• Solar wind flow angle and geoeffectiveness of corotating interaction regions: First results 

  Rout, D.; Chakrabarty, D.; Janardhan, P.; Sekar, R.; Maniya, V.; Pandey, K. (Geophysical Research Letters, 2017-05-04)

  "A total of 43 Corotating Interaction Region (CIR)‐induced geomagnetic storms during the unusually deep solar minimum of solar cycle 23 (2006–2010) were identified using a superposed epoch analysis technique. Of these 43 ...
• June Solstice Equatorial Spread F in the American Sector: A Numerical Assessment of Linear Stability Aided by Incoherent Scatter Radar Measurements 

  Zhan, W.; Rodrigues, F. (Journal of Geophysical Research: Space Physics banner, 2017-12-13)

  "Previous studies have suggested that weakening downward plasma drifts can produce favorable conditions for the ionospheric Generalized Rayleigh‐Taylor (GRT) instability and explain the occurrence of postmidnight equatorial ...
• Gravity Wave‐Induced Ionospheric Irregularities in the Postsunset Equatorial Valley Region 

  Hysell, D.; Fritts, D.; Laughman, B.; Chau, J. (Journal of Geophysical Research: Space Physics, 2017-09-29)

  "Plasma irregularities in the postsunset equatorial valley region ionosphere are investigated experimentally and through numerical simulation. Coherent radar backscatter observed at the Jicamarca Radio Observatory shows ...
• Equatorial Ionospheric Response to Different Estimated Disturbed Electric Fields as Investigated Using Sheffield University Plasmasphere Ionosphere Model at INPE 

  Bravo, M.; Batista, S.; Souza, J.; Foppiano, A. (Journal of Geophysical Research: Space Physics banner, 2017-09-14)

  "Good ionospheric modeling is important to understand anomalous effects, mainly during geomagnetic storm events. Ionospheric electric fields, thermospheric winds, and neutral composition are affected at different degrees, ...
• Comparison of ionospheric profile parameters with IRI-2012 model over Jicamarca 

  Bello, S.; Abdullah, M.; Hamid, N.; Reinisch, B. (Journal of Physics: Conference Series, 2017-01-01)

  "We used the hourly ionogram data obtained from Jicamarca station (12° S, 76.9° W, dip latitude: 1.0° N) an equatorial region to study the variation of the electron density profile parameters: maximum height of F2-layer ...

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