Notes to GEOF346 Tidal Dynamics and Sea Level Variations

Total Page:16

File Type:pdf, Size:1020Kb

Notes to GEOF346 Tidal Dynamics and Sea Level Variations Notes to GEOF346 Tidal Dynamics and Sea Level Variations Fall 2021 Helge Drange Geophysical Institute, University of Bergen helge.drange@gfi.uib.no Mainly off-hour typing { so give a word regarding errors, inconsistencies, etc... Also give a word in case of specific requests (derivations, unclear issues), and I will try to update the notes accordingly. The note will be regularly updated { so keep printing at a minimum... The notation (closely) follows that used in the text book: Sea-Level Science by D. Pugh and P. Woodworth, Cambridge, 2014 (https://doi.org/10.1017/CBO9781139235778) Parts of the derivations follow Forelesninger over tidevann og tidevannsstrømmer. Teori, opptreden, analyse og prediksjon, by Herman G. Gade, Geofysisk institutt, Universitetet i Bergen Note: • Symbols/expressions in red are, to the best of the author's knowledge, cor- rections to typos in the text book. • For simplicity, the notation (614) sin 2 a = 2 sin a cos a implies that, in this case, equation (614) has been adopted in the displayed expression. • Norwegian word/phrases are given in quotation marks in footnotes. • A (far from) complete Norwegian dictionary is provided in appendix I. • ...and the index section is only slowly being updated. • Last, but not least: Comments to the compendium are always appreciated! 1 October 4, 2021 2 Contents I Tides, basic astronomical periods and frequencies 8 1 Supporting literature 8 1.1 General text . .8 1.2 Tidal energy . .8 2 Definition of the tides 8 3 Solar periods and frequencies 9 4 Lunar periods and frequencies 10 II Equilibrium theory and derivations thereof 12 5 Equilibrium theory, direct method 12 5.1 Geometry of the Earth-Moon system . 12 5.2 Centre of mass of the Earth-Moon system . 12 5.3 Newton's law of universal gravitation . 14 5.4 Gravitational forces and accelerations in the Earth-Moon system . 14 5.5 Earth's movement around the Earth-Moon centre of mass . 15 5.6 A (somewhat complicating) side note . 15 5.7 Net gravity on the Earth caused by the Moon . 17 5.8 Introducing the zenith angle and simplifying . 17 5.9 Radial and tangential components of the tidal acceleration . 18 5.9.1 Geometric approach . 18 5.9.2 Using the definition of the dot and cross products . 19 5.9.3 The radial component can be ignored; the tangential component is important 20 5.10 Surface elevation caused by the Moon . 20 5.10.1 Determining the integration constant for the Equilibrium Tide surface el- evation . 21 6 The combined surface elevation caused by the Moon and the Sun 23 6.1 Amplitudes . 23 6.2 Relative contribution from the Sun and the Solar planets . 23 6.3 Tidal potential . 24 6.4 Gravitational potential . 25 7 Introducing latitude, hour and declination angles 26 7.1 The three leading lunar tidal components . 26 7.2 The Equilibrium Tide caused by the Moon . 28 7.3 Properties of the three leading lunar components . 28 7.3.1 Declination or nodal component, ζ0 ..................... 29 7.3.2 Diurnal component, ζ1 ............................. 29 7.3.3 Semi-diurnal component, ζ2 .......................... 29 8 Sidereal and synodic periods 30 8.1 The Moon's sidereal and synodic monthly periods . 30 3 8.2 The synodic lunar day . 32 8.3 The Earth's daily sidereal period . 33 8.4 The synodic lunar day as seen from a fixed star . 34 8.5 Key periods and frequencies for the Moon-Earth-Sun system . 35 8.6 The lunar and solar hour angles expressed by the sidereal time . 36 9 Decomposing the solar and lunar tides into a series of simple harmonic con- stituents 38 9.1 Geometry of the Earth-Sun system . 38 9.1.1 Angular speed of the Earth and the Sun . 38 9.1.2 Expressing sin 2ds as sin ds ......................... 40 9.1.3 Expressing ζ1 in terms of simple harmonics . 