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Past and recent studies of the empirical relations between the solar wind (SW) parameters and geomagnetic activity indices have provided a general understanding of the SW‐magnetosphere transfer processes. The present study deals with the relationship between the y‐component (GSM coordinate system) of the interplanetary electric field (IEF, E y ) and the low latitude magnetospheric convection electric field E M . This relationship provides an estimate of the field transfer efficiency between SW and magnetosphere. First the E M ‐field, which has been obtained from electron density profiles measured onboard the GEOS‐1 and ISEE‐1 spacecraft, is correlated directly with the corresponding E y ‐field, as calculated from published values of the interplanetary magnetic field and velocity [King, 1979] in a case‐by‐case study. Second, a statistical study is made between E y and the geomagnetic index K m for low and moderate magnetic activity (K m ≤ 5+) from which one deduces a ’statistical’ relationship between E y and E M . The transfer coefficients obtained by both methods are identical: ΔE M /ΔE y = 0.13. This result is discussed in the framework of present theories of SW‐magnetosphere transfer processes.
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Wu et al. (1981) studied this question.
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