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Journal articles on the topic 'Earth's rotation'

Author: Grafiati

Published: 10 March 2023

Last updated: 31 July 2025

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1

Arma Fuziah, Clarissa Oktoferin Sinaga, Mita Nasalisa Br Barus, Sri Andini, Widya Khairunisa, and Elsa Kardiana. "Analisis Pengaruh Rotasi Bumi terhadap Perbedaan Waktu dan Iklim Antar Wilayah." SOSIAL : Jurnal Ilmiah Pendidikan IPS 3, no. 3 (2025): 20–29. https://doi.org/10.62383/sosial.v3i3.975.

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Understanding of the Earth's rotation is often limited to the alternation of day and night. However, its impact is far more complex, including the formation of time zones and varying climate patterns. The objectives of this study include analyzing the Earth's rotation's influence on the formation of time differences between regions based on longitude and the relationship between the Earth's rotation and climate variations caused by atmospheric movement and global wind patterns. This study employs literature review techniques using secondary data, which involves collecting data indirectly by st

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2

Wahr, J. M. "The Earth's Rotation." Annual Review of Earth and Planetary Sciences 16, no. 1 (1988): 231–49. http://dx.doi.org/10.1146/annurev.ea.16.050188.001311.

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3

HIDE, R., and J. O. DICKEY. "Earth's Variable Rotation." Science 253, no. 5020 (1991): 629–37. http://dx.doi.org/10.1126/science.253.5020.629.

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4

Brumberg, Victor A., and Tamara V. Ivanova. "A supplementary note on constructing the general Earth's rotation theory." Proceedings of the International Astronomical Union 9, S310 (2014): 13–16. http://dx.doi.org/10.1017/s1743921314007716.

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AbstractRepresenting a post-scriptum supplementary to a previous paper of the authors Brumberg & Ivanova (2011) this note aims to simplify the practical development of the Earth's rotation theory, in the framework of the general planetary theory, avoiding the non–physical secular terms and involving the separation of the fast and slow angular variables, both for planetary–lunar motion and Earth's rotation. In this combined treatment of motion and rotation, the fast angular terms are related to the mean orbital longitudes of the bodies, the diurnal and Euler rotations of the Earth. The slow

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5

Volland, Hans. "Atmosphere and Earth's rotation." Surveys in Geophysics 17, no. 1 (1996): 101–44. http://dx.doi.org/10.1007/bf01904476.

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6

Hide, R. "Flactuations in the earth's rotation and earth's deep interior." Physics of the Earth and Planetary Interiors 62, no. 1-2 (1990): 3. http://dx.doi.org/10.1016/0031-9201(90)90187-3.

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7

Sun, Jinyi, Weining Wang, and Dandan Zhao. "Global existence of 3D rotating magnetohydrodynamic equations arising from Earth's fluid core." Networks and Heterogeneous Media 20, no. 1 (2025): 35–51. https://doi.org/10.3934/nhm.2025003.

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<p>The paper is concerned with the three-dimensional magnetohydrodynamic equations in the rotational framework concerning with fluid flow of Earth's core and the variation of the Earth's magnetic field. By establishing new balances between the regularizing effects arising from viscosity dissipation and magnetic diffusion with the dispersive effects caused by the rotation of the Earth, we obtain the global existence and uniqueness of solutions of the Cauchy problem of the three-dimensional rotating magnetohydrodynamic equations in Besov spaces. Moreover, the spatial analyticity of solutio

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8

Lee, S. P. "Lee:-Effect of Earth's Rotation." Bulletin of the Geological Society of China 23, no. 3-4 (2009): 173–84. http://dx.doi.org/10.1111/j.1755-6724.1943.mp233-4009.x.

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9

Sonett, C. "Historical eclipses and earth's rotation." Eos, Transactions American Geophysical Union 79, no. 14 (1998): 175. http://dx.doi.org/10.1029/98eo00130.

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10

Mazzarella, A., and A. Palumbo. "Earth's Rotation and Solar Activity." Geophysical Journal International 97, no. 1 (1989): 169–71. http://dx.doi.org/10.1111/j.1365-246x.1989.tb00492.x.

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11

Chao, B. F., D. N. Dong, H. S. Liu, and T. A. Herring. "Libration in the Earth's rotation." Geophysical Research Letters 18, no. 11 (1991): 2007–10. http://dx.doi.org/10.1029/91gl02491.

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12

Maddox, John. "Earthquakes and the Earth's rotation." Nature 332, no. 6159 (1988): 11. http://dx.doi.org/10.1038/332011a0.

