Theory of tides - wikipedia Theory of tides Fourier transform of tides measured at Ft. Pulaski in 2012. Data downloaded from http://tidesandcurrents.noaa.gov/datums.html?id=8670870 Fourier transform computed with https://sourceforge.net/projects/amoreaccuratefouriertransform/ `` The greater circle represents the orbit of the Earth around the Sun... while the smaller one is the rotating Earth itself '' ( Palmeri 1998, p. 229 ). The theory of tides is the application of continuum mechanics to interpret and predict the tidal deformations of planetary and satellite bodies and their atmospheres and oceans ( especially Earth 's Ocean ) under the gravitational loading of another astronomical body or bodies ( especially the Moon ). Contents 1 Kepler 2 Galileo 's attempt to explain the tides 3 Newton 4 The dynamic theory of Laplace 5 Laplace 's tidal equations 6 Tidal analysis and prediction 6.1 Harmonic analysis 6.2 Tidal constituents 6.2. 1 Higher harmonics 6.2. 2 Semi-diurnal 6.2. 3 Diurnal 6.2. 4 Long period 7 See also 8 References and notes 9 External links Kepler In 1609 Johannes Kepler correctly suggested that the gravitation of the Moon causes the tides, basing his argument upon ancient observations and correlations. The influence of the Moon on tides was mentioned in Ptolemy 's Tetrabiblos as having derived from ancient observation. Galileo 's attempt to explain the tides Justus Sustermans -- Portrait of Galileo Galilei, 1636 In 1616, Galileo Galilei wrote Discourse on the Tides ( Discorso sul flusso e il reflusso del mare ), in a letter to Cardinal Orsini. In this discourse, he tried to explain the occurrence of the tides as the result of the Earth 's rotation and revolution around the Sun. Galileo believed that the oceans moved like water in a large basin : as the basin moves, so does the water. Therefore, as the Earth revolves, the force of the Earth 's rotation causes the oceans to `` alternately accelerate and retardate ''. His view on the oscillation and `` alternately accelerated and retardated '' motion of the Earth 's rotation is a `` dynamic process '' that deviated from the previous dogma, which proposed `` a process of expansion and contraction of seawater. '' However, Galileo 's theory was erroneous. In subsequent centuries, further analysis led to the current tidal physics. Galileo rejected Kepler 's explanation of the tides. Newton Newton, in the Principia, provided a correct explanation for the tidal force, which can be used to explain tides on a planet covered by a uniform ocean, but which takes no account of the distribution of the continents or ocean bathymetry. The dynamic theory of Laplace The dynamic theory of tides describes and predicts the actual real behavior of ocean tides. While Newton explained the tides by describing the tide - generating forces and Bernoulli gave a description of the static reaction of the waters on Earth to the tidal potential, the dynamic theory of tides, developed by Pierre - Simon Laplace in 1775, describes the ocean 's real reaction to tidal forces. Laplace 's theory of ocean tides took into account friction, resonance and natural periods of ocean basins. It predicted the large amphidromic systems in the world 's ocean basins and explains the oceanic tides that are actually observed. The equilibrium theory, based on the gravitational gradient from the Sun and Moon but ignoring the Earth 's rotation, the effects of continents, and other important effects, could not explain the real ocean tides. Since measurements have confirmed the theory, many things have possible explanations now, like how the tides interact with deep sea ridges and chains of seamounts give rise