Fig. 14From: Spread F occurrence and drift under the crest of the equatorial ionization anomaly from continuous Doppler sounding and FORMOSAT-3/COSMIC scintillation dataComparison of oblique spread structure (OSS) velocities with horizontal neutral winds determined by the HWM14 model at heights and times of observations for a Tucumán and b Taiwan. Values determined by the time delay method shown in blue; velocities determined by the tilt method shown in magenta. The dashed line marks the spread velocity equal to the HWM14 neutral wind model velocityBack to article page