Climatology analysis of the daytime topside ionospheric diffusive O+ flux based on incoherent scatter radar observations at Millstone Hill

Yihui Cai

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Climatology analysis of the daytime topside ionospheric diffusive O+ flux based on incoherent scatter radar observations at Millstone Hill

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Yihui Cai

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Description: Topside ionospheric O+ diffusive flux in solar minimum is derived from ISR data at Millstone Hill. O+ diffusive flux has evident seasonal, local time and altitude dependence. Geomagnetic activity changes the spatiotemporal variations of O+ diffusive flux through modulating the vertical structure of the plasma density profile in the topside ionosphere. However, such variations are clearly dependent on season.

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Climatology analysis of the daytime topside ionospheric diffusive O+ flux based on incoherent scatter radar observations at Millstone Hill

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