Publication Abstracts

Rind 1980

Rind, D., 1980: Microseisms at Palisades: 3. Microseisms and microbaroms. J. Geophys. Res., 85, no. B9, 4854-4862, doi:10.1029/JB085iB09p04854.

Microseisms (seismic surface waves) in the frequency range of 0.1-1 Hz recorded at Palisades, New York, are compared with microbaroms (infrasound) in the same frequency range recorded simultaneously. Both are thought to be generated by interfering ocean waves, and the question addressed is how often does their comparison imply that they have the same source. Compared were their approximate regions of formation, the formation conditions (both meteorological and oceanographic), amplitude variations, and frequency spectra. It is concluded that for the signals recorded at this location the two phenomena appear to have the same ocean wave sources 2/3 of the times and at least some of the remaining times one of the signals is prevented from arriving owing to propagation difficulties.

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BibTeX Citation

  author={Rind, D.},
  title={Microseisms at Palisades: 3. Microseisms and microbaroms},
  journal={J. Geophys. Res.},

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RIS Citation

ID  - ri05900r
AU  - Rind, D.
PY  - 1980
TI  - Microseisms at Palisades: 3. Microseisms and microbaroms
JA  - J. Geophys. Res.
VL  - 85
IS  - B9
SP  - 4854
EP  - 4862
DO  - 10.1029/JB085iB09p04854
ER  -

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