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S

S. Ray

Researcher at University of Calcutta

Publications -  25
Citations -  441

S. Ray is an academic researcher from University of Calcutta. The author has contributed to research in topics: TEC & Ionosphere. The author has an hindex of 10, co-authored 24 publications receiving 316 citations.

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Day‐to‐day variability of the equatorial ionization anomaly and scintillations at dusk observed by GUVI and modeling by SAMI3

TL;DR: In this article, the authors used the Global Ultraviolet Imager (GUVI) data collected during evening at solar maximum to study the morphology of these so-called collapses, since the EIA collapse is shown to be linked to the suppression of equatorial plasma bubbles and scintillations.
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Long-term observations of VHF scintillation and total electron content near the crest of the equatorial anomaly in the Indian longitude zone

TL;DR: In this article, the importance of electrodynamic drift near the magnetic equator in controlling nighttime ionospheric F region ionization and irregularities in the equatorial region was investigated.
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Errors in position‐fixing by GPS in an environment of strong equatorial scintillations in the Indian zone

TL;DR: The signal-to-noise ratio (SNR) of the L1 (1.6 GHz) transmission from GPS and GLONASS satellites has been recorded at Calcutta (22.58°N, 88.38°E geographic; 32°N magnetic dip, 17.35°N dip latitude) since 1999 by a stand-alone coarse acquisition (C/A) code Ashtec receiver.
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Equatorial scintillations in relation to the development of ionization anomaly

TL;DR: In this paper, the authors used the diurnal maximum and integrated value (integrated from the time of onset of plasma influx to off-equatorial latitudes till local sunset) of the strength of the electrojet in the Indian longitude sector to calculate the vertical drift of the F-layer over the magnetic equator for the period August through October 2000.
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Study of the effect of 17-18 March 2015 geomagnetic storm on the Indian longitudes using GPS and C/NOFS

TL;DR: The largest geomagnetic storm in solar cycle 24 occurred during March 17-18, 2015 where the main phase of the storm reached the negative minimum at 22:00 UT as discussed by the authors.