dc.contributor.author |
Saha, Sovan |
|
dc.contributor.author |
Pallamraju, Duggirala |
|
dc.contributor.author |
Ghodpage, Rupesh N. |
|
dc.coverage.spatial |
United States of America |
|
dc.date.accessioned |
2022-09-17T09:58:57Z |
|
dc.date.available |
2022-09-17T09:58:57Z |
|
dc.date.issued |
2022-12 |
|
dc.identifier.citation |
Saha, Sovan; Pallamraju, Duggirala and Ghodpage, Rupesh N., “Investigations of equatorial plasma bubbles as observed in the OI 630 nm nightglow emissions over off-equatorial and low-latitudinal locations over Indian longitudes”, Advances in Space Research, DOI: 10.1016/j.asr.2022.08.023, vol. 70, no. 11, pp. 3686-3698, Dec. 2022. |
en_US |
dc.identifier.issn |
0273-1177 |
|
dc.identifier.uri |
https://doi.org/10.1016/j.asr.2022.08.023 |
|
dc.identifier.uri |
https://repository.iitgn.ac.in/handle/123456789/8138 |
|
dc.description.abstract |
Equatorial plasma bubbles (EPBs), generated over the dip-equator during the sunset time, get mapped over to the low-latitudes through the geomagnetic field lines and contribute to structures of different scales in the nighttime thermosphere-ionosphere system. In the present study, the EPBs are observed in the OI 630 nm nightglow emissions over Mt. Abu and Kolhapur using a High Throughput Imaging Echelle spectrograph (HiTIES) and All-Sky Imager (ASI), respectively. Similar periodicities obtained in these measurements consistently corroborate the presence of the EPBs at both these locations. The strength of the Pre-Reversal Enhancement (PRE) in the zonal electric field has been investigated using the ionosonde data over Trivandrum, a dip-equatorial location. The strength of PRE decides the latitudinal extent of the EPBs. The eastward movement of the EPBs has been estimated to be in the range of 190-90 ms-1, decreasing in magnitude from post-sunset to midnight. The wave number analysis carried out using the observed OI 630 nm emissions in the zonal direction has resulted in a contrasting behaviour during the presence/absence of the EPBs. Based on the analysis of around 1300 images of data, it is revealed that the scale sizes in the range of 250-300 km are omnipresent, whereas, shorter scale sizes (50-250 km) are present only during the presence of EPBs. It is inferred that these shorter scale size gravity waves played a significant role in the seeding the perturbation of the EPBs. |
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dc.description.statementofresponsibility |
by Sovan Saha, Duggirala Pallamraju and Rupesh N. Ghodpage |
|
dc.format.extent |
vol. 70, no. 11, pp. 3686-3698 |
|
dc.language.iso |
en_US |
en_US |
dc.publisher |
Elsevier |
en_US |
dc.subject |
OI 630 nm nightglow |
en_US |
dc.subject |
Equatorial plasma bubbles |
en_US |
dc.subject |
Equatorial electrodynamics |
en_US |
dc.subject |
Gravity waves |
en_US |
dc.subject |
High-resolution spectrographs |
en_US |
dc.title |
Investigations of equatorial plasma bubbles as observed in the OI 630 nm nightglow emissions over off-equatorial and low-latitudinal locations over Indian longitudes |
en_US |
dc.type |
Journal Paper |
en_US |
dc.relation.journal |
Advances in Space Research |
|