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Journal articles on the topic 'Earth tides'

Author: Grafiati

Published: 4 June 2021

Last updated: 21 September 2024

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1

Gemael, Camil. "Earth Tides in Brazil." Zentralblatt für Geologie und Paläontologie, Teil I 1985, no. 9-10 (1986): 1495–500. http://dx.doi.org/10.1127/zbl_geol_pal_1/1985/1986/1495.

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2

Kuo, John T. "Earth tides." Reviews of Geophysics 25, no. 5 (1987): 847. http://dx.doi.org/10.1029/rg025i005p00847.

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3

Levin, B. W., and E. V. Sasorova. "Seismotectonics and Earth tides." Russian Journal of Pacific Geology 6, no. 1 (2012): 70–77. http://dx.doi.org/10.1134/s1819714012010095.

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4

Agnew, Duncan C. "Time and tide: pendulum clocks and gravity tides." History of Geo- and Space Sciences 11, no. 2 (2020): 215–24. http://dx.doi.org/10.5194/hgss-11-215-2020.

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Abstract. Tidal fluctuations in gravity will affect the period of a pendulum and hence the timekeeping of any such clock that uses one. Since pendulum clocks were, until the 1940s, the best timekeepers available, there has been interest in seeing if tidal effects could be observed in the best performing examples of these clocks. The first such observation was in 1929, before gravity tides were measured with spring gravimeters; at the time of the second (1940–1943), such gravimeters were still being developed. Subsequent observations, having been made after pendulum clocks had ceased to be the

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5

Goring, Derek G., and Roy A. Walters. "Ocean‐tide loading and Earth tides around New Zealand." New Zealand Journal of Marine and Freshwater Research 36, no. 2 (2002): 299–309. http://dx.doi.org/10.1080/00288330.2002.9517087.

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6

Dehant, V., P. Defraigne, and J. M. Wahr. "Tides for a convective Earth." Journal of Geophysical Research: Solid Earth 104, B1 (1999): 1035–58. http://dx.doi.org/10.1029/1998jb900051.

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7

Auclair-Desrotour, P., J. Laskar, and S. Mathis. "Atmospheric tides in Earth-like planets." Astronomy & Astrophysics 603 (July 2017): A107. http://dx.doi.org/10.1051/0004-6361/201628252.

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Context. Atmospheric tides can strongly affect the rotational dynamics of planets. In the family of Earth-like planets, which includes Venus, this physical mechanism coupled with solid tides makes the angular velocity evolve over long timescales and determines the equilibrium configurations of their spin. Aims. Unlike the solid core, the atmosphere of a planet is subject to both tidal gravitational potential and insolation flux coming from the star. The complex response of the gas is intrinsically linked to its physical properties. This dependence has to be characterized and quantified for app

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8

Vieira, R. "Xth International Symposium on Earth Tides." Bulletin Géodésique 61, no. 2 (1987): 201–2. http://dx.doi.org/10.1007/bf02521269.

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9

Bai, Yanzhuo, Shengwen Chang, and Shangcheng Wu. "Relationship Between Earth-Moon Distance and Tides." Highlights in Science, Engineering and Technology 85 (March 13, 2024): 286–92. http://dx.doi.org/10.54097/xkxh4q35.

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For residents and fishermen in coastal cities, tidal phenomena are a dangerous existence, and for tidal power stations, tidal phenomena will bring clean energy to them. For the formation of tidal phenomena, the most closely related is the distance between the Earth and the Moon. Therefore, this paper collects the tides and Earth-Moon records in New York in 2022, and performs data visualization operations on the data, and uses STL (Seasonal Decomposition of Time Series), MSTL (Multiple Seasonal-Trend Decomposition using Loess) models to predict, so as to explore the concern between the Earth-Mo

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10

Navarro, Thomas, Timothy M. Merlis, Nicolas B. Cowan, and Natalya Gomez. "Atmospheric Gravitational Tides of Earth-like Planets Orbiting Low-mass Stars." Planetary Science Journal 3, no. 7 (2022): 162. http://dx.doi.org/10.3847/psj/ac76cd.