41 9.1.4 Expressing ζ2 in terms of simple harmonics . 42 9.2 Sun's leading tidal constituents . 43 9.3 Moon's leading tidal constituents . 43 9.4 Doodson's system for labelling tidal constituents . 44 10 The spring/neap tide 46 10.1 Derivation . 47 10.1.1 Amplitude and range . 48 10.1.2 Timing of maximum amplitude . 48 10.1.3 Age of the tide . 48 10.1.4 A note . 50 11 Tidal forcing in the momentum equation 51 12 Laplace's Tidal Equations 52 13 The tidal force expressed in terms of the tidal potential 53 13.1 The potential of a conservative force . 53 13.2 Defining the tidal potential . 53 13.2.1 Gradient of the factor q=q3 .......................... 53 13.2.2 Gradient of the factor R=R3 ......................... 54 13.2.3 Resulting tidal potential . 55 13.3 Tidal potential expressed in terms of the zenith angle . 55 13.3.1 Radial and tangential tidal forces per unit mass . 56 14 Introducing the tidal potential in the primitive momentum equations 57 15 Including the effect of elliptic orbits 58 15.1 The Sun-Earth system1 ................................ 58 15.2 Kepler's second law . 60 15.3 Kepler's first law . 61 15.4 Kepler's third law . 62 15.5 Mean anomaly E0 ................................... 63 15.6 Real vs mean length of the radius vector, and Kepler's equation . 63 15.6.1 Rs vs Rs .................................... 63 15.6.2 Kepler's equation . 64 1Mainly based on R. Fitzpatrick (): An Introduction to Celestial Mechanics, M. Hendershott (): Lecture 1: Introduction to ocean tides, and Murray & Dermott (1999), Solar Syatem Dynamics, Chap. 2. 4 15.6.3 Solving Kepler's equation . 66 15.6.4 Rs=Rs expressed by means of E0 ...................... 66 15.6.5 Introducing the ecliptic longitude and the longitude of perihelion . 67 15.7 Right Ascension . 68 15.8 Equation of time . 70 15.8.1 Equation of center . 70 15.8.2 Longitudinal differences . 71 15.8.3 Equation of time, final expression . 71 15.8.4 Equation of time, graphical representation . 71 III Tidal harmonic analysis 74 16 Background 74 17 Implementation, sea surface height variations 77 17.1 Extraction of the M2 tide . 78 17.2 Note 1 . 78 17.3 Note 2 . 78 17.4 Extraction of the S2 tide . 79 17.5 Extraction of the N2 tide . 79 17.6 Extraction of the K2 tide . 79 17.7 Extraction of the O1 tide . 79 17.8 Extraction of the K1 tide . 79 17.9 Note 3 . 80 17.10Note 4 . 81 18 Tidal current analysis 81 18.1 Direction of flow θ and current speed q ....................... 81 18.2 Semi-major and semi-minor axes . 84 18.3 Time of maximum current speed . 85 18.4 Direction of maximum current speed . 85 18.5 Direction of rotation . 85 IV Tidal related wave dynamics 87 19 The shallow water equations 87 19.1 Starting point and configuration . 87 19.2 The continuity equation . 87 19.3 The momentum equations . 89 19.4 The final set of equations . 89 20 Gravity waves 91 20.1 One-dimensional gravity waves . 91 20.1.1 Typical wavelengths for tidal waves . 91 20.2 One-dimensional gravity waves in a closed channel . 92 20.3 One-dimensional gravity waves in a semi-closed channel . 93 20.3.1 Resonance . 94 5 21 Sverdrup waves and other related waves 95 21.1 Derivation . 95 21.2 Case ! =0 ....................................... 96 2 2 2 2 21.3 Case ! = f + c0 kh ................................. 96 21.3.1 The resulting wave motion . 97 21.3.2 Approximate length of the tidal axes . 100 21.4 Case f =0 ....................................... 101 21.5 Case k2 f 2=(gD) (short waves) . 101 21.6 Case k2 f 2=(gD) (long waves) . 102 21.7 Interaction between tidal ellipses and internal oscillations . 102 V Appendix 104 A Some key parameters of the Earth, Moon, Sun system 104 A.1 Mass . 104 A.2 Length and distance . 104 B Spherical coordinates 105 B.1 Two commonly used spherical coordinate systems . 105 B.2 Volume and surface elements in spherical coordinates . ..
