25 citations as recorded by crossref.

1. On the QBO modulation in the frequency of occurrence of pre noon F3 layers over the dip equatorial location of Thiruvananthapuram N. Mridula et al. 10.1016/j.jastp.2018.07.004
2. Quantification of the role of gravity wave induced TIDs in modulating ESF day to day variability during geomagnetically disturbed periods T. Sruthi & G. Manju 10.1016/j.asr.2021.11.038
3. Gravity wave control on ESF day‐to‐day variability: An empirical approach R. Aswathy & G. Manju 10.1002/2017JA023983
4. Simultaneous OI 630 nm imaging observations of thermospheric gravity waves and associated revival of fossil depletions around midnight near the equatorial ionization anomaly (EIA) crest N. Parihar et al. 10.5194/angeo-42-131-2024
5. SBAS-derived TEC maps: a new tool to forecast the spatial maps of maximum probable scintillation index over India S. Sunda et al. 10.1007/s10291-017-0625-6
6. Evolutionary phases of equatorial spreadFincluding L band scintillations and plumes in the context of GPS total electron content variability: A case study M. Bagiya & R. Sridharan 10.1029/2011JA016893
7. Impact of Stratospheric Sudden Warming on the Occurrence of the Equatorial Spread‐F L. Jose et al. 10.1002/2017JA024652
8. The particularly clean response of the Indian sector to a strong but short lived geomagnetic storm R. Choudhary et al. 10.1016/j.asr.2023.05.048
9. Simultaneous observation on the post-sunset occurrence of travelling ionospheric disturbance alongside ionospheric irregularities over the East Africa low latitude region O. Olwendo & P. Cilliers 10.1016/j.asr.2023.12.005
10. Response of the tropical mesopause to the longest annular solar eclipse of this millennium S. Sumod et al. 10.1029/2010JA016326
11. Relationship Between Presunset Wave Structures and Interbubble Spacing: The Seeding Perspective of Equatorial Plasma Bubble S. Das et al. 10.1029/2020JA028122
12. Role of gravity wave seed perturbations in ESF day-to-day variability: A quantitative approach G. Manju et al. 10.1016/j.asr.2015.12.019
13. Critical assessment of the forecasting capability of L-band scintillation over the magnetic equatorial region – Campaign results M. Bagiya et al. 10.1016/j.jastp.2014.01.012
14. On the behavior of thermospheric O1D 630.0 nm dayglow emission during counter electrojet events C. Vineeth et al. 10.1016/j.asr.2022.08.048
15. Signatures of Sudden Storm Commencement on the equatorial thermospheric dayglow S. Sumod et al. 10.1051/swsc/2019026
16. Refinement of the background ionospheric conditions and plausible explanation based on neutral dynamics for the occurrence/non-occurrence of L-band scintillation patches against forecast. R. Sridharan et al. 10.1016/j.jastp.2015.07.018
17. First estimations of gravity wave potential energy in the Martian thermosphere: an analysis using MAVEN NGIMS data G. Manju & N. Mridula 10.1093/mnras/staa3491
18. First observational evidence of the modulation of the threshold height h'Fc for the occurrence of equatorial spread F by neutral composition changes M. Madhav Haridas et al. 10.1002/jgra.50331
19. A novel method based on GPS TEC to forecast L band scintillations over the equatorial region through a case study R. Sridharan et al. 10.1016/j.jastp.2012.02.007
20. On the role of horizontal wind shears in the generation of F0.5 layers over the dip equatorial location of Thiruvananthapuram: A numerical simulation study N. Mridula & T. Pant 10.1016/j.jastp.2017.02.005
21. Mesospheric wave signatures and equatorial plasma bubbles: A case study A. Taori et al. 10.1029/2009JA015088
22. Daytime upper mesospheric energetics over a tropical station, Trivandrum (8.5°N, 77°E): An investigation using the multiwavelength dayglow photometry C. Vineeth et al. 10.1029/2010JA015633
23. Day-to-day and short-term variabilities in the equatorial plasma bubble/spread F irregularity seeding and development M. Abdu 10.1186/s40645-019-0258-1
24. Equatorial Ionization Anomaly crest magnitude and its implications on the nocturnal equatorial ionospheric plasma irregularity characteristics R. Aswathy & G. Manju 10.1016/j.asr.2021.07.019
25. F layer postsunset height rise due to electric field prereversal enhancement: 2. Traveling planetary wave ionospheric disturbances and their role on the generation of equatorial spread F P. Fagundes et al. 10.1029/2009JA014482