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Abstract Temperate terrestrial planets orbiting low-mass stars are subject to strong tidal forces. The effects of gravitational tides on the solid planet and that of atmospheric thermal tides have been studied, but the direct impact of gravitational tides on the atmosphere itself has so far been ignored. We first develop a simplified analytic theory of tides acting on the atmosphere of a planet. We then implement gravitational tides into a general circulation model of a static-ocean planet in a short-period orbit around a low-mass star—the results agree with our analytic theory. Because atmosp

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11

Bogusz, J. "Environmental Influences on Gravimetric Earth Tides Observations." Artificial Satellites 42, no. 1 (2007): 41–57. http://dx.doi.org/10.2478/v10018-007-0016-2.

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Environmental Influences on Gravimetric Earth Tides Observations The following article presents the results of the adjustment (by means of the classical least squares method) of 3-year series of gravimetric Earth tides observations recorded in Observatory at Jozefoslaw (Józefosław - Poland) using LaCoste&Romberg model ET-26 gravimeter. The set of atmospheric data (pressure, temperature and humidity) has been taken into account in the analysis. Several models of ocean's tides were compared to find out how large the indirect effect in Jozefoslaw is. Hydrological observations were made parall

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12

REDDY, S. JEEV ANANDA. "Lunar tides in earth current at Barrow." MAUSAM 23, no. 3 (2022): 407–10. http://dx.doi.org/10.54302/mausam.v23i3.5297.

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The lunar tides in earth current (viz., Telluric current) at Barrow (71° 18'N, 156°47'W) have been studied by using hourly values of N-S and E-W components for the period 1963-1965 and 1961-1962, respectively. The study shows that significant results can be obtained from data for even short periods of Telluric current. Further it has been found that there is good agreement between lunar semi-diurnal oscillations in earth currents (studied by Egedal and Rougerie) and Telluric current (present study).

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13

Stavinschi, M., and M. Souchay. "Some correlations between earthquakes and Earth tides." Acta Geodaetica et Geophysica Hungarica 38, no. 1 (2003): 77–92. http://dx.doi.org/10.1556/ageod.38.2003.1.10.

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14

Saleh, Bassam. "Study of Earth Tides Using Quartz Tiltmeter." Journal of Surveying Engineering 129, no. 2 (2003): 51–55. http://dx.doi.org/10.1061/(asce)0733-9453(2003)129:2(51).

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15

Hsu, H. T. "The 11th International Symposium on Earth Tides." Bulletin Géodésique 64, no. 1 (1990): 109–10. http://dx.doi.org/10.1007/bf02530618.

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16

Zharov, V. E., and D. Gambis. "Atmospheric tides and rotation of the Earth." Journal of Geodesy 70, no. 6 (1996): 321–26. http://dx.doi.org/10.1007/bf00868183.

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17

Zharov, V. E., and D. Gambis. "Atmospheric tides and rotation of the Earth." Journal of Geodesy 70, no. 6 (1996): 321–26. http://dx.doi.org/10.1007/s001900050022.

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18

Su, Yongkang. "The influence of the Sun, Moon and Earth Tides." Theoretical and Natural Science 31, no. 1 (2024): 149–53. http://dx.doi.org/10.54254/2753-8818/31/20241155.

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Tidal phenomena, a ubiquitous spectacle along coastlines, have captivated human curiosity for centuries. It can be involved in some small activities like fishing on the sea. Also, some big activities like the prediction of the position of the Earth should take the consideration of tides. This paper is aimed to have a summary of the formation and the principles of tides. Then, according to the essential theory, some applications are discussed based on the fields of astrology, geography, and clean energy. The principles of these applications are summarized and concluded into some useful informat

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19

Yurkina, M. I., Z. Šimon, and A. Zeman. "Constant part of the Earth tides in the Earth figure theory." Bulletin Géodésique 60, no. 4 (1986): 339–43. http://dx.doi.org/10.1007/bf02522341.