Recommended publications
  • Arxiv:1303.4129V2 [Gr-Qc] 8 May 2013 Counters with Supermassive Black Holes (SMBH) of Mass in Some Preceding Tidal Event
    Relativistic effects in the tidal interaction between a white dwarf and a massive black hole in Fermi normal coordinates Roseanne M. Cheng∗ Center for Relativistic Astrophysics, School of Physics, Georgia Institute of Technology, Atlanta, Georgia 30332, USA and Department of Physics and Astronomy, University of North Carolina, Chapel Hill, North Carolina 27599, USA Charles R. Evansy Department of Physics and Astronomy, University of North Carolina, Chapel Hill, North Carolina 27599 (Received 17 March 2013; published 6 May 2013) We consider tidal encounters between a white dwarf and an intermediate mass black hole. Both weak encounters and those at the threshold of disruption are modeled. The numerical code combines mesh-based hydrodynamics, a spectral method solution of the self-gravity, and a general relativistic Fermi normal coordinate system that follows the star and debris. Fermi normal coordinates provide an expansion of the black hole tidal field that includes quadrupole and higher multipole moments and relativistic corrections. We compute the mass loss from the white dwarf that occurs in weak tidal encounters. Secondly, we compute carefully the energy deposition onto the star, examining the effects of nonradial and radial mode excitation, surface layer heating, mass loss, and relativistic orbital motion. We find evidence of a slight relativistic suppression in tidal energy transfer. Tidal energy deposition is compared to orbital energy loss due to gravitational bremsstrahlung and the combined losses are used to estimate tidal capture orbits. Heating and partial mass stripping will lead to an expansion of the white dwarf, making it easier for the star to be tidally disrupted on the next passage.
    [Show full text]
  • Astrometry and Tidal Migration V
    Astrometry and tidal migration V. Lainey (JPL/IMCCE), J.Fuller (Caltech) [email protected] -KISS workshop- October 16th 2018 Astrometric measurements Example 1: classical astrometric observations (the most direct measurement) Images suitable for astrometric reduction from ground or space Tajeddine et al. 2013 Mallama et al. 2004 CCD obs from ground Cassini ISS image HST image Photographic plates (not used anymore BUT re-reduction now benefits from modern scanning machine) Astrometric measurements Example 2: photometric measurements (undirect astrometric measurement) Eclipses by the planet Mutual phenomenae (barely used those days…) (arising every six years) By modeling the event, one can solve for mid-time event and minimum distance between the center of flux figure of the objects à astrometric measure Time (hours) Astrometric measurements Example 3: other measurements (non exhaustive list) During flybys of moons, one can (sometimes!) solved for a correction on the moon ephemeris Radio science measurement (orbital tracking) Radar measurement (distance measurement between back and forth radio wave travel) Morgado et al. 2016 Mutual approximation (measure of moons’ distance rate) Astrometric accuracy Remark: 1- Accuracy of specific techniques STRONGLY depends on the epoch 2- Total numBer of oBservations per oBservation opportunity can Be VERY different For the Galilean system: (numbers are purely indicative) From ground Direct imaging: 100 mas (300 km) to 20 mas (60 km) –stacking techniques- Mutual events: typically 20-80 mas
    [Show full text]
  • Effect of Mantle and Ocean Tides on the Earth’S Rotation Rate
    A&A 493, 325–330 (2009) Astronomy DOI: 10.1051/0004-6361:200810343 & c ESO 2008 Astrophysics Effect of mantle and ocean tides on the Earth’s rotation rate P. M. Mathews1 andS.B.Lambert2 1 Department of Theoretical Physics, University of Madras, Chennai 600025, India 2 Observatoire de Paris, Département Systèmes de Référence Temps Espace (SYRTE), CNRS/UMR8630, 75014 Paris, France e-mail: [email protected] Received 7 June 2008 / Accepted 17 October 2008 ABSTRACT Aims. We aim to compute the rate of increase of the length of day (LOD) due to the axial component of the torque produced by the tide generating potential acting on the tidal redistribution of matter in the oceans and the solid Earth. Methods. We use an extension of the formalism applied to precession-nutation in a previous work to the problem of length of day variations of an inelastic Earth with a fluid core and oceans. Expressions for the second order axial torque produced by the tesseral and sectorial tide-generating potentials on the tidal increments to the Earth’s inertia tensor are derived and used in the axial component of the Euler-Liouville equations to arrive at the rate of increase of the LOD. Results. The increase in the LOD, produced by the same dissipative mechanisms as in the theoretical work on which the IAU 2000 nutation model is based and in our recent computation of second order effects, is found to be at a rate of 2.35 ms/cy due to the ocean tides, and 0.15 ms/cy due to solid Earth tides, in reasonable agreement with estimates made by other methods.
