Study of the influence of meteorological factors on the parameters of the main tidal waves in the NS direction
DOI:
https://doi.org/10.24028/gj.v48i3.349607Keywords:
earth tides, tiltmeter observations, temperature and barometric observations, tidal harmonic analysis, thermoelastic deformations, reliable geophysical informationAbstract
In order to identify the influence of meteorological factors on the parameters of the main tidal waves of tilt, which have important geophysical significance, hourly series of 11-year tiltmeter observations in Poltava for the NS direction and similar 10-year series of air temperature and atmospheric pressure were processed by tidal harmonic analysis. Significant systematic disturbances of the parameters of the main tidal waves and the phase delay of the daily disturbing tilt of the ground in relation to the air temperature were revealed, which in January—March is 3 hours, and in May—December — 6 hours. It was established that the causes of systematic disturbances of the tidal parameters are deformation processes of the soil layer at a depth of 0.10—0.25 m, which are caused by local exogenous and endogenous factors, among which the main role is played by the instability of the thermal field, soil moisture and the length of thermal waves in the vicinity of the tiltmeter point. The possibility of freeing the parameters of daily tidal waves from systematic temperature disturbances by involving the theory of thermoelastic deformations, physical properties of the soil, and temperature field parameters is shown. Thus, for the K1 wave, the difference in amplitudes and phase shifts between the temperature perturbing tilts obtained from observations and those calculated on the basis of the theory of thermoelastic deformations turned out to be practically absent in the average annual measurement. This convincingly indicates the possibility and necessity of cleaning the observed data from the systematic influence of temperature disturbances in order to obtain reliable geophysical information. It was established that atmospheric pressure practically does not affect the parameters of semidiurnal and diurnal tidal waves of lunar origin. The obtained results convincingly indicate the influence of atmospheric pressure on both the amplitude and the phase of the tidal wave of solar origin S2.
References
Aksentyeva, Z.N., Bulatsen, V.G., & Tokar, V.I. (1970). On the processing of an 11-year series of observations (1930-1941) of the plumb line fluctuations in Poltava. Vraschenie i prilivnyie deformatsii Zemli, (2), 3—8 (in Russian).
Anokhina, K.M., & Shirokov, I.A. (1974). Some results of observations of periodic thermal tilts of the earth’s surface. Vraschenie i prilivnyie deformatsii Zemli, (6), 82—88 (in Russian).
Bagmet, A.L., & Kutnyi, A.M. (1973). Standardization of tiltmeters with photoelectric magnification at small tilt angles. Vraschenie i prilivnyie deformatsii Zemli, (5), 46—50 (in Russian).
Balenko, V.G. (1980). Study of the slopes of the earth’s surface along the Kyiv-Artemovsk profile. Kiev: Naukova Dumka, 173 p. (in Russian).
Balenko, V.G., Kutnyi, A.M., & Novikova, A.N. (1978).
Results of observations of tidal tilts at the Berezovaya Rudka station. Vraschenie i prilivnyie deformatsii Zemli, (10), 14—22 (in Russian).
Balenko, V.G., Kutnyi, A.M., & Novikova, A.N. (1972). Results of observations of tidal tilts at the Katerinovka station. Vraschenie i prilivnyie deformatsii Zemli, (4), 65—75 (in Russian).
Balenko, V.G., Kutnyi, A.M., & Novikova, A.N. (1975). Results of observations of tidal tilts at the Pokrovskaya Bagachka station. Vraschenie i prilivnyie deformatsii Zemli, (7), 15—21 (in Russian).
Balenko, V.G., Kutnyi, A.M., & Novikova, A.N. (1970). Results of observations of tidal tilts at the Shevchenkovo station, Karlovka district, Poltava region. Vraschenie i prilivnyie deformatsii Zemli, (2), 41—56 (in Russian).
Bulatsen, V.G., & Bogdan, I.Yu. (1978). On the influence of the daily meteorological wave S1 on the results of the harmonic analysis of an 11-year (1930—1941) series of tiltmeter observations in Poltava. Vraschenie i prilivnyie deformatsii Zemli, (10), 48—51 (in Russian).