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13

Soffel, Michael, and Sergei A. Klioner. "Relativistic aspects of Earth's rotation." Proceedings of the International Astronomical Union 2, no. 14 (2006): 469. http://dx.doi.org/10.1017/s1743921307011441.

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14

Maddox, John. "Weather and the Earth's rotation." Nature 346, no. 6285 (1990): 605. http://dx.doi.org/10.1038/346605a0.

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15

Stephenson, F. Richard. "Historical eclipses and Earth's rotation." Astronomy and Geophysics 44, no. 2 (2003): 2.22–2.27. http://dx.doi.org/10.1046/j.1468-4004.2003.44222.x.

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16

Levin, B. W., E. V. Sasorova, V. B. Gurianov, and V. V. Yarmolyuk. "The relationship between global volcanic activity and variations in the velocity of Earth's rotation." Доклады Академии наук 484, no. 6 (2019): 729–33. http://dx.doi.org/10.31857/s0869-56524846729-733.

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Analysis of observations of the Earth's rotational velocity and volcanic activity of the planet from 1720 until 2015 suggests that higher volcanic activity temporally coincided with periods of decreased angular velocity of Earth's rotation (deceleration), and, vice versa, lower volcanic activity coincided with the periods of increased velocity of the Earth's rotation (acceleration). Our analysis employed the data from the catalog by the Smithsonian Institute, United States, in which each volcanic explosion had its own determined value of the Volcanic Explosivity Index (VEI). The total number o

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17

Lambeck, Kurt. "The Earth's variable rotation: some geophysical causes." Symposium - International Astronomical Union 128 (1988): 1–20. http://dx.doi.org/10.1017/s0074180900119199.

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The Earth's variable rotation, its departures from what it would be if it were a rigid body rotating in isolation, has occupied the interest of astronomers and geophysicists for more than 100 years. The reason for this is quite clear when one becomes aware of the range of processes that perturb the Earth from uniform rotation (Figure 1). A complete understanding of the driving mechanisms requires a study of the deformation of the solid Earth, of fluid motions in the core and the magnetic field, of the mass redistributions and motions within the oceans and atmosphere, and of the interactions be

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18

Malkin, Z. M. "Large Analysis of progress in improving the prediction accuracy of Earth's rotation parameters in Russian and international EOP services during last 16 years." Publications of the Pulkovo Observatory 231 (December 2023): 31–36. http://dx.doi.org/10.31725/0367-7966-2023-231-4.

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The paper analyzes the real predictions of the Earth's rotation parameters (ERP) made in the Russian State Service of the Earth's Rotation (the Center for processing and analyzing data on the parameters of the Earth's rotation of the Main Metrological Center of the State Service of Time, Frequency and Determination of the Parameters of the Earth's Rotation, SSTF) and the International Earth Rotation and Reference Systems Service (IERS) in 2007--2023. Daily predictions of the Earth's Pole coordinates and Universal Time were considered. In total, 6021 SSTF predictions and 5684 IERS predictions w

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19

de Verdière, A. Colin, and R. Schopp. "Flows in a rotating spherical shell: the equatorial case." Journal of Fluid Mechanics 276 (October 10, 1994): 233–60. http://dx.doi.org/10.1017/s0022112094002545.

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It is well known that the widely used powerful geostrophic equations that single out the vertical component of the Earth's rotation cease to be valid near the equator. Through a vorticity and an angular momentum analysis on the sphere, we show that if the flow varies on a horizontal scale L smaller than (Ha)1/2 (where H is a vertical scale of motion and a the Earth's radius), then equatorial dynamics must include the effect of the horizontal component of the Earth's rotation. In equatorial regions, where the horizontal plane aligns with the Earth's rotation axis, latitudinal variations of plan

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20

Chao, Benjamin F., WeiYung Chung, ZongRong Shih, and YiKai Hsieh. "Earth's rotation variations: a wavelet analysis." Terra Nova 26, no. 4 (2014): 260–64. http://dx.doi.org/10.1111/ter.12094.

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21

Jackson, Andy. "A new turn for Earth's rotation." Nature 465, no. 7294 (2010): 39–40. http://dx.doi.org/10.1038/465039a.

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22

WEBB, D. J. "Earth's Rotation from Eons to Days." Geophysical Journal International 105, no. 3 (1991): 807–8. http://dx.doi.org/10.1111/j.1365-246x.1991.tb00817.x.

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23

Brosche, P. "The oceans and the Earth's rotation." Symposium - International Astronomical Union 128 (1988): 349–52. http://dx.doi.org/10.1017/s0074180900119710.