    [Show full text]
  • A Possible Explanation of the Secular Increase of the Astronomical Unit 1
    T. Miura 1 A possible explanation of the secular increase of the astronomical unit Takaho Miura(a), Hideki Arakida, (b) Masumi Kasai(a) and Syuichi Kuramata(a) (a)Faculty of Science and Technology,Hirosaki University, 3 bunkyo-cyo Hirosaki, Aomori, 036-8561, Japan (b)Education and integrate science academy, Waseda University,1 waseda sinjuku Tokyo, Japan Abstract We give an idea and the order-of-magnitude estimations to explain the recently re- ported secular increase of the Astronomical Unit (AU) by Krasinsky and Brumberg (2004). The idea proposed is analogous to the tidal acceleration in the Earth-Moon system, which is based on the conservation of the total angular momentum and we apply this scenario to the Sun-planets system. Assuming the existence of some tidal interactions that transfer the rotational angular momentum of the Sun and using re- d ported value of the positive secular trend in the astronomical unit, dt 15 4(m/s),the suggested change in the period of rotation of the Sun is about 21(ms/cy) in the case that the orbits of the eight planets have the same "expansionrate."This value is suf- ficiently small, and at present it seems there are no observational data which exclude this possibility. Effects of the change in the Sun's moment of inertia is also investi- gated. It is pointed out that the change in the moment of inertia due to the radiative mass loss by the Sun may be responsible for the secular increase of AU, if the orbital "expansion"is happening only in the inner planets system.
    [Show full text]
  • Tidal Locking and the Gravitational Fold Catastrophe
    City University of New York (CUNY) CUNY Academic Works Publications and Research New York City College of Technology 2020 Tidal locking and the gravitational fold catastrophe Andrea Ferroglia CUNY New York City College of Technology Miguel C. N. Fiolhais CUNY Borough of Manhattan Community College How does access to this work benefit ou?y Let us know! More information about this work at: https://academicworks.cuny.edu/ny_pubs/679 Discover additional works at: https://academicworks.cuny.edu This work is made publicly available by the City University of New York (CUNY). Contact: [email protected] Tidal locking and the gravitational fold catastrophe Andrea Ferroglia1;2 and Miguel C. N. Fiolhais3;4 1The Graduate School and University Center, The City University of New York, 365 Fifth Avenue, New York, NY 10016, USA 2 Physics Department, New York City College of Technology, The City University of New York, 300 Jay Street, Brooklyn, NY 11201, USA 3 Science Department, Borough of Manhattan Community College, The City University of New York, 199 Chambers St, New York, NY 10007, USA 4 LIP, Departamento de F´ısica, Universidade de Coimbra, 3004-516 Coimbra, Portugal The purpose of this work is to study the phenomenon of tidal locking in a pedagogical framework by analyzing the effective gravitational potential of a two-body system with two spinning objects. It is shown that the effective potential of such a system is an example of a fold catastrophe. In fact, the existence of a local minimum and saddle point, corresponding to tidally-locked circular orbits, is regulated by a single dimensionless control parameter which depends on the properties of the two bodies and on the total angular momentum of the system.
