Modeling the diurnal variation of ionospheric layers via Thom canonical potentials: time-frequency signatures

David H. Hughes

doi:10.1117/12.447888

6 December 2002 Modeling the diurnal variation of ionospheric layers via Thom canonical potentials: time-frequency signatures

David H. Hughes

Author Affiliations +

Proceedings Volume 4791, Advanced Signal Processing Algorithms, Architectures, and Implementations XII; (2002) https://doi.org/10.1117/12.447888
Event: International Symposium on Optical Science and Technology, 2002, Seattle, WA, United States

Abstract

The A₃ Thom canonical polynomial is used in a Newtonian gradient system to model the diurnal variation of ionospheric E and F layers. Time-frequency signatures of the plasma frequency variation over a scaled day are modeled.

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David H. Hughes "Modeling the diurnal variation of ionospheric layers via Thom canonical potentials: time-frequency signatures", Proc. SPIE 4791, Advanced Signal Processing Algorithms, Architectures, and Implementations XII, (6 December 2002); https://doi.org/10.1117/12.447888

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