13 citations as recorded by crossref.

1. Multilayered structures in the ionosphere F2 region and impulse‐like increase of the nightglow red 630 nm line intensity as a result of influence of shear excited atmospheric vortical perturbations G. Didebulidze et al. 10.1029/2008JA013348
2. Disturbances in Sporadic‐E During the Great Solar Eclipse of August 21, 2017 G. Chen et al. 10.1029/2020JA028986
3. The Role of Wind Velocity, Wind Shear, and Electric Fields in the Formation of Sporadic E (Es) G. Didebulidze et al. 10.3390/atmos16091002
4. Constantly forming sporadic E-like layers and rifts in the Martian ionosphere and their implications for Earth G. Collinson et al. 10.1038/s41550-019-0984-8
5. The Role of Neutral Wind Velocity and Its Vertical Component on Predictability of Formation and Localization of Sporadic E (Es) G. Didebulidze et al. 10.3390/atmos14061008
6. Sporadic E Layer with a Structure of Double Cusp in the Vertical Sounding Ionogram K. Yusupov & N. Bakhmetieva 10.3390/atmos12091093
7. Formation of sporadic-E (Es) layers under the influence of AGWs evolving in a horizontal shear flow G. Didebulidze et al. 10.1016/j.jastp.2015.09.012
8. Formation of Multilayered Sporadic E under an Influence of Atmospheric Gravity Waves (AGWs) G. Didebulidze et al. 10.3390/atmos11060653
9. The importance of electric field or/and neutral wind in formation and prediction of sporadic E (Es) at the equatorial and mid-latitude regions G. Didebulidze et al. 10.1016/j.jastp.2025.106540
10. Sporadic E layer observations over Arecibo using coherent and incoherent scatter radar: Assessing dynamic stability in the lower thermosphere D. Hysell et al. 10.1029/2009JA014403
11. Double atmospheric gravity wave frequency oscillations of sporadic E formed in a horizontal shear flow G. Didebulidze & L. Lomidze 10.1016/j.physleta.2009.12.026
12. Formation of sporadic E (Es) layer by homogeneous and inhomogeneous horizontal winds G. Dalakishvili et al. 10.1016/j.jastp.2020.105403
13. Global distribution of neutral wind shear associated with sporadic E layers derived from GAIA H. Shinagawa et al. 10.1002/2016JA023778