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&deg; N, 79.2&deg; E, dip 12.5&deg;) and the E<sub>s</sub> parameters using an ionosonde at a nearby station Sriharikota (...

Full description

Bibliographic Details
Main Authors: A. K. Patra, S. Sripathi, P. B. Rao, K. S. V. Subbarao
Format: Article
Language:English
Published: Copernicus Publications 2005-03-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/23/773/2005/angeo-23-773-2005.pdf
id doaj-d18c4d4a3ee74988ade149cab3b9c094
record_format Article
spelling 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&deg; N, 79.2&deg; E, dip 12.5&deg;) and the E<sub>s</sub> parameters using an ionosonde at a nearby station Sriharikota (13.7&deg; N, 80.1&deg; E, dip 12.6&deg;) 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&deg; N, 79.2&deg; E, dip 12.5&deg;) and the E<sub>s</sub> parameters using an ionosonde at a nearby station Sriharikota (13.7&deg; N, 80.1&deg; E, dip 12.6&deg;) 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 AT akpatra simultaneousvhfradarbackscatterandionosondeobservationsoflowlatitudeeregion
AT ssripathi simultaneousvhfradarbackscatterandionosondeobservationsoflowlatitudeeregion
AT pbrao simultaneousvhfradarbackscatterandionosondeobservationsoflowlatitudeeregion
AT ksvsubbarao simultaneousvhfradarbackscatterandionosondeobservationsoflowlatitudeeregion
_version_ 1725197788215508992