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20

Gubanov, V. S., and S. L. Kurdubov. "Resonances in solid Earth tides from VLBI observations." Astronomy Letters 41, no. 5 (2015): 232–37. http://dx.doi.org/10.1134/s1063773715050035.

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21

Wang, Chi‐Yuen, Ai‐Yu Zhu, Xin Liao, Michael Manga, and Lee‐Ping Wang. "Capillary Effects on Groundwater Response to Earth Tides." Water Resources Research 55, no. 8 (2019): 6886–95. http://dx.doi.org/10.1029/2019wr025166.

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22

Auclair-Desrotour, P., S. Mathis, J. Laskar, and J. Leconte. "Oceanic tides from Earth-like to ocean planets." Astronomy & Astrophysics 615 (July 2018): A23. http://dx.doi.org/10.1051/0004-6361/201732249.

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Context. Oceanic tides are a major source of tidal dissipation. They drive the evolution of planetary systems and the rotational dynamics of planets. However, two-dimensional (2D) models commonly used for the Earth cannot be applied to extrasolar telluric planets hosting potentially deep oceans because they ignore the three-dimensional (3D) effects related to the ocean’s vertical structure. Aims. Our goal is to investigate, in a consistant way, the importance of the contribution of internal gravity waves in the oceanic tidal response and to propose a modelling that allows one to treat a wide r

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23

Ray, Richard D., and Gary D. Egbert. "Fortnightly Earth rotation, ocean tides and mantle anelasticity." Geophysical Journal International 189, no. 1 (2012): 400–413. http://dx.doi.org/10.1111/j.1365-246x.2012.05351.x.

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24

Wang, Rongjiang. "Effect of Rotation and Ellipticity On Earth Tides." Geophysical Journal International 117, no. 2 (1994): 562–65. http://dx.doi.org/10.1111/j.1365-246x.1994.tb03953.x.

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25

Cochran, E. S. "Earth Tides Can Trigger Shallow Thrust Fault Earthquakes." Science 306, no. 5699 (2004): 1164–66. http://dx.doi.org/10.1126/science.1103961.

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26

Simon, Jacob, Patrick Fulton, Alain Prinzhofer, and Lawrence Cathles. "Earth Tides and H2 Venting in the Sao Francisco Basin, Brazil." Geosciences 10, no. 10 (2020): 414. http://dx.doi.org/10.3390/geosciences10100414.

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Hydrogen gas seeping from Proterozoic basins worldwide is a potential non-carbon energy resource, and the vents are consequently receiving research attention. A curious feature of H2 venting in the Sao Francisco Basin in Brazil is that the venting displays a very regular daily cycle. It has been shown that atmospheric pressure tides could explain this cycle, but solid earth tides might be an alternative explanation. We show here that it is unlikely that solid earth tides are a dominant control because they have two equally strong peaks per day whereas the H2 venting has only one.

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27

Lin, Lei, Hao Liu, Xiaomeng Huang, Qingjun Fu, and Xinyu Guo. "Effect of tides on river water behavior over the eastern shelf seas of China." Hydrology and Earth System Sciences 26, no. 20 (2022): 5207–25. http://dx.doi.org/10.5194/hess-26-5207-2022.

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Abstract. Rivers carry large amounts of freshwater and terrestrial material into shelf seas, which is an important part of the global water and biogeochemical cycles. The earth system model or climate model is an important instrument for simulating and projecting the global water cycle and climate change, in which tides however are commonly removed. For a better understanding of the potential effect of the absence of tides in the simulation of the water cycle, this study compared the results of a regional model with and without considering tides, and evaluated the effect of tides on the behavi

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28

Rau, Gabriel C., Mark O. Cuthbert, R. Ian Acworth, and Philipp Blum. "Technical note: Disentangling the groundwater response to Earth and atmospheric tides to improve subsurface characterisation." Hydrology and Earth System Sciences 24, no. 12 (2020): 6033–46. http://dx.doi.org/10.5194/hess-24-6033-2020.