Golubitskiy, V.G., Matveev, P.S., Bogdan, I.Yu., Krivonos, A.L., & Slavinskaya, E.A. (1982). Results of harmonic analysis of tiltmeter observations at the Peregonovka station for 1974—1978. Vraschenie i prilivnyie deformatsii Zemli, (14), 23—31 (in Russian).
Golubitskiy, V.G., Matveev, P.S., Bogdan, I.Yu., & Slavinskaya, E.A. (1977). Results of harmonic analysis of tiltmeter observations in Khristoforovka. Vraschenie i prilivnyie deformatsii Zemli, (9), 3—12 (in Russian).
Gridnev, D.G. (1975). Standardization of Askania gravimeters and determination of the scale of recording tidal changes in gravity by tilt. Temperature tilts of pedestals. Vraschenie i prilivnyie deformatsii Zemli, (6), 42—53 (in Russian).
Kutnyi, A.M., & Babich, T.M. (2010). Accuracy increase of determination of resonance effect of liquid core of the Earth on the earth’s tides. Geofizicheskiy Zhurnal, 32(3), 140—142. https://doi.org/10.24028/gzh.0203-3100.v32i3. 2010.117548 (in Ukrainian).
Kutnyi, A.M., Bulatsen, V.G., Brodskiy, B.I., & Sostin, A.A. (1992). Borehole extensometer of the Poltava gravimetric observatory. In Rotation and deformation of the Earth (pp. 97—104). Kiev: Naukova Dumka (in Russian).
Kutnyi, A.M., Pavlyk, V.G., & Babych, T.M. (2013). Modeling and separate elimination of disturbances in tidal observations. Geofizicheskiy Zhurnal, 35(2), 157—162. https://doi.org/ 10.24028/gzh.0203-3100.v35i2.2013.111359 (in Ukrainian).
Kutnyi, A.M., Pavlyk, V.G., Bulacen, V.G., Golubytsky, V.G., Bohdan, I.Yu., Korba, P.S., Babych, T.M., & Plys, V.P. (2015). Results and analysis of tidal observations in the territory of Ukraine. Geofizicheskiy Zhurnal, 37(2), 56—72. https://doi.org/10.24028/gzh.0203-3100.v37i2. 2015.111305 (in Ukrainian).
Matveev, P.S., Bohdan, I.Yu., Dubyk, B.S., & Slavynskaya, E.A. (1971). The results of the harmonic analysis of inclinometers observed in Samotoevka and Lykhovka. Vraschenie i prilivnyie deformatsii Zemli, (3), 39—52 (in Russian).
Matveev, P.S., Golubitskiy, V.G., Bohdan, I.Yu., Dubyk, B.S., & Slavynskaya, E.A. (1977). Refined values of earth’s tide parameters for stations of the Sumy-Kherson tiltmeter profile. Vraschenie i prilivnyie deformatsii Zemli, (9), 16—33 (in Russian).
Matveev, P.S., Golubitskiy, V.G., Dubyk, B.S., & Slavynskaya, E.A. (1974). Results of the harmonic analysis of tiltmeters observed in Murakhovka. Vraschenie i prilivnyie deformatsii Zemli, (6), 28—36 (in Russian).
Matveev, P.S., Ostrovskiy, A.E., Golubitskiy, V.G., Bohdan, I.Yu., Dubyk, B.S., & Slavynskaya, E.A. (1975). Results of harmonic analysis of tiltmeters observed at the Sudiivka station for 1971—1973. Vraschenie i prilivnyie deformatsii Zemli, (7), 3—9 (in Russian).
Meteopost. Weather data archive. (2024). Retrieved from https://meteopost.com/weather/archive/.
Pavlyk, V.G., Balenko, V.G., Kutnyi, A.M., & Novikova, A.N. (1988). Some issues of thermal and gravitational tides in the atmosphere. In Study of the Earth as a planet by methods of geophysics, geodesy and astronomy: Proceedings of the II Orlov Conference (pp. 174—176). Kiev: Naukova Dumka (in Russian).
Shirokov, I.A., & Anokhina, K.M. (1975). Local temperature slopes of the earth’s surface. Vraschenie i prilivnyie deformatsii Zemli, (7), 32—38 (in Russian).
Albano, A., Corrado, G., Gervasi, A., Guerra, I. (2015). Continuous gravity and tilt observations in an active geodynamic area of southern Italy: the Calabrian Arc system. Bollettino di Geofisica Teorica ed Applicata, 56(1), 1—18. https://doi.org/10.4430/bgta0133.