    [Show full text]
  • Tidal Tomography to Probe the Moon's Mantle Structure Using
    Tidal Tomography to Probe the Moon’s Mantle Structure Using Lunar Surface Gravimetry Kieran A. Carroll1, Harriet Lau2, 1: Gedex Systems Inc., [email protected] 2: Department of Earth and Planetary Sciences, Harvard University, [email protected] Lunar Tides Gravimetry of the Lunar Interior VEGA Instrument through the Moon's PulSE • Gedex has developed a low cost compact space gravimeter instrument , VEGA (Vector (GLIMPSE) Investigation Gravimeter/Accelerometer) Moon • Currently this is the only available gravimeter that is suitable for use in space Earth GLIMPSE Investigation: • Proposed under NASA’s Lunar Surface Instrument and Technology Payloads • ca. 1972 MIT developed a space gravimeter (LSITP) program. instrument for use on the Moon, for Apollo 17. That instrument is long-ago out of • To fly a VEGA instrument to the Moon on a commercial lunar lander, via NASA’s production and obsolete. Commercial Lunar Payload Services (CLPS) program. VEGA under test in thermal- GLIMPSE Objectives: VEGA Space Gravimeter Information vacuum chamber at Gedex • Prove the principle of measuring time-varying lunar surface gravity to probe the lunar • Measures absolute gravity vector, with no • Just as the Moon and the Sun exert tidal forces on the Earth, the Earth exerts tidal deep interior using the Tidal Tomography technique. bias forces on the Moon. • Determine constraints on parameters defining the Lunar mantle structure using time- • Accuracy on the Moon: • Tidal stresses in the Moon are proportional to the gravity gradient tensor field at the varying gravity measurements at a location on the surface of the Moon, over the • Magnitude: Effective noise of 8 micro- Moon’s centre, multiplies by the distance from the Moon’s centre.
    [Show full text]
  • Black Hole Math Is Designed to Be Used As a Supplement for Teaching Mathematical Topics
    National Aeronautics and Space Administration andSpace Aeronautics National ole M a th B lack H i This collection of activities, updated in February, 2019, is based on a weekly series of space science problems distributed to thousands of teachers during the 2004-2013 school years. They were intended as supplementary problems for students looking for additional challenges in the math and physical science curriculum in grades 10 through 12. The problems are designed to be ‘one-pagers’ consisting of a Student Page, and Teacher’s Answer Key. This compact form was deemed very popular by participating teachers. The topic for this collection is Black Holes, which is a very popular, and mysterious subject among students hearing about astronomy. Students have endless questions about these exciting and exotic objects as many of you may realize! Amazingly enough, many aspects of black holes can be understood by using simple algebra and pre-algebra mathematical skills. This booklet fills the gap by presenting black hole concepts in their simplest mathematical form. General Approach: The activities are organized according to progressive difficulty in mathematics. Students need to be familiar with scientific notation, and it is assumed that they can perform simple algebraic computations involving exponentiation, square-roots, and have some facility with calculators. The assumed level is that of Grade 10-12 Algebra II, although some problems can be worked by Algebra I students. Some of the issues of energy, force, space and time may be appropriate for students taking high school Physics. For more weekly classroom activities about astronomy and space visit the NASA website, http://spacemath.gsfc.nasa.gov Add your email address to our mailing list by contacting Dr.