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Abstract. The groundwater response to Earth tides and atmospheric pressure changes can be used to understand subsurface processes and estimate hydraulic and hydro-mechanical properties. We develop a generalised frequency domain approach to disentangle the impacts of Earth and atmospheric tides on groundwater level responses. By considering the complex harmonic properties of the signal, we improve upon a previous method for quantifying barometric efficiency (BE), while simultaneously assessing system confinement and estimating hydraulic conductivity and specific storage. We demonstrate and vali

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29

de Mello Gallep, Cristiano, and Daniel Robert. "Are cyclic plant and animal behaviours driven by gravimetric mechanical forces?" Journal of Experimental Botany 73, no. 4 (2021): 1093–103. http://dx.doi.org/10.1093/jxb/erab462.

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Abstract The celestial mechanics of the Sun, Moon, and Earth dominate the variations in gravitational force that all matter, live or inert, experiences on Earth. Expressed as gravimetric tides, these variations are pervasive and have forever been part of the physical ecology with which organisms evolved. Here, we first offer a brief review of previously proposed explanations that gravimetric tides constitute a tangible and potent force shaping the rhythmic activities of organisms. Through meta-analysis, we then interrogate data from three study cases and show the close association between the

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30

Dehant, V. "Review of the Earth tidal models and contribution of Earth tides in geodynamics." Journal of Geophysical Research: Solid Earth 96, B12 (1991): 20235–40. http://dx.doi.org/10.1029/91jb01529.

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31

Siwek, Sławomir. "Earth tides and seismic activity in deep coal mining." International Journal of Rock Mechanics and Mining Sciences 148 (December 2021): 104972. http://dx.doi.org/10.1016/j.ijrmms.2021.104972.

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32

Dinger, Florian, Stefan Bredemeyer, Santiago Arellano, Nicole Bobrowski, Ulrich Platt, and Thomas Wagner. "On the link between Earth tides and volcanic degassing." Solid Earth 10, no. 3 (2019): 725–40. http://dx.doi.org/10.5194/se-10-725-2019.

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Abstract. Long-term measurements of volcanic gas emissions conducted during the last decade suggest that under certain conditions the magnitude or chemical composition of volcanic emissions exhibits periodic variations with a period of about 2 weeks. A possible cause of such a periodicity can be attributed to the Earth tidal potential. The phenomenology of such a link has been debated for long, but no quantitative model has yet been proposed. The aim of this paper is to elucidate whether a causal link between tidal forcing and variations in volcanic degassing can be traced analytically. We mod

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33

Burton, Paul W. "Geophysics: Is there coherence between Earth tides and earthquakes?" Nature 321, no. 6066 (1986): 115. http://dx.doi.org/10.1038/321115a0.

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34

Goodkind, John M. "Test of Theoretical Solid Earth and Ocean Gravity Tides." Geophysical Journal International 125, no. 1 (1996): 106–14. http://dx.doi.org/10.1111/j.1365-246x.1996.tb06537.x.

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35

Middlemiss, R. P., A. Samarelli, D. J. Paul, J. Hough, S. Rowan, and G. D. Hammond. "Measurement of the Earth tides with a MEMS gravimeter." Nature 531, no. 7596 (2016): 614–17. http://dx.doi.org/10.1038/nature17397.

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36

Bodri, B., and S. Iizuka. "On the correlation between Earth tides and microseismic activity." Physics of the Earth and Planetary Interiors 55, no. 1-2 (1989): 126–34. http://dx.doi.org/10.1016/0031-9201(89)90238-0.

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37

Métivier, Laurent, Olivier de Viron, Clinton P. Conrad, Stéphane Renault, Michel Diament, and Geneviève Patau. "Evidence of earthquake triggering by the solid earth tides." Earth and Planetary Science Letters 278, no. 3-4 (2009): 370–75. http://dx.doi.org/10.1016/j.epsl.2008.12.024.

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38

Valois, Rémi, Agnès Rivière, Jean-Michel Vouillamoz, and Gabriel C. Rau. "Technical note: Analytical solution for well water response to Earth tides in leaky aquifers with storage and compressibility in the aquitard." Hydrology and Earth System Sciences 28, no. 4 (2024): 1041–54. http://dx.doi.org/10.5194/hess-28-1041-2024.