to deep eddies that transport nutrients from the deep to the surface. The equilibrium tide theory calculates the height of the tide wave of less than half a meter, while the dynamic theory explains why tides are up to 15 meters. Satellite observations confirm the accuracy of the dynamic theory, and the tides worldwide are now measured to within a few centimeters. Measurements from the CHAMP satellite closely match the models based on the TOPEX data. Accurate models of tides worldwide are essential for research since the variations due to tides must be removed from measurements when calculating gravity and changes in sea levels. Laplace 's tidal equations A. Lunar gravitational potential : this depicts the Moon directly over 30 ° N ( or 30 ° S ) viewed from above the Northern Hemisphere. B. This view shows same potential from 180 ° from view A. Viewed from above the Northern Hemisphere. Red up, blue down. In 1776, Pierre - Simon Laplace formulated a single set of linear partial differential equations, for tidal flow described as a barotropic two - dimensional sheet flow. Coriolis effects are introduced as well as lateral forcing by gravity. Laplace obtained these equations by simplifying the fluid dynamic equations. But they can also be derived from energy integrals via Lagrange 's equation. For a fluid sheet of average thickness D, the vertical tidal elevation ζ, as well as the horizontal velocity components u and v ( in the latitude φ and longitude λ directions, respectively ) satisfy Laplace 's tidal equations : ∂ ζ ∂ t + 1 a cos ⁡ ( φ ) ( ∂ ∂ λ ( u D ) + ∂ ∂ φ ( v D cos ⁡ ( φ ) ) ) = 0, ∂ u ∂ t − v ( 2 Ω sin ⁡ ( φ ) ) + 1 a cos ⁡ ( φ ) ∂ ∂ λ ( g ζ + U ) = 0 and ∂ v ∂ t + u ( 2 Ω sin ⁡ ( φ ) ) + 1 a ∂ ∂ φ ( g ζ + U ) = 0, ( displaystyle ( \begin ( aligned ) ( \frac ( partial zeta ) ( partial t ) ) & + ( \frac ( 1 ) ( a cos ( \varphi ) ) ) left ( ( \frac ( partial ) ( partial lambda ) ) ( uD ) + ( \frac ( partial ) ( partial \varphi ) ) left ( vD cos ( \varphi ) \right ) \right ) = 0, ( 2ex ) ( \frac ( partial u ) ( partial t ) ) & - v left ( 2 Omega sin ( \varphi ) \right ) + ( \frac ( 1 ) ( a cos ( \varphi ) ) ) ( \frac ( partial ) ( partial lambda ) ) left ( g zeta + U \right ) = 0 qquad ( \text ( and ) ) ( 2ex ) ( \frac ( partial v ) ( partial t ) ) & + u left ( 2 Omega sin ( \varphi ) \right ) + ( \frac ( 1 ) ( a ) ) ( \frac ( partial ) ( partial \varphi ) ) left ( g zeta + U \right ) = 0, end ( aligned ) ) ) where Ω is the angular frequency of the planet 's rotation, g is the planet 's gravitational acceleration at the mean ocean surface, a is the planetary radius, and U is the external gravitational tidal - forcing potential. William Thomson ( Lord Kelvin ) rewrote Laplace 's momentum terms using the curl to find an equation for vorticity. Under certain conditions this can be further rewritten as a conservation of vorticity. Tidal analysis and prediction Harmonic analysis Laplace 's improvements in theory were substantial, but they still left prediction in an approximate state. This position changed in the 1860s when the local circumstances of tidal phenomena were more fully brought into account by William Thomson 's application of Fourier analysis to the tidal motions as harmonic analysis. Thomson 's work in this field was then further developed and extended by George Darwin, applying the lunar theory current in his time. Darwin 's symbols for the tidal harmonic constituents are still used. Darwin 's harmonic developments of the tide - generating forces were later improved when AT Doodson, applying the lunar theory of EW Brown, developed the tide - generating potential ( TGP ) in harmonic form, distinguishing 