Airglow observations of mesoscale low‐velocity traveling ionospheric disturbances at midlatitudes

By F. J. Garcia, M. Kelley, J. Makela, Chaosong Huang. 2000

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GPS observations of medium-scale traveling ionospheric disturbances over Europe (2011, background): “Garcia et al. (2000) and Martinis et al. (2010) report that MSTID occurrence rates at Arecibo, Puerto Rico (18.3◦ N, 66.7◦ W), have a major peak around the December solstice.”
Climatological study of GPS total electron content variations caused by medium‐scale traveling ionospheric disturbances (2006, methodology): “On the other hand, Garcia et al. [2000] have reported a high occurrence in winter over Arecibo, using an approximately 1-year long airglow imaging observation.”
Medium‐scale traveling ionospheric disturbances detected with dense and wide TEC maps over North America (2007, background): “Arecibo, Puerto Rico has a major peak in winter [Garcia et al., 2000].”
Instability of the E‐F coupled nighttime midlatitude ionosphere (2003, background): “[2] One of the outstanding questions in midlatitude ionospheric physics is, what is the source mechanism responsible for the substantial plasma structure and electric fields found in the nighttime midlatitude F layer? Most curious is the finding that these structures display a frontal form with skew”
Statistical study of medium-scale traveling ionospheric disturbances observed with the GPS networks in Southern California (2007, methodology): “Garcia et al. (2000) and Shiokawa et al. (2003a) investigated statistically the period, phase velocity, and horizontal wavelength of nighttime MSTIDs.”