Abstract
The effects of F-region neutral winds on the distribution of He + in the equatorial ionosphere have been examined using a theoretical model and an observational data set. It is shown by the model that components of neutral wind in the magnetic meridian up to only 50 m s − can produce He + gradients in the northern and southern sectors of a flux tube that differ by more than 80%. This is associated with interhemisphere transport velocities of He + as large as 15 m s −1 at 800 km. A substantial latitude gradient in the He + distribution across the dip equator also results from the redistribution of He + The changes in the He + concentration at the dip equator and the latitude distribution of He + in response to different neutral wind components is determined from the model and used to construct longitude distributions of He + to compare with observations made at equinox. Good agreement between the calculations and observations is obtained both at the geographic and geomagnetic equators using the relationship between neutral winds, interhemispheric transport velocity and He + concentration derived from the model. If these relationships can be extrapolated to accommodate the different conditions expected during solstice, we can also discuss the He + distributions expected during this season.
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