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
✦ LIBER ✦
Comments on “Modelling the peak of the ionospheric E-layer” by J.E. Titheridge
✍ Scribed by Q.H. Zhou; J.D. Mathews
- Publisher
- Elsevier Science
- Year
- 2001
- Tongue
- English
- Weight
- 112 KB
- Volume
- 63
- Category
- Article
- ISSN
- 1364-6826
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