388 tidal frequencies. Doodson 's work was carried out and published in 1921. Doodson devised a practical system for specifying the different harmonic components of the tide - generating potential, the Doodson numbers, a system still in use. Since the mid-twentieth century further analysis has generated many more terms than Doodson 's 388. About 62 constituents are of sufficient size to be considered for possible use in marine tide prediction, but sometimes many fewer can predict tides to useful accuracy. The calculations of tide predictions using the harmonic constituents are laborious, and from the 1870s to about the 1960s they were carried out using a mechanical tide - predicting machine, a special - purpose form of analog computer now superseded in this work by digital electronic computers that can be programmed to carry out the same computations. Tidal constituents Tidal constituents combine to give an endlessly varying aggregate because of their different and incommensurable frequencies : the effect is visualized in an animation of the American Mathematical Society illustrating the way in which the components used to be mechanically combined in the tide - predicting machine. Amplitudes of tidal constituents are given below for six example locations : Eastport, Maine ( ME ), Biloxi, Mississippi ( MS ), San Juan, Puerto Rico ( PR ), Kodiak, Alaska ( AK ), San Francisco, California ( CA ), and Hilo, Hawaii ( HI ). Higher harmonics Darwin Period Speed Doodson coefficients Doodson Amplitude at example location ( cm ) NOAA Species Symbol ( hr ) rate ( ° / hr ) n ( L ) n ( m ) n ( y ) n ( mp ) number ME MS PR AK CA HI order Shallow water overtides of principal lunar 6.210300601 57.9682084 455.555 6.0 0.6 0.9 2.3 5 Shallow water overtides of principal lunar 4.140200401 86.9523127 6 655.555 5.1 0.1 1.0 7 Shallow water terdiurnal MK 8.177140247 44.0251729 365.555 0.5 1.9 8 Shallow water overtides of principal solar 6 60 - 4 491.555 0.1 9 Shallow water quarter diurnal MN 6.269173724 57.4238337 - 1 445.655 2.3 0.3 0.9 10 Shallow water overtides of principal solar 90 6 6 - 6 * 0.1 12 Lunar terdiurnal 8.280400802 43.4761563 355.555 0.5 32 Shallow water terdiurnal 2 `` MK 8.38630265 42.9271398 - 1 345.555 0.5 0.5 1.4 34 Shallow water eighth diurnal 3.105150301 115.9364166 8 855.555 0.5 0.1 36 Shallow water quarter diurnal MS 6.103339275 58.9841042 - 2 473.555 1.8 0.6 1.0 37 Semi-diurnal Darwin Period Speed Doodson coefficients Doodson Amplitude at example location ( cm ) NOAA Species Symbol ( hr ) ( ° / hr ) n ( L ) n ( m ) n ( y ) n ( mp ) number ME MS PR AK CA HI order Principal lunar semidiurnal 12.4206012 28.9841042 255.555 268.7 3.9 15.9 97.3 58.0 23.0 Principal solar semidiurnal 12 30 - 2 273.555 42.0 3.3 2.1 32.5 13.7 9.2 Larger lunar elliptic semidiurnal 12.65834751 28.4397295 - 1 245.655 54.3 1.1 3.7 20.1 12.3 4.4 Larger lunar evectional ν 12.62600509 28.5125831 - 1 - 1 247.455 12.6 0.2 0.8 3.9 2.6 0.9 11 Variational MU 12.8717576 27.9682084 - 2 237.555 2.0 0.1 0.5 0.7 0.8 13 Lunar elliptical semidiurnal second - order 2 `` N 12.90537297 27.8953548 - 2 235.755 6.5 0.1 0.5 2.4 1.4 0.6 14 Smaller lunar evectional λ 12.22177348 29.4556253 - 2 263.655 5.3 0.1 0.7 0.6 0.2 16 Larger solar elliptic 12.01644934 29.9589333 - 3 272.555 3.7 0.2 0.1 1.9 0.9 0.6 27 Smaller solar elliptic 11.98359564 30.0410667 - 1 274.555 0.9 0.2 0.1 0.1 28 Shallow water semidiurnal 2SM 11.60695157 31.0158958 - 4 291.555 0.5 31 Smaller lunar elliptic semidiurnal 12.19162085 29.5284789 - 1 265.455 13.5 0.1 0.5 2.4 1.6 0.5 33 Lunisolar semidiurnal 11.96723606 30.0821373 275.555 11.6 0.9 0.6 9.0 4.0 2.8 35 Diurnal Darwin Period Speed Doodson