A large-scale ionospheric depletion by intense radio wave heating

A large (100 km N/S), stable, smoothly‐structured and significant depletion (15% in number density) of the daytime Tromsø F‐region was produced inadvertently during a Heater polarisation and beam‐forming procedure. We show that the depletion coincided with the passage of an atmospheric gravity wave...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Wright, J.W., Kopka, H., Stubbe, P.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 1988
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/522186/
https://doi.org/10.1029/GL015i013p01531
Description
Summary:A large (100 km N/S), stable, smoothly‐structured and significant depletion (15% in number density) of the daytime Tromsø F‐region was produced inadvertently during a Heater polarisation and beam‐forming procedure. We show that the depletion coincided with the passage of an atmospheric gravity wave of natural origin which served as a large‐scale ‘seed‘ depletion for the self‐focussing instability