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The nature of terrestrial infragravitational “noise”

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Abstract

This paper is focused on analysis of comprehensive experimental research data on the infragravitational range of periods (from 20 s to 10–12 min) obtained by synchronous measurements of fluctuations in deformations of the Earth’s crust and atmospheric and hydrospheric pressure variations. It is established that the identified variations in the period range of 1–4 min are rarely observed in records of a laser nanobarograph and laser instrument for measuring hydrospheric pressure variations (laser hydrophone), while they are frequently observed in records of laser strainmeters at a variation period of 3–4 min. Oscillation excitation in the period ranges of 7–13 min, especially in the period ranges of 8–12 min, is largely related to atmospheric processes in the corresponding periods.

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Authors and Affiliations

  1. Il’ichev Pacific Oceanological Institute, Far East Branch, Russian Academy of Sciences, Vladivostok, 690000, Russia

    G. I. Dolgikh, S. G. Dolgikh & V. A. Chupin

  2. School of Natural Sciences, Far East Federal University, Vladivostok, 690091, Russia

    G. I. Dolgikh, S. G. Dolgikh & V. A. Chupin

  3. Taiwan Ocean Research Institute, Kaohsiung, Taiwan

    Yu-Hung Hsiao

Authors
  1. G. I. Dolgikh
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  2. S. G. Dolgikh
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  3. V. A. Chupin
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  4. Yu-Hung Hsiao
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Correspondence to G. I. Dolgikh.

Additional information

Original Russian Text © G.I. Dolgikh, S.G. Dolgikh, V.A. Chupin, Yu-Hung Hsiao, 2016, published in Doklady Akademii Nauk, 2016, Vol. 471, No. 4, pp. 470–474.

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Dolgikh, G.I., Dolgikh, S.G., Chupin, V.A. et al. The nature of terrestrial infragravitational “noise”. Dokl. Earth Sc. 471, 1257–1260 (2016). https://doi.org/10.1134/S1028334X16120011

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  • DOI: https://doi.org/10.1134/S1028334X16120011

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