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Abstract. In recent years, there has been a growing interest in utilizing the groundwater response to Earth tides as a means of estimating subsurface properties. However, existing analytical models have been insufficient in accurately capturing realistic physical conditions. This study presents a new analytical solution to calculate the groundwater response to Earth tide strains, including storage and compressibility of the aquitard, borehole storage, and skin effects. We investigate the effects of aquifer and aquitard parameters on the well water response to Earth tides at two dominant freque

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39

Bos, M. S., T. F. Baker, F. H. Lyard, W. E. Zurn, and P. A. Rydelek. "Long-period lunar Earth tides at the geographic South Pole and recent models of ocean tides." Geophysical Journal International 143, no. 2 (2000): 490–94. http://dx.doi.org/10.1046/j.1365-246x.2000.01260.x.

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40

Issaka, Yakubu, and Bernard Kumi-Boateng. "ARTIFICIAL INTELLIGENCE TECHNIQUES FOR PREDICTING TIDAL EFFECTS BASED ON GEOGRAPHIC LOCATIONS IN GHANA." Geodesy and cartography 46, no. 1 (2020): 1–7. http://dx.doi.org/10.3846/gac.2020.7696.

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Tidal forces as a result of attraction of external bodies (Sun, Moon and Stars) through gravity and are a source of noise in many geoscientific field observations. The solid earth tides cause deformation. This deformation results in displacement in geographic positions on the surface of the earth. The displacement due to tidal effects can result in deformation of engineering structures, loss of lives, and economic cost. Tidal forces also help in detecting other environmental and tectonic signals. This study quantifies the effects of solid earth tides on stationary survey controls in five regio

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41

Becker, Matthew W., and Thomas I. Coleman. "Distributed Acoustic Sensing of Strain at Earth Tide Frequencies." Sensors 19, no. 9 (2019): 1975. http://dx.doi.org/10.3390/s19091975.

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The solid Earth strains in response to the gravitational pull from the Moon, Sun, and other planetary bodies. Measuring the flexure of geologic material in response to these Earth tides provides information about the geomechanical properties of rock and sediment. Such measurements are particularly useful for understanding dilation of faults and fractures in competent rock. A new approach to measuring earth tides using fiber optic distributed acoustic sensing (DAS) is presented here. DAS was originally designed to record acoustic vibration through the measurement of dynamic strain on a fiber op

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42

Cunha, Diana, Alexandre C. M. Correia, and Jacques Laskar. "Spin evolution of Earth-sized exoplanets, including atmospheric tides and core–mantle friction." International Journal of Astrobiology 14, no. 2 (2014): 233–54. http://dx.doi.org/10.1017/s1473550414000226.

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AbstractPlanets with masses between 0.1 and 10 M⊕ are believed to host dense atmospheres. These atmospheres can play an important role on the planet's spin evolution, since thermal atmospheric tides, driven by the host star, may counterbalance gravitational tides. In this work, we study the long-term spin evolution of Earth-sized exoplanets. We generalize previous works by including the effect of eccentric orbits and obliquity. We show that under the effect of tides and core–mantle friction, the obliquity of the planets evolves either to 0° or 180°. The rotation of these planets is also expect

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43

Chen, L., J. G. Chen, and Q. H. Xu. "Correlations between solid tides and worldwide earthquakes <i>M</i><sub>S</sub> ≥ 7.0 since 1900." Natural Hazards and Earth System Sciences 12, no. 3 (2012): 587–90. http://dx.doi.org/10.5194/nhess-12-587-2012.

