Midlatitude sporadic-E layers and vertical metallic ion drift profiles

Physics

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Ionospheric Drift, Ionospheric Electron Density, Metal Ions, Midlatitude Atmosphere, Sporadic E Layer, Atmospheric Tides, Drift Rate, Gravity Waves, Incoherent Scatter Radar, Ionospheric Ion Density

Scientific paper

An investigation of the relationship between the occurrence of midlatitude sporadic-E-layers and convergent points in the ion drift profiles has been made using the 430 MHz incoherent scatter radar at the Arecibo Observatory. Electron concentration profiles were obtained using a 13 baud Barker coded pulse yielding 600 m range resolution, while a 5-pulse sequence with 2.4 km range resolution was used to obtain line-of-sight ion drift velocities. With some exceptions, observed sporadic-E layers occur near convergent points in the vertical metallic ion drift profile, and vertical motions of these layers follow the vertical motions of the convergent point. A sudden increase in the altitude of a sporadic-E layer has been observed. This is attributed to the disappearance of the convergent point, releasing the layer, followed by an ascent of the layer to the closest overlying convergent point.

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