coefficients Doodson Amplitude at example location ( cm ) NOAA Species Symbol ( hr ) ( ° / hr ) n ( L ) n ( m ) n ( y ) n ( mp ) number ME MS PR AK CA HI order Lunar diurnal 23.93447213 15.0410686 165.555 15.6 16.2 9.0 39.8 36.8 16.7 Lunar diurnal 25.81933871 13.9430356 - 1 145.555 11.9 16.9 7.7 25.9 23.0 9.2 6 Lunar diurnal OO 22.30608083 16.1391017 185.555 0.5 0.7 0.4 1.2 1.1 0.7 15 Solar diurnal 24 15 - 1 164.555 1.0 0.5 1.2 0.7 0.3 17 Smaller lunar elliptic diurnal 24.84120241 14.4920521 155.555 0.6 1.2 0.5 1.4 1.1 0.5 18 Smaller lunar elliptic diurnal 23.09848146 15.5854433 - 1 175.455 0.9 1.3 0.6 2.3 1.9 1.1 19 Larger lunar evectional diurnal ρ 26.72305326 13.4715145 - 2 - 1 137.455 0.3 0.6 0.3 0.9 0.9 0.3 25 Larger lunar elliptic diurnal Q 26.868350 13.3986609 - 2 135.655 2.0 3.3 1.4 4.7 4.0 1.6 26 Larger elliptic diurnal 2Q 28.00621204 12.8542862 - 3 125.755 0.3 0.4 0.2 0.7 0.4 0.2 29 Solar diurnal 24.06588766 14.9589314 - 2 163.555 5.2 5.4 2.9 12.6 11.6 5.1 30 Long period Darwin Period Speed Doodson coefficients Doodson Amplitude at example location ( cm ) NOAA Species Symbol ( hr ) ( ° / hr ) n ( L ) n ( m ) n ( y ) n ( mp ) number ME MS PR AK CA HI order Lunar monthly 661.3111655 0.5443747 0 - 1 65.455 0.7 1.9 20 Solar semiannual 4383.076325 0.0821373 0 57.555 1.6 2.1 1.5 3.9 21 Solar annual 8766.15265 0.0410686 0 56.555 5.5 7.8 3.8 4.3 22 Lunisolar synodic fortnightly 354.3670666 1.0158958 0 - 2 73.555 1.5 23 Lunisolar fortnightly 327.8599387 1.0980331 0 75.555 1.4 2.0 0.7 24 See also Kelvin wave References and notes Jump up ^ Johannes Kepler, Astronomia nova... ( 1609 ), p. 5 of the Introductio in hoc opus ^ Jump up to : Rice University : Galileo 's Theory of the Tides, by Rossella Gigli, retrieved 10 March 2010 Jump up ^ Tyson, Peter. `` Galileo 's Big Mistake ''. NOVA. PBS. Retrieved 2014 - 02 - 19. Jump up ^ Palmieri, Paolo ( 1998 ). Re-examining Galileo 's Theory of Tides. Springer - Verlag. p. 229. Jump up ^ Palmeri, Paolo ( 1998 ). Re-examining Galileo 's Theory of Tides. Springer - Verlag. p. 227. Jump up ^ http://web.vims.edu/physical/research/TCTutorial/static.htm Jump up ^ http://www.pearsonhighered.com/samplechapter/0132401223.pdf Jump up ^ http://www.preservearticles.com/2011112017524/short-notes-on-the-dynamical-theory-of-laplace.html Jump up ^ `` Shelf and Coastal Oceanography ''. Es.flinders.edu.au. Retrieved 2012 - 06 - 02. Jump up ^ http://faculty.washington.edu/luanne/pages/ocean420/notes/tidedynamics.pdf Jump up ^ http://ocean.kisti.re.kr/downfile/volume/kess/JGGHBA/2009/v30n5/JGGHBA_2009_v30n5_671.pdf Jump up ^ Tidal theory website South African Navy Hydrographic Office Jump up ^ `` Dynamic theory for tides ''. Oberlin.edu. Retrieved 2012 - 06 - 02. Jump up ^ `` Dynamic Theory of Tides ''. Jump up ^ `` Dynamic Tides -- In contrast to `` static '' theory, the dynamic theory of tides recognizes that water covers only three - quarters o ``. Web.vims.edu. Retrieved 2012 - 06 - 02. Jump up ^ `` The Dynamic Theory of Tides ''. Coa.edu. Retrieved 2012 - 06 - 02. Jump up ^ https://beacon.salemstate.edu/~lhanson/gls214/gls214_tides Jump up ^ `` Tides -- building, river, sea, depth, oceans, effects, important, largest, system, wave, effect, marine, Pacific ''. Waterencyclopedia.com. 2010 - 06 - 27. Retrieved 2012 - 06 - 02. Jump up ^ `` TIDES ''. Ocean.tamu.edu. Retrieved 2012 - 06 - 02. Jump up ^ Floor Anthoni. `` Tides ''. Seafriends.org.nz. Retrieved 2012 - 06 - 02. Jump up ^ `` The Cause & Nature of Tides ''. Jump up ^ `` Scientific Visualization Studio TOPEX / Poseidon images ''. Svs.gsfc.nasa.gov. Retrieved 2012 - 06 - 02. Jump up ^ `` TOPEX / Poseidon Western Hemisphere : Tide Height Model : NASA / Goddard Space Flight Center Scientific Visualization Studio : Free Download & Streaming : Internet Archive ''. Archive.org. Retrieved 2012 - 06 - 02. Jump up ^ TOPEX data used to model actual tides for 15 days from the year 2000 url = http://svs.gsfc.nasa.gov/vis/a000000/a001300/a001332/ Jump up ^ http://www.geomag.us/info/Ocean/m2_CHAMP+longwave_SSH.swf Jump up ^ `` OSU Tidal Data Inversion ''. Volkov.oce.orst.edu. Retrieved 2012 - 06 - 02. Jump up ^ `` Dynamic and residual ocean tide analysis for improved GRACE de-aliasing ( DAROTA ) ''. Jump up ^ `` The Laplace Tidal Equations and Atmospheric Tides '' ( PDF ). Jump up ^ DE Cartwright, `` Tides : a scientific history '', Cambridge University Press 2001, at pages 163 - 4. Jump up ^ S Casotto, F Biscani, `` A fully analytical approach to the harmonic development of the tide - generating potential accounting for precession, nutation, and perturbations due to figure and planetary terms '', AAS Division on Dynamical Astronomy, April 2004, vol. 36 ( 2 ), 67. Jump up ^ AT Doodson ( 1921 ), `` The Harmonic Development of the Tide - Generating Potential '', Proceedings of the Royal Society of London. Series A, Vol. 100, No. 704 ( Dec. 1, 1921 ), pp. 305 - 329. Jump up ^ See e.g. TD Moyer ( 2003 ), `` Formulation for observed and computed values of Deep Space Network data types for navigation '', vol. 3 in Deep - space communications and navigation series, Wiley ( 2003 ), e.g. at pp. 126 - 8. Jump up ^ NOAA. `` Eastport, ME Tidal Constituents ''. NOAA. Retrieved 2012 - 05 - 22. External links Wikiquote has quotations related to : Theory of tides Arctic and Antarctic Barotropic Tide Models Amphidrome Equilibrium Theory of Tides Dynamic Tides Annual amphidromes : a common feature in the ocean ? http://www.aviso.oceanobs.com/en/news/idm/2000/oct-2000-sun-and-moon-shape-tides-on-earth/ Tides Contributions of satellite laser ranging to the studies of earth tides Sun and Moon shape tides on Earth Study of harmonic site position variations determined by very long baseline interferometry http://www.coa.edu/stodd/oceanweb/oceanography/Oceanlectures02/Lecture8/sld014.htm Dynamic Theory of Tides Tidal Observations Myths about Gravity and Tides https://books.google.com/books?id=3mGZUHDuEdwC&lpg=PA150&ots=soMAFKsRkc&dq=number%20of%20amphidromes&pg=PA150#v=onepage&q=amphidrome&f=false Publications from NOAA 's Center for Operational Oceanographic Products and Services Understanding Tides 150 Years of Tides on the Western Coast Our Relentless Tides U. Manna, J.L. Menaldi and S.S. Sritharan : Stochastic Analysis of Tidal Dynamics Equation in Infinite Dimensional Stochastic Analysis, edited by A.N. Sengupta and P. Sundar, World Scientific Publishers, 2008. M. Suvinthra, S.S. Sritharan and K. Balachandran : ( 1 ) Large Deviations of Stochastic Tidal Dynamics Equation, in Communications on Stochastic Analysis, Vol. 9, No. 4 ( 2015 ) 477 - 502. Retrieved from `` https://en.wikipedia.org/w/index.php?title=Theory_of_tides&oldid=807319159 '' Categories : Tides Geophysics Oceanography Continuum mechanics Fluid dynamics Fluid mechanics Planetary science Hidden categories : Use dmy dates from September 2010 Talk Contents About Wikipedia Wikiquote Català Deutsch Español हिन्दी Italiano Nederlands Edit links This page was last edited on 27 October 2017, at 06 : 37. Text is available under the Creative Commons Attribution - ShareAlike License ; additional terms may apply. By using this site, you agree to the Terms of Use and Privacy Policy. 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Question: who had propounded the dynamic theory of origin of ocean tides
Answer: Pierre-Simon Laplace