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|Title:||An Explanation for the Banded Structure of Low-Latitude Whistlers Observed on the Ground|
|Abstract:||Employing a wave-slab interaction model, full-wave calculations are carried out to explain the banded structure in low-latitude whistlers observed at Nainital ground station. The results show that the specular reflection of the whistler waves from a field-aligned slab of enhanced ionization existing in the E-region of the ionosphere, possibly in the form of sporadic-E layers, is the only possible mechanism in which banding in whistler spectrum may be caused.|
|ISSN:||0975-105X (Online); 0367-8393 (Print)|
|Appears in Collections:||IJRSP Vol.09(1) [February 1980]|
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