    [Show full text]
  • Editorial Manager(Tm) for Earth, Moon, and Planets Manuscript Draft
    Editorial Manager(tm) for Earth, Moon, and Planets Manuscript Draft Manuscript Number: MOON491 Title: Irregularly Shaped Satellites-Phobos & Deimos- moons of Mars, and their evolutionary history. Article Type: Manuscript Keywords: gravitational sling shot effect; Clarke's Orbits; Roche's Limit; velocity of recession/approach; sub-synchronous orbit; extra-synchronous orbit. Corresponding Author: DOCTOR BIJAY KUMAR SHARMA, Ph.D Corresponding Author's Institution: NATIONAL INSTITUTE OF TECHNOLOGY First Author: Bijay K Sharma, B.Tech,MS & Ph.D. Order of Authors: Bijay K Sharma, B.Tech,MS & Ph.D.; BIJAY KUMAR SHARMA, Ph.D Abstract: Phobos, a moon of Mars, is below the Clarke's synchronous orbit and due to tidal interaction is losing altitude. With this altitude loss it is doomed to the fate of total destruction by direct collision with Mars. On the other hand Deimos, the second moon of Mars is in extra-synchronous orbit and almost stay put in the present orbit. The reported altitude loss of Phobos is 1.8 m per century by wikipedia and 60ft per century according to ozgate url . The reported time in which the destruction will take place is 50My and 40My respectively. The authors had proposed a planetary-satellite dynamics based on detailed study of Earth-Moon[personal communication: http://arXiv.org/abs/0805.0100 ]. Based on this planetary satellite dynamics, 2 m/century approach velocity leads to the age of Phobos to be 23 Gyrs which is physically untenable since our Solar System's age is 4.567Gyrs. Hence the present altitude loss is assumed to be 20 m per century.
    [Show full text]
  • Confusion Around the Tidal Force and the Centrifugal Force
    Jein Institute for Fundamental Science・Research Note, 2015 Confusion around the tidal force and the centrifugal force Confusion around the tidal force and the centrifugal force Takuya Matsuda, NPO Einstein, 5-14, Yoshida-Honmachiu, Sakyo-ku, Kyoto, 606-8317 Hiromu Isaka, Shimadzu Corp., 1, Nishinokyo-Kuwabaracho, Nakagyoku, Kyoto, 604-8511 Henri M. J. Boffin, ESO, Alonso de Cordova 3107, Vitacur, Casilla 19001, Santiago de Cile, Chile We discuss the tidal force, whose notion is sometimes misunderstood in the public domain literature. We discuss the tidal force exerted by a secondary point mass on an extended primary body such as the Earth. The tidal force arises because the gravitational force exerted on the extended body by the secondary mass is not uniform across the primary. In the derivation of the tidal force, the non-uniformity of the gravity is essential, and inertial forces such as the centrifugal force are not needed. Nevertheless, it is often asserted that the tidal force can be explained by the centrifugal force. If we literally take into account the centrifugal force, it would mislead us. We therefore also discuss the proper treatment of the centrifugal force. 1.Introduction 2.Confusion around the centrifugal force In the present paper, we discuss the tidal force. We distinguish the tidal As was described earlier, the Earth and the Moon revolve about the force and the tidal phenomenon for the sake of exactness. The tide is a common center of gravity in the inertial frame. Fig. 1 shows a wrong geophysical phenomenon produced by the tidal force. The surface of the picture of the sea surface affected by the tidal force due to the Moon.
