A statistical study of large-scale traveling ionospheric disturbances using the GPS network in Japan

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Medium‐scale traveling ionospheric disturbances detected with dense and wide TEC maps over North America (2007, background): “The ion-drag effect can damp the AGWs in the daytime ionosphere [ Tsugawa et al., 2003, 2004 ].”
Medium-scale traveling ionospheric disturbances affecting GPS measurements: Spatial and temporal analysis (2006, methodology): “This detrending can be done in several ways, for example, Tsugawa et al. [2004] makes this detrending by looking for vertical TEC perturbations from a dense GPS network, whereas other authors make the detrending using a band filtering or a polynomial adjust of the ionospheric data over a period of”
Large-scale traveling ionospheric disturbances observed by GPS total electron content during the magnetic storm of 29-30 October 2003 (2007, methodology): “reported from the statistical results of Tsugawa et al. [2004] .”
Directivity and apparent velocity of the coseismic ionospheric disturbances observed with a dense GPS array (2005, background): “8 km/sec by GPS observations of LSTID, a large-scale traveling disturbance in TEC caused by a gravity wave originating in the auroral oval [13, 14].”
GNSS Observations of Ionospheric Variations During the 21 August 2017 Solar Eclipse (2017, methodology): “Differential TEC has been successfully used to observe both large-scale and medium-scale TIDs (Tsugawa et al., 2003, 2004).”