<abstract xmlns="http://www.w3.org/1999/xhtml">

The Geodynamic Laboratory in Książ includes investigations of various kinds of geodynamic signals. Among others, we registered harmonic signals of the range 10−3–10−4 Hz. These signals had been found in the measurement series of the long water-tube (WT) tiltmeters. The discovered signals consist of two classes of harmonics associated with various kinds of phenomena. The first class of these signals belongs to viscoelastic vibrations of the Earth’s solid body, while the second class is produced possibly by the extremely long atmospheric infrasound waves. The signals of the vibrations of the Earth had been well recognized by the characteristic frequencies of the Earth’s free vibrations’ resonance, which occur mainly after strong earthquakes. The atmospheric pressure microvibrations affected the water level in the hydrodynamic systems of the WTs as a result of an inverse barometric effect. We observed that signals from both classes blend in the harmonics of similar frequencies and jointly affect the hydrodynamic systems of the WTs. We found that the amplitude of the second-class signals strongly depends on the location of water-tube gauges inside the underground, while the amplitudes of the first-class signals are similar for all the gauges. These observations clearly indicate the atmospheric origin of the second class of registered signals.
</abstract>

The Geodynamic Laboratory in Książ includes investigations of various kinds of geodynamic signals. Among others, we registered harmonic signals of the range 10−3–10−4 Hz. These signals had been found in the measurement series of the long water-tube (WT) tiltmeters. The discovered signals consist of two classes of harmonics associated with various kinds of phenomena. The first class of these signals belongs to viscoelastic vibrations of the Earth’s solid body, while the second class is produced possibly by the extremely long atmospheric infrasound waves. The signals of the vibrations of the Earth had been well recognized by the characteristic frequencies of the Earth’s free vibrations’ resonance, which occur mainly after strong earthquakes. The atmospheric pressure microvibrations affected the water level in the hydrodynamic systems of the WTs as a result of an inverse barometric effect. We observed that signals from both classes blend in the harmonics of similar frequencies and jointly affect the hydrodynamic systems of the WTs. We found that the amplitude of the second-class signals strongly depends on the location of water-tube gauges inside the underground, while the amplitudes of the first-class signals are similar for all the gauges. These observations clearly indicate the atmospheric origin of the second class of registered signals.

Investigation of Signals of the Range 10−3–10−4 Hz Registered by Water-Tube Tiltmeters in the Underground Geodynamic Laboratory in Książ (Sw Poland)

Wrocław University of Science and Technology

Artificial Satellites

This work is licensed under the Creative Commons Attribution 4.0 International License.

Investigation of Signals of the Range 10–10 Hz Registered by Water-Tube Tiltmeters in the Underground Geodynamic Laboratory in Książ (Sw Poland)

The Geodynamic Laboratory in Książ includes investigations of various kinds of geodynamic signals. Among others, we registered harmonic signals of the range...

Investigation of Signals of the Range 10⁻³–10⁻⁴ Hz Registered by Water-Tube Tiltmeters in the Underground Geodynamic Laboratory in Książ (Sw Poland)

Publicado en línea: 29 dic 2022

Páginas: 210 - 236

Recibido: 11 may 2022

Aceptado: 02 dic 2022

DOI: https://doi.org/10.2478/arsa-2022-0011

Palabras clave
interferometry, time series analysis, tides, planetary waves, acoustic-gravity waves, surface waves, free oscillations, ionosphere/atmosphere interactions

© 2022 Marek Kaczorowski et al., published by Sciendo

This work is licensed under the Creative Commons Attribution 4.0 International License.

Investigation of Signals of the Range 10−3–10−4 Hz Registered by Water-Tube Tiltmeters in the Underground Geodynamic Laboratory in Książ (Sw Poland)

Publicado en línea: 29 dic 2022

Páginas: 210 - 236

Recibido: 11 may 2022

Aceptado: 02 dic 2022

DOI: https://doi.org/10.2478/arsa-2022-0011

Palabras claveinterferometry, time series analysis, tides, planetary waves, acoustic-gravity waves, surface waves, free oscillations, ionosphere/atmosphere interactions

© 2022 Marek Kaczorowski et al., published by Sciendo

This work is licensed under the Creative Commons Attribution 4.0 International License.

Investigation of Signals of the Range 10⁻³–10⁻⁴ Hz Registered by Water-Tube Tiltmeters in the Underground Geodynamic Laboratory in Książ (Sw Poland)

Palabras clave
interferometry, time series analysis, tides, planetary waves, acoustic-gravity waves, surface waves, free oscillations, ionosphere/atmosphere interactions