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Fig. 4 | Earth, Planets and Space

Fig. 4

From: Influence of uncertainties of the empirical models for inferring the E-region electric fields at the dip equator

Fig. 4

Schematic representations of the variables associated with the MSIS, IRI, and IGRF models used to infer the E-region electric fields. The acronyms used are as follows: ν in is ion–neutral collision frequency, ν en is electron–neutral collision frequency, n(O), n(O2), and n(N2) are the neutral densities of O, O2, and N2, respectively, N i is ions density, N e is the electron density, H is the horizontal component of magnetic field B, Ω i is the ion gyro frequency, Ω e is the electron gyro frequency, Ψ 0 is the anisotropic factor. Local Hall (σ H) and Pedersen (σ P) conductivities, field-line-integrated Hall (Σ H) and Pedersen (Σ P) conductivities, and zonal (Ey) and vertical (Ez) electric field components are placed in the central circle

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