A Love wave is a horizontally polarized shear wave trapped in a slower elastic surface layer above a faster elastic half-space. Zero shear traction at the free surface, displacement continuity and traction continuity at the interface produce its dispersion relation. A trapped mode has phase speed between the two shear speeds and decays exponentially into the half-space.
For an aligned anisotropic surface layer, , while the isotropic substrate has . Zero top traction and welded displacement/traction continuity give the displayed dispersion relation. The horizontal speed sets the limiting phase velocity; the vertical speed sets rigid-base cutoff frequencies. The effective contrast for the high-contrast transition is .
A free top and rigid base impose transverse wavenumbers on guided SH modes between rigid and free planes. Their phase velocity and group velocity are and for . A real Love wave replaces the rigid base by an evanescent elastic load; the approximation becomes reliable sufficiently above the corresponding strong-dispersion transition, not at the actual mode cutoff.
With , and a fixed mode index, put , and . The exact Love wave branch has and . Its minimum group velocity occurs near , with transition width of order . Well above that width, the rigid-base approximation to Love waves captures both velocities. Density ratios and the mode index must be controlled in this estimate.
For a slow uniform layer over a faster half-space, the nth Love wave branch reaches the half-space shear wave speed at the displayed threshold. Its half-space decay exponent then vanishes, so the threshold is a limiting nonlocalized state, not a trapped finite-energy mode. The fundamental has zero threshold and exists at every positive frequency; overtones require frequency strictly above their positive threshold. At high frequency each fixed branch approaches the layer shear wave speed from above.
For a slower surface layer supporting propagating SH-waves with vertical wavenumber above an evanescent half-space with decay exponent , continuity of displacement field and traction gives the displayed reflection coefficient for a downward incident displacement field wave. Its modulus is one and its wave phase is . A traction-free top reflects displacement field with coefficient . The round-trip condition then gives , equivalent to direct Love wave mode matching.
For a slow elastic layer above a faster half-space, put and . The positive branches of intersect the positive strictly decreasing traction ratio once whenever their left endpoint is strictly below . The fundamental exists for every positive ; the second requires the displayed strict inequality. At equality and the half-space decay exponent vanishes, so that endpoint is a cutoff, not a trapped mode satisfying decay at minus infinity.
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A Love wave is a type of surface seismic wave that travels along the Earth's surface and is named after the British mathematician A. E. H. Love, who first described them in the early 20th century. Love waves are characterized by a horizontal shearing motion that occurs in a horizontal plane perpendicular to the direction of wave propagation. Key characteristics of Love waves include: 1. **Motion**: Love waves involve side-to-side motion of the ground.