A theory of the origin of microseisms

@article{LonguetHiggins1950ATO,
  title={A theory of the origin of microseisms},
  author={Michael Selwyn Longuet-Higgins},
  journal={Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences},
  year={1950},
  volume={243},
  pages={1 - 35}
}
  • M. Longuet-Higgins
  • Published 27 September 1950
  • Physics
  • Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences
In the past it has been considered unlikely that ocean waves are capable of generating microseismic oscillations of the sea bed over areas of deep water, since the decrease of the pressure variations with depth is exponential, according to the first-order theory generally used. However, it was recently shown by Miche that in the second approximation to the standing wave there is a second-order pressure variation which is not attenuated with depth and which must therefore ultimately predominate… 

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I 943 Versl . gewone Vergad
  • Trans . Amer . Geophys . Un . Seism . Soc . Amer .
  • 1948
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