Spatial Coherence of Surface Waves

Abstract

Using spatial coherency estimates of Rayleigh and Love waves recorded at ALPA, LASA and NORSAR, it is demonstrated that for a particular frequency the wave propagation cannot be described by a unique wavevector. Instead, the propagation is better described by a distribution in the wavenumber domain or, in physical terms, a distribution in azimuth and phase velocity. In general the coherency in the mean direction of propagation, which is a function of the velocity distribution, stays high relative to the coherency along the mean wavefront, which is a function of the azimuthal distribution.

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Document Details

Document Type
Technical Report
Publication Date
Dec 20, 1972
Accession Number
AD0756897

Entities

People

  • H. Mack

Organizations

  • Teledyne Technologies

Tags

Communities of Interest

  • Air Platforms
  • Energy and Power Technologies
  • Sensors

DTIC Thesaurus Topics

  • Ambient Noise
  • Background Noise
  • Baja California
  • Dispersions
  • Frequency
  • Love Waves
  • Noise
  • Phase Velocity
  • Power Spectra
  • Rayleigh Waves
  • Regions
  • Scattering
  • Seismic Arrays
  • Spectra
  • Surface Waves
  • Wave Propagation
  • Waveforms

Fields of Study

  • Physics

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Seismology