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In the long run, the tidal interaction between the Moon and the solid Earth is mediated by the oceans. It produces the retardation of the Earth's rotation known as ‘tidal friction’. Due to the changing configuration of the continents, it is a non-monotonic function of time. Tides of the solid Earth dominate the short-periodic tidal effects while the exchange with the atmosphere is preponderant in climatic changes, especially with an annual signature. It is shown that the influences of the oceans within such short time-scales must be taken into account for tidal and for non-tidal variations as

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24

Sidorenkov, N. S. "Physics of the Earth's rotation instabilities." Astronomical & Astrophysical Transactions 24, no. 5 (2005): 425–39. http://dx.doi.org/10.1080/10556790600593506.

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25

Oman, H. "Magnetic braking of the Earth's rotation." IEEE Aerospace and Electronic Systems Magazine 4, no. 4 (1989): 3–10. http://dx.doi.org/10.1109/62.24888.

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26

Souriau, A. "EARTH'S INNER CORE:Is the Rotation Real?" Science 281, no. 5373 (1998): 55–56. http://dx.doi.org/10.1126/science.281.5373.55.

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27

Wilson, C. R. "GEOPHYSICS:Oceanic Effects on Earth's Rotation Rate." Science 281, no. 5383 (1998): 1623–24. http://dx.doi.org/10.1126/science.281.5383.1623.

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28

Jochmann, H., and H. Greiner-Mai. "Climate variations and the earth's rotation." Journal of Geodynamics 21, no. 2 (1996): 161–76. http://dx.doi.org/10.1016/0264-3707(95)00030-5.

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29

Van Zanten, Leonard. "Earth's journey." JOURNAL OF ADVANCES IN PHYSICS 12, no. 1 (2016): 4197–203. http://dx.doi.org/10.24297/jap.v12i1.174.

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In the beginning the earth was flat and no one was to prove that it was round, but with the advent in science this is now quite obvious. Â But no less obvious will be the fact that the earth has its seasons due to a rotation of precession rather than the fixed immovable position that current science has given it.Â And that in a manner of speaking the earth, like unto the moon orbiting the earth, also appears to have a single period of rotation for each orbital period that it makes around the sun.The earth thus for each single orbit around the sun makes one full turn of precession which gives i

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30

Tissen, Viktor M. "FORECAST OF TEMPERATURE ANOMALIES IN EUROPE AND RUSSIA BY THEIR CORRELATION WITH CHANGES IN THE EARTH'S ROTATION SPEED." Interexpo GEO-Siberia 8, no. 2 (2020): 31–37. http://dx.doi.org/10.33764/2618-981x-2020-8-2-31-37.

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The article provides information about the relationship between changes in the global temperature on the Earth and variations in the speed of its rotation. Special attention is paid to the study of the correlation between the onset of abnormal warm and cold winters of the Eurasian continent and sharp changes in the Earth's rotation speed. It been observed, that during periods of rapid deceleration in the 20th and 21st century, there were abnormally cold winters, and during periods of acceleration, abnormally warm ones. Thus, the periods of acceleration and deceleration of the Earth's rotation

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31

Borisov, Mirko, Miro Govedarica, and Maja Orihan. "Rotation of Earth and Determination of Earth Orientation Parameters." Geodetski glasnik, no. 46 (December 31, 2015): 75–90. http://dx.doi.org/10.58817/2233-1786.2015.49.46.75.

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Earth's rotation and elements of the Earth's orientation, with emphasis on the determination of the parameters of the Earth's orientation were described. The technique that was used for the determination of the parameters is called very long baseline interferometry, VLBI. After determining the parameters of the Earth's orientation, the obtained results were compared using different reference frames, and the factors that have influence on their changes were also analyzed. For comparison were used vievstTrf and vtrf2008 reference frames. Data processing is performed in software VieVS (Vienna VLB

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32

Souza, A. J. "On the use of the Stokes number to explain frictional tidal dynamics and water column structure in shelf seas." Ocean Science 9, no. 2 (2013): 391–98. http://dx.doi.org/10.5194/os-9-391-2013.

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Abstract. In recent years coastal oceanographers have suggested using the "Strouhal" number or its inverse, the "Stokes" number, to describe the effect of bottom boundary layer turbulence on the vertical structure of both density and currents. These are defined as the ratios of the frictional depth (δ) to the water column depth (h) or vice versa. Although many researchers have mentioned that the effects of the earth's rotation should be important, they have tended to omit it. Rotation may have an important influence on tidal currents, as the frictional depth from a fully cyclonic to a fully an

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33

Cazenave, Anny, Julia Pfeffer, Mioara Mandea, and Veronique Dehant. "ESD Ideas: A 6-year oscillation in the whole Earth system?" Earth System Dynamics 14, no. 4 (2023): 733–35. http://dx.doi.org/10.5194/esd-14-733-2023.

