radar backscatter and ionosonde observations of low-latitude E region |
title_full |
Simultaneous VHF radar backscatter and ionosonde observations of low-latitude E region |
title_fullStr |
Simultaneous VHF radar backscatter and ionosonde observations of low-latitude E region |
title_full_unstemmed |
Simultaneous VHF radar backscatter and ionosonde observations of low-latitude E region |
title_sort |
simultaneous vhf radar backscatter and ionosonde observations of low-latitude e region |
publisher |
Copernicus Publications |
series |
Annales Geophysicae |
issn |
0992-7689 1432-0576 |
publishDate |
2005-03-01 |
description |
The first results of simultaneous observations made on the low-latitude
field-aligned irregularities (FAI) using the MST radar located at Gadanki
(13.5° N, 79.2° E, dip 12.5°) and the E<sub>s</sub> parameters
using an ionosonde at a nearby station Sriharikota (13.7° N, 80.1° E,
dip 12.6°) are presented. The observations show that while the
height of the most intense radar echoes is below the virtual height of
E<sub>s</sub> (h'E<sub>s</sub>) during daytime, it is found to be either below
or above during nighttime. The strength of the FAI is better correlated with
the top penetration frequency (f<sub>t</sub>E<sub>s</sub>) and the blanketing frequency
(f<sub>b</sub>E<sub>s</sub>) during the night (r=0.4 in both cases) as compared to the
day (r=0.35 and -0.04, respectively). Furthermore, the signal strength of FAI
is reasonably correlated with (f<sub>t</sub>E<sub>s</sub>-f<sub>b</sub>E<sub>s</sub>) during daytime
(r=0.59) while very poorly correlated during nighttime (r=0.18). While
the radar observations in general appear to have characteristics close to
that of mid-latitudes, the relationship of these with the E<sub>s</sub> parameters
are poorer than that of mid-latitudes. The observations reported here,
nevertheless, are quite consistent with the expectations based on the gradient
drift instability mechanism. |
url |
https://www.ann-geophys.net/23/773/2005/angeo-23-773-2005.pdf |
work_keys_str_mv |
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1725197788215508992 |