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Abstract. Most studies on the correlations between earthquakes and solid tides mainly concluded the syzygies (i.e. new or full moons) of each lunar cycle have more earthquakes than other days in the month. We show a correlation between the aftershock sequence of the ML = 6.3 Christchurch, New Zealand, earthquake and the diurnal solid tide. Ms ≥ 7 earthquakes worldwide since 1900 are more likely to occur during the 0°, 90°, 180° or 270° phases (i.e. earthquake-prone phases) of the semidiurnal solid earth tidal curve (M2). Thus, the semidiurnal solid tides triggers earthquakes. However, the long

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44

Englich, Sigrid, Harald Schuh, and Robert Weber. "Short-term tidal variations in UT1: compliance between modelling and observation." Proceedings of the International Astronomical Union 5, H15 (2009): 215. http://dx.doi.org/10.1017/s1743921310008847.

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AbstractThe Earth rotation rate and consequently universal time (UT1) and length of day (LOD) are periodically affected by solid Earth tides and oceanic tides. Solid Earth tides induce changes with periods from around 5 days to 18.6 years, with the largest amplitudes occurring at fortnightly, monthly, semi-annual and annual periods, and at 18.6 years. The principal variations caused by oceanic tides have diurnal and semi-diurnal periods. For the investigation of the tidal effects with periods of up to 35 days, UT1 series are estimated from VLBI observation data of the time interval 1984–2008.

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45

Hart-Davis, Michael G., Denise Dettmering, Roman Sulzbach, Maik Thomas, Christian Schwatke, and Florian Seitz. "Regional Evaluation of Minor Tidal Constituents for Improved Estimation of Ocean Tides." Remote Sensing 13, no. 16 (2021): 3310. http://dx.doi.org/10.3390/rs13163310.

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Satellite altimetry observations have provided a significant contribution to the understanding of global sea surface processes, particularly allowing for advances in the accuracy of ocean tide estimations. Currently, almost three decades of satellite altimetry are available which can be used to improve the understanding of ocean tides by allowing for the estimation of an increased number of minor tidal constituents. As ocean tide models continue to improve, especially in the coastal region, these minor tides become increasingly important. Generally, admittance theory is used by most global oce

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46

Brosche, P. "Oceanic Influences on the Angular Velocity of the Earth." Symposium - International Astronomical Union 141 (1990): 156. http://dx.doi.org/10.1017/s0074180900086617.

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Hydrodynamical computations of the major partial tides in the oceans have been evaluated for the changes both in moment of inertia and relative angular momentum due to ocean currents. If the system solid Earth plus oceans is seen as an isolated system for these time scales, the oceanic variations lead to mirror-like changes in the rotation of the solid Earth. Amplitudes are of the order of 0.1 ms in Universal time. In contrast to the effects of solid Earth tide, phases are away from equilibrium phases.

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47

Al Mohit, Md Abdul, Md. Towhiduzzaman, and Mst Rabiba Khatun. "Development of A Novel Conceptual and Calculative Method for the Prediction of Tide within the Bay of Bengal." European Journal of Mathematics and Statistics 3, no. 4 (2022): 54–61. http://dx.doi.org/10.24018/ejmath.2022.3.4.134.

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Ebb and flow of seawater at regular intervals under the influence of gravitational forces from outside the earth is called tides. This study sheds light on how to measure tides through a new kind of innovative method. This method can be used to measure tides at new locations based on a known tide station. Some parameters play an important role in measuring tides, such as datum information, mean sea level (MSL), mean high water springs (MHWS), mean low water springs (MLWS) and so on. This fancy method is a computational process that relies on observable data and other factors. This innovative m

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48

Hsieh, Paul A., John D. Bredehoeft, and Stuart A. Rojstaczer. "Response of well aquifer systems to Earth tides: Problem revisited." Water Resources Research 24, no. 3 (1988): 468–72. http://dx.doi.org/10.1029/wr024i003p00468.

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49

Xu, Jianqiao, Heping Sun, and Bernard Ducarme. "A global experimental model for gravity tides of the Earth." Journal of Geodynamics 38, no. 3-5 (2004): 293–306. http://dx.doi.org/10.1016/j.jog.2004.07.003.

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50

Sato, T., S. Miura, Y. Ohta, et al. "Earth tides observed by gravity and GPS in southeastern Alaska." Journal of Geodynamics 46, no. 3-5 (2008): 78–89. http://dx.doi.org/10.1016/j.jog.2008.03.004.

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