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1. High‐latitude GPS phase scintillation from E region electron density gradients during the 20–21 December 2015 geomagnetic storm

   https://doi.org/10.1002/2016JA023839  

   Loucks, Diana ; Palo, Scott ; Pilinski, Marcin ; Crowley, Geoff ; Azeem, Irfan ; Hampton, Don ( July 2017 , Journal of Geophysical Research: Space Physics)
2. Performance Evaluation of an Automatic GPS Ionospheric Phase Scintillation Detector Using a Machine-Learning Algorithm: Scintillation detection with machine learning

   https://doi.org/10.1002/navi.188  

   Jiao, Yu ; Hall, John J. ; Morton, Yu T. ( September 2017 , Navigation)
3. The variability of low-latitude ionospheric amplitude and phase scintillation detected by a triple-frequency GPS receiver: Variability of Ionospheric Scintillation

   https://doi.org/10.1002/2016RS006165  

   de Oliveira Moraes, Alison ; Costa, Emanoel ; Abdu, Mangalathayil Ali ; Rodrigues, Fabiano S. ; de Paula, Eurico Rodrigues ; Oliveira, Kelias ; Perrella, Waldecir João ( April 2017 , Radio Science)
4. Severe L-band scintillation over low-to-mid latitudes caused by an extreme equatorial plasma bubble: joint observations from ground-based monitors and GOLD

   https://doi.org/10.1186/s40623-023-01797-5  

   Sousasantos, Jonas ; Gomez Socola, Josemaria ; Rodrigues, Fabiano S. ; Eastes, Richard W. ; Brum, Christiano G. ; Terra, Pedrina ( December 2023 , Earth, Planets and Space)

   Abstract The occurrence of plasma irregularities and ionospheric scintillation over the Caribbean region have been reported in previous studies, but a better understanding of the source and conditions leading to these events is still needed. In December 2021, three ground-based ionospheric scintillation and Total Electron Content monitors were installed at different locations over Puerto Rico to better understand the occurrence of ionospheric irregularities in the region and to quantify their impact on transionospheric signals. Here, the findings for an event that occurred on March 13–14, 2022 are reported. The measurements made by the ground-based instrumentation indicated that ionospheric irregularities and scintillation originated at low latitudes and propagated, subsequently, to mid-latitudes. Imaging of the ionospheric F-region over a wide range of latitudes provided by the GOLD mission confirmed, unequivocally, that the observed irregularities and the scintillation were indeed caused by extreme equatorial plasma bubbles, that is, bubbles that reach abnormally high apex heights. The joint ground- and space-based observations show that plasma bubbles reached apex heights exceeding 2600 km and magnetic dip latitudes beyond 28 ° . In addition to the identification of extreme plasma bubbles as the source of the ionospheric perturbations over low-to-mid latitudes, GOLD observations also provided experimental evidence of the background ionospheric conditions leading to the abnormally high rise of the plasma bubbles and to severe L-band scintillation. These conditions are in good agreement with the theoretical hypothesis previously proposed. Graphical Abstract 

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5. Dependencies of GPS Scintillation Indices on the Ionospheric Plasma Drift and Rate of Change of TEC Around the Dawn Sector of the Polar Ionosphere

   https://doi.org/10.1029/2022JA030870  

   Wang, Y. ; Jayachandran, P. T. ; Ma, Y.‐Z. ; Zhang, Q.‐H. ; Xing, Z.‐Y. ; Ruohoniemi, J. M. ; Shepherd, S. G. ; Lester, M. ( November 2022 , Journal of Geophysical Research: Space Physics)