Modelling the peak of the ionospheric E-
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J.E Titheridge
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Article
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2000
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Elsevier Science
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English
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Calculations with a full time-varying model are used to study changes in the height and density of the E-layer peak, caused by known changes in the neutral atmosphere. Agreement with mean observed values of N m E requires an increase of 10% in calculated ion densities, and an increase of 33% in the