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Abstract. An oscillation of about 6 years has been reported in Earth's fluid core motions, magnetic field, rotation, and crustal deformations. Recently, a 6-year cycle has also been detected in several climatic parameters (e.g., sea level, surface temperature, precipitation, land hydrology, land ice, and atmospheric angular momentum). Here, we suggest that the 6-year oscillations detected in the Earth's deep interior, rotation, and climate are linked together and that the core processes previously proposed as drivers of the 6-year cycle in the Earth's rotation additionally cause the atmosphere

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34

ANTONOV, V. A. "HORIZONTAL ROTATION OF DEFORMED ELEMENTS OF THE EARTH'S SURFACE." News of the Tula state university. Sciences of Earth 3, no. 1 (2023): 380–94. http://dx.doi.org/10.46689/2218-5194-2023-3-1-380-394.

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The structural composition and properties of the horizontal rotation of the elements of the Earth's surface, which is part of the skew-symmetric part of the geomechanical distortion tensor, are investigated. It is established that it consists of a real rotation, showing the rotation of a deformed area element in geospatial space, and a virtual one, displaying its artificial rotation. The decomposition of angular deformations into components leading to real and virtual rotation, as well as the calculation of their angles, is carried out according to the presented nomogram and the formulas attac

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35

BOOK, DAVID L., and J. A. VALDIVIA. "Viscous drag and the differential rotation of the Earth's core." Journal of Plasma Physics 57, no. 1 (1997): 231–33. http://dx.doi.org/10.1017/s002237789600534x.

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It is proposed that the differential rotation of the Earth's inner core deduced by Song and Richards is due to a combination of the deceleration of the Earth's rotation and the viscous drag between the Earth's inner and outer cores. If this model is correct then the dynamic viscosity in the outer core of the Earth can be estimated to be μ≈104 poise. Besides providing a novel way of determining the viscosity of the core, this simple model suggests some new tests and shows how astronomical effects can influence geological phenomena.

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36

Capitaine, Nicole. "Models and nomenclature in Earth rotation." Proceedings of the International Astronomical Union 5, S261 (2009): 69–78. http://dx.doi.org/10.1017/s1743921309990172.

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AbstractThe celestial Earth's orientation is required for many applications in fundamental astronomy and geodesy; it is currently determined with sub-milliarcsecond accuracy by astro-geodetic observations. Models for that orientation rely on solutions for the rotation of a rigid Earth model and on the geophysical representation of non-rigid Earth effects. Important IAU 2000/2006 resolutions on reference systems have been passed (and endorsed by the IUGG) that recommend a new paradigm and high accuracy models to be used in the transformation from terrestrial to celestial systems. This paper rev

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37

Ostřihanský, L. "Earth's rotation variations and earthquakes 2010–2011." Solid Earth Discussions 4, no. 1 (2012): 33–130. http://dx.doi.org/10.5194/sed-4-33-2012.

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Abstract. In contrast to unsuccessful searching (lasting over 150 years) for correlation of earthquakes with biweekly tides, the author found correlation of earthquakes with sidereal 13.66 days Earth's rotation variations expressed as length of a day (LOD) measured daily by International Earth's Rotation Service. After short mention about earthquakes M 8.8 Denali Fault Alaska 3 November 2002 triggered on LOD maximum and M 9.1 Great Sumatra earthquake 26 December 2004 triggered on LOD minimum and the full Moon, the main object of this paper are earthquakes of period 2010–June 2011: M 7.0 Haiti

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38

Richards, P. G. "Detecting Possible Rotation of Earth's Inner Core." Science 282, no. 5392 (1998): 1227a—1227. http://dx.doi.org/10.1126/science.282.5392.1227a.

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39

Dickman, S. R. "Dynamic Ocean-Tide Effects On Earth's Rotation." Geophysical Journal International 112, no. 3 (1993): 448–70. http://dx.doi.org/10.1111/j.1365-246x.1993.tb01180.x.

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40

Glatzmaier, G. A., and P. H. Roberts. "Rotation and Magnetism of Earth's Inner Core." Science 274, no. 5294 (1996): 1887–91. http://dx.doi.org/10.1126/science.274.5294.1887.

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41

DRAAD, A. A., and F. T. M. NIEUWSTADT. "The Earth's rotation and laminar pipe flow." Journal of Fluid Mechanics 361 (April 25, 1998): 297–308. http://dx.doi.org/10.1017/s0022112098008702.

