Book contents
- Frontmatter
- Contents
- Preface
- 1 The ionosphere and magnetosphere
- 2 The basic equations
- 3 The constitutive relations
- 4 Magnetoionic theory 1. Polarisation and refractive index
- 5 Magnetoionic theory 2. Rays and group velocity
- 6 Stratified media. The Booker quartic
- 7 Slowly varying medium. The W.K.B. solutions
- 8 The Airy integral function and the Stokes phenomenon
- 9 Integration by steepest descents
- 10 Ray tracing in a loss-free stratified medium
- 11 Reflection and transmission coefficients
- 12 Ray theory results for isotropic ionosphere
- 13 Ray theory results for anisotropic plasmas
- 14 General ray tracing
- 15 Full wave solutions for isotropic ionosphere
- 16 Coupled wave equations
- 17 Coalescence of coupling points
- 18 Full wave methods for anisotropic stratified media
- 19 Applications of full wave methods
- Answers to problems
- Bibliography
- Index of definitions of the more important symbols
- Subject and name index
17 - Coalescence of coupling points
Published online by Cambridge University Press: 06 December 2010
- Frontmatter
- Contents
- Preface
- 1 The ionosphere and magnetosphere
- 2 The basic equations
- 3 The constitutive relations
- 4 Magnetoionic theory 1. Polarisation and refractive index
- 5 Magnetoionic theory 2. Rays and group velocity
- 6 Stratified media. The Booker quartic
- 7 Slowly varying medium. The W.K.B. solutions
- 8 The Airy integral function and the Stokes phenomenon
- 9 Integration by steepest descents
- 10 Ray tracing in a loss-free stratified medium
- 11 Reflection and transmission coefficients
- 12 Ray theory results for isotropic ionosphere
- 13 Ray theory results for anisotropic plasmas
- 14 General ray tracing
- 15 Full wave solutions for isotropic ionosphere
- 16 Coupled wave equations
- 17 Coalescence of coupling points
- 18 Full wave methods for anisotropic stratified media
- 19 Applications of full wave methods
- Answers to problems
- Bibliography
- Index of definitions of the more important symbols
- Subject and name index
Summary
Introduction
The first order coupled wave equations (16.22) were derived and studied in § 16.3 for the neighbourhood of a coupling point z = zp where two roots q1, q2 of the Booker quartic equation are equal. If this coupling point is sufficiently isolated, a uniform approximation solution can be used in its neighbourhood and this was given by (16.29), (16.30). It was used in § 16.7 to study the phase integral formula for coupling. The approximations may fail, however, if there is another coupling point near to zp, and then a more elaborate treatment is needed. When two coupling points coincide this is called ‘coalescence’. This chapter is concerned with coupled wave equations when conditions are at or near coalescence.
A coupling point that does not coincide with any other will be called a ‘single coupling point’. It is isolated only if it is far enough away from other coupling points and singularities for the uniform approximation solution (16.30) to apply with small error for values of |ζ| up to about unity. Thus an isolated coupling point is single, but the reverse is not necessarily true.
Various types of coalescence are possible. The two coupling points that coalesce may be associated with different pairs q1, q2 and q3, q4 of roots of the Booker quartic. This is not a true coalescence because the two pairs of waves are propagated independently of each other.
- Type
- Chapter
- Information
- The Propagation of Radio WavesThe Theory of Radio Waves of Low Power in the Ionosphere and Magnetosphere, pp. 520 - 549Publisher: Cambridge University PressPrint publication year: 1985