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Coupled forms of the differential equations governing radio propagation in the ionosphere. II

Published online by Cambridge University Press:  24 October 2008

K. G. Budden
Affiliation:
Cavendish Laboratory Cambridge
P. C. Clemmow
Affiliation:
Cavendish Laboratory Cambridge

Abstract

The four first-order ‘coupled’ equations governing the propagation of electromagnetic waves in the ionosphere, previously obtained in symbolic matrix form (Clemmow and Heading (4)), are expressed explicitly in terms of the ionospheric parameters. The physical significance of the equations is illustrated by considering the energy flux in one characteristic wave when coupling and damping are neglected. Three special cases are then discussed for which second-order coupled equations are also given, namely, the cases of (a) vertical incidence with oblique magnetic field, (b) oblique incidence with vertical magnetic field, (c) horizontal magnetic field in the plane of incidence. For case (a) the second-order equations are those previously derived by Försterling(5).

The form of the coupled equations is physically illuminating and, in principle, suitable for solution by successive approximations. Extensive numerical work has indeed been carried out on the second-order coupled equations in case (a) (e.g. Gibbons and Nertney(6)), and it is probable that the first-order coupled equations would prove more advantageous. The present authors, however, feel that better methods are available for purely numerical work (e.g. Budden(3)), and that the chief interest of the coupled form is that it shows the scope and limitations of the physical conception of characteristic waves.

Type
Research Article
Copyright
Copyright © Cambridge Philosophical Society 1957

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References

REFERENCES

(1)Appleton, E. V.J. Instn Elect. Engrs, 71 (1932), 642.Google Scholar
(2)Booker, H. G.Proc. Roy. Soc. A, 155 (1936), 235.Google Scholar
(3)Budden, K. G.Proc. Roy. Soc. A, 227 (1955), 516.Google Scholar
(4)Clemmow, P. C. and Heading, J.Proc. Camb. Phil. Soc. 50 (1954), 319 (Paper I).CrossRefGoogle Scholar
(5)Försterling, K.Hochfrequenztech. u. Elektroakust. 59 (1942), 10.Google Scholar
(6)Gibbons, J. J. and Nertney, R. J.J. Geophys. Res. 57 (1952), 323.CrossRefGoogle Scholar
(7)Kelso, J. M., Nearhoof, H. J., Nertney, R. J. and Waynick, A. H.Ann. Géophys. 7 (1951), 215.Google Scholar
(8)Lindquist, R. J.Atmos. Terr. Phys. 4 (1953), 10.CrossRefGoogle Scholar
(9)Rydbeck, O. E. H.Chalmers tek. Högsk. Handl. 101 (1951).Google Scholar
(10)Heading, J. Thesis (Cambridge, 1954).Google Scholar