    [Show full text]
  • Natural Moons Dynamics and Astrometry
    OBSERVATOIRE DE PARIS MEMOIRE D’HABILITATION A DIRIGER DES RECHERCES Présenté par Valéry LAINEY Natural moons dynamics and astrometry Soutenue le 29 mai 2017 Jury: Anne LEMAITRE (Rapporteur) François MIGNARD (Rapporteur) William FOLKNER (Rapporteur) Doris BREUER (Examinatrice) Athéna COUSTENIS (Examinatrice) Carl MURRAY (Examinateur) Francis NIMMO (Examinateur) Bruno SICARDY (Président) 2 Index Curriculum Vitae 5 Dossier de synthèse 11 Note d’accompagnement 31 Coordination d’équipes et de réseaux internationaux 31 Encadrement de thèses 34 Tâches de service 36 Enseignement 38 Résumé 41 Annexe 43 Lainey et al. 2007 : First numerical ephemerides of the Martian moons Lainey et al. 2009 : Strong tidal dissipation in Io and Jupiter from astrometric observations Lainey et al. 2012 : Strong Tidal Dissipation in Saturn and Constraints on Enceladus' Thermal State from Astrometry Lainey et al. 2017 : New constraints on Saturn's interior from Cassini astrometric data Lainey 2008 : A new dynamical model for the Uranian satellites 3 4 Curriculum Vitae Name: Valéry Lainey Address: IMCCE/Observatoire de Paris, 77 Avenue Denfert-Rochereau, 75014 Paris, France Email: [email protected]; Tel.: (+33) (0)1 40 51 22 69 Birth: 19/08/1974 Qualifications: Ph.D. Observatoire de Paris, December 2002 Title of thesis: “Théorie dynamique des satellites galiléens" Master degree “Astronomie fondamentale, mécanique céleste et géodésie” Observatoire de Paris 1998. Academic Career: Sep. 2006 - Present Astronomer at the Paris Observatory Apr. 2004 - Aug. 2006 Post-doc position at the Royal Observatory of Belgium Jun. 2003 - Mar. 2004 Post-doc position at the Paris Observatory Mar. - May 2003 Invited fellow at the Indian Institute of Astrophysics Dec. 2002 - Feb.
    [Show full text]
  • Destroying the Earth by Using Tidal Energy
    Destroying the Earth by Using Tidal Energy Jerry Z. Liu Stanford University, California, USA (Submitted to arXiv.org, May 30th, 2019) Abstract Sciences and technologies have been advanced to a level that they can be used to destroy the Earth, if in a wrong hand. However, you might be surprised to hear that the Earth may also be destroyed by using tidal energy, even with a positive intention!? Consuming tidal energy is actually taking, therefore reducing, the rotational energy of the Earth, which decelerates the rotation speed. Based on current pace of world energy consumption, if we were taking the rotational energy just to supplement 1% of world energy requirements, the rotation of the Earth could be literally stopped in about 1000 ​ years. As a consequence, one side of the Earth would expose to the Sun for much ​ ​ longer time than it is today. The temperature would be extremely high on this side, and extremely low on the opposite side. The environment would be intolerable and life would be wiped out from the Earth. Introduction Global warming has brought awareness to many people as a consequence of consuming fossil fuels. As a clean, renewable alternative, tidal energy has attracted more and more attention. Technologies have been developed and made it possible to collect tidal energy and convert it to ​ electricity to supply the increasing energy requirements for the world’s growing economies. However, it might be a surprise to many people that tidal energy is actually not renewable ​ energy and using tidal energy will create more severe environmental problems than global warming.
    [Show full text]
  • Lecture 21: Tidal Forces
    Lecture 21: Tidal Forces • For most of the problems we’ll treat this semester, we’ll assume that the Earth is an inertial frame of reference • But there are effects that arise precisely because that isn’t exactly true • Ocean tides are one example, and since they’re caused by gravity, we’ll look at them now • We take a simple model, where the universe consists only of the Earth and the moon, and the Earth is covered entirely by water m • R r eD Moon Earth D • The net gravitational force on the element of water m is the sum of the forces due to the Earth and the Moon: GmM GmM F = − E e − m e = m"r" m r2 r R2 R m • In principal, we could solve this equation of motion and determine exactly how this element of water moves • But what we really want to know is how someone on Earth will observe it to move – That is, we want the motion relative to the Earth • The first step is writing the equation of motion for the Earth: GM M Note: both rE and "" = − m E M E rE 2 eD rm are measured in D some inertial frame • Therefore the relative motion is given by: = − "r" "r"m "r"E GM GM GM = − E e − m e + m e r2 r R2 R D2 D • The first term is just the usual acceleration towards the center of the Earth (the one that’s equal to g near the Earth’s surface) • The other terms only exist due to the presence of the Moon • We identify these terms as the tidal acceleration: e e ’ a = −GM ∆ R − D ÷ T m «R2 D2 ◊ Magnitude of the Tidal Force • We can now find the tidal force at any point P on the Earth’s surface: y eD ξ • P Earth’s rotation e R θ To Moon x = − eD
    [Show full text]