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A pipe flow facility with a length of 32 m and a diameter of 40 mm has been designed in which a laminar flow of water can be maintained for Reynolds numbers up to 60 000. Velocity measurements taken in this facility show an asymmetric velocity profile both in the vertical as well as horizontal direction with velocities that deviate strongly from the parabolic Hagen–Poiseuille profile. The cause of this asymmetry is traced back to the influence of the Earth's rotation. This is confirmed by means of a comparison of the experimental data with the results from a perturbation solution and from a nu

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42

Stacey, F. D. "Tidal friction and the Earth's rotation, II." Tectonophysics 115, no. 3-4 (1985): 355–56. http://dx.doi.org/10.1016/0040-1951(85)90149-0.

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43

Melchior, P. "Tidal friction and the Earth's rotation, II." Marine Geology 65, no. 1-2 (1985): 195–97. http://dx.doi.org/10.1016/0025-3227(85)90055-6.

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44

Mörner, Nils-Axel. "Trans-polar vgp shifts and earth's rotation." Geophysical & Astrophysical Fluid Dynamics 60, no. 1-4 (1991): 149–55. http://dx.doi.org/10.1080/03091929108220000.

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45

Merriam, J. B. "Tidal friction and the Earth's Rotation, II." Sedimentary Geology 44, no. 1-2 (1985): 174–75. http://dx.doi.org/10.1016/0037-0738(85)90039-9.

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46

Levin, B., A. Domanski, and E. Sasorova. "Zonal concentration of some geophysical process intensity caused by tides and variations in the Earth's rotation velocity." Advances in Geosciences 35 (January 6, 2014): 137–44. http://dx.doi.org/10.5194/adgeo-35-137-2014.

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Abstract. We analyzed what kind of fundamental physical phenomena can be responsible for the generation of the anomalous latitudinal zones of the seismic activity, and the hotspots, and some other geophysical processes. The assessment of tidal effect contribution to the earthquake preparation process is discussed. A disk model of the Earth's rotation was proposed. The model is acceptable for the homogeneous Earth and for the heterogeneous one. The disk model explains the nucleation of two maximums of the gradient of the moment of inertia over latitude with respect to the Equator. Effects of th

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47

Sasorova, Elena, and Boris Levin. "Relationship between Seismic Activity and Variations in the Earth’s Rotation Angular Velocity." Journal of Geography and Geology 10, no. 2 (2018): 43. http://dx.doi.org/10.5539/jgg.v10n2p43.

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The Earth's seismic activity (SA) demonstrates a distinct unevenness both in space and in time. The periods of intensification of seismic activity are followed by periods of its decline. In this work, an attempt was first made to determine the effect of low-frequency components of the variations in the angular velocity of the Earth's rotation (AVER) on the dynamics of its seismic activity (for 1720 – 2017). Analysis of the time series of the density of seismic events and variations in the Earth's rotation velocity of about 300 years shows that each stage of reducing the angular velocity of rot

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48

Tian, Wei. "On tidal tilt corrections to large ring laser gyroscope observations." Geophysical Journal International 196, no. 1 (2013): 189–93. http://dx.doi.org/10.1093/gji/ggt415.

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Abstract With the fast development of the large ring laser gyroscope (RLG) technology in the last decades, promising applications in geophysics and geodesy (e.g. observations of high-frequency variations of Earth's rotation, Earth's tide tilt and seismic waves) have been realized by various groups with currently running large RLGs. In this letter, we point out that in a large number of previous tilt correction models a significant term is missing. This term is related with the Shida number l2 (called l2-term in the following) and has a contribution, which is comparable with that from high-freq

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49

Brumberg, V. A. "Earth Rotation Velocity in Relation with Different Reference Frames." Symposium - International Astronomical Union 166 (1995): 293. http://dx.doi.org/10.1017/s0074180900228222.

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The high precision of present observations makes it reasonable to clear up a question about GRT (general relativity theory) corrections in the problem of Earth's rotation. The answer is that one may almost forget about GRT corrections when dealing in an adequate reference system (RS). The problem of Earth's rotation may be related to the relativistic hierarchy of RS started in (Brumberg and Kopejkin, 1989) and completed in (Klioner, 1993). Let letters B, G and T be related to barycentric, geocentric and topocentric RS, respectively. Let DRS and KRS be dynamically nonrotating or kinematically n

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50

Goldstein, S. J. ,. Jr. "On the slow changes in the earth's rotation." Astronomical Journal 90 (September 1985): 1900. http://dx.doi.org/10.1086/113894.

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