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Lateral Electromagnetic Waves - Theory and Applications to Communications, Geophysical Exploration, and Remote Sensing (Paperback, Softcover reprint of the original 1st ed. 1992)
Loot Price: R4,888
Discovery Miles 48 880
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Lateral Electromagnetic Waves - Theory and Applications to Communications, Geophysical Exploration, and Remote Sensing (Paperback, Softcover reprint of the original 1st ed. 1992)
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The propagation of waves along and across the boundary between two
media with different characteristic velocities is much more
complicated when the source is on or near the boundary than when it
is far away and the incident waves are plane. Examples of waves
generated by localized sources near a boundary are the
electromagnetic waves from the currents in a dipole on the surface
of the earth and the seismic waves from a slip event in a fault in
the earth's crust like the San Andreas fault in California. Both
involve a type of surface wave that is called a lateral wave in
electro magnetics and a head wave in seismology. Since the two are
analogous and the latter is more easily visualized, it is
conveniently used here to introduce and describe this important
type of surface wave using the data of Y. Ben Zion and P. Malin
("San Andreas Fault Zone Head Waves Near Parkfield, CA," Science
251, 1592-1594, 29 March 1991)."
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