Bán, D., Mentes, G., Kis, M., & Koppán, A. (2018). Observation of the Earth Liquid Core Resonance by Extensometers. Pure and Applied Geophysics, 175(4), 1631—1642. https://doi.org/10.1007/s00024-017-1724-6.
Braitenberg, C. (2018). The deforming and rotating Earth — A review of the 18th International Symposium on Geodynamics and Earth Tide, Trieste 2016. Geodesy and Geodynamics, 9(3), 187—196. https://doi.org/10.1016/j.geog.2018.03.003.
Cui, X., Sun, H., Xu, J., Zhou, J., & Chen, X. (2018). Detection of free core nutation resonance variation in Earth tide from global superconducting gravimeter observations. Earth, Planets and Space, 70, 199. https://doi.org/10.1186/s40623-018-0971-9.
Harrison, J.C. (1976). Cavity and topographic effects in tilt and strain measurement. Journal of Geophysical Research, 81(2), 319—328. https://doi.org/10.1029/JB081i002p00319.
Jobert, G. (1960). Perturbations des marees terrestres. Annales Geophysicae, 16, 1—55.
Lyard, L., Lefevre, L., Letellier, T., & Francis, O. (2006). Modelling the global ocean tides: insights from FES2004. Ocean Dynamics, 56, 394—415. https://doi.org/10.1007/s10236-006-0086-x.
Mathews, P.M., Buffett, B.A., & Shapiro, I.I. (1995). Love numbers for diurnal tides: Relation to wobble admittances and resonance expansions. Journal of Geophysical Research, 100, 9935—9948. https://doi.org/10.1029/95JB00670.
Melchior, P. (1966). The Earth tides. Pergamon Press, 458 p.
Nakano, S. (1963). The effect of surface temperature on the crustal deformations. Bulletins of the Disaster Prevention Research Institute, Kyoto University, 60, 6—15.
Peltier, A., Beauducel, F., Staudacher, T., Catherine, Ph., & Kowalski, Ph. (2016). Contribution of tiltmeters and extensometers to monitor piton de la fournaise activity. In P. Bachelery, J.F. Lenat, A. Di Muro, L. Michon (Eds.), Active Volcanoes of the Southwest Indian Ocean (pp. 287—303). https://doi.org/10.1007/978-3-642-31395-0_17.
Petrosino, S., Ricco, C., De Lauro, E., Aquino, I., & Falanga, M. (2020). Time evolution of medium and long-period ground tilting at Campi Flegrei caldera. Advances in Geosciences, 52, 9—17. https://doi.org/10.5194/adgeo-52-9-2020.
Schueller, K. (2015). Theoretical basis for Earth Tide analysis with the new ETERNA34-ANA-V4.0 program. Marees Terrestres Bulletin d’Informations, 149, 12024—12061.
Schwiderski, E.W. (1980). On charting Global Ocean Tides. Reviews of Geophysics, 18(1), 243—268. https://doi.org/10.1029/RG018i001 p00243.
Sun, H., Braitenberg, C., Feng, W., & Cui, X. (2023). A review of the 19th International Symposium on geodynamics and earth tide, Wuhan 2021. Geodesy and Geodynamics, 14(1), 4—14. https://doi.org/10.1016/j.geog.2022.11.003.
Varga, P., & Grafarend, E. (2018). Influence of Tidal Forces on the Triggering of Seismic Events. Pure and Applied Geophysics, 175(1), 1649—1657. https://doi.org/10.1007/s00024-017-1563-5.
Venedikov, A.P. (1966). Une methode pour l’analyse des marees terrestres a partir d’enregistrements de longueur arbitraire. Bulletins de l’Académie Royale de Belgique, 52, 463—485.
Wahr, J.M. (1981). Body tides on an elliptical, rotating, elastic, and oceanless Earth. Geophysical Journal International, 64(3), 677—703. https://doi.org/10.1111/j.1365-246X.1981.tb02690.x.
Wenzel, H.G. (1996). The Nanogal Software: Earth Tide Data Processing Package: ETERNA 3.3. Marees Terrestres Bulletin d’Informations, 124, 9425—9439.
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