In physics, a gravitational wave is a fluctuation in the curvature of spacetime which propagates as a wave, traveling outward from a moving object or system of objects. Gravitational radiation is the energy transported by these waves. Important examples of systems which emit gravitational waves are binary star systems, where the two stars in the binary are white dwarfs, neutron stars, or black holes.
Although gravitational radiation has not yet been directly detected, it has been indirectly shown to exist. This was the basis for the 1993 Nobel Prize in Physics, awarded for measurements of the Hulse-Taylor binary system.
In Einstein's theory of general relativity, gravity is defined as the curvature of spacetime. This curvature is caused by the presence of massive objects. Roughly speaking, the more massive the object is, the greater the curvature it causes, and hence the more intense the gravity. As massive objects move around in spacetime, the curvature will change to reflect the changed locations of those objects. If the objects move around in a certain way, ripples in spacetime can spread outward like ripples on the surface of a pond. These ripples are gravitational waves.
The simplest example of a strong source of gravitational waves is binary neutron stars. The mass of stars in orbit causes curvature of the spacetime. The cyclical movement of the two extremely massive stars will roil spacetime, much like a boat propeller stirring up water. The waves will spread out through the Universe at the speed of light, never stopping or slowing down.
As these waves pass a distant observer, that observer will find spacetime distorted in a very particular way. Distances between objects will increase and decrease rhythmically as the wave passes. The magnitude of this effect will decrease the farther the observer is from the source. Any gravitational waves expected to be seen on Earth will be quite small; the change in size of any object will never be much more than 1 in 1020. Still, scientists are attempting to measure the effects of these waves using extraordinarily precise experiments.
By measuring these waves, astrophysicists hope to learn about systems that they could not observe with more traditional means such as optical telescopes and radio telescopes. Gravitational waves can penetrate regions that the more familiar waves cannot, providing us with a view of black holes and other mysterious objects in the distant Universe. Using precise measurements of gravitational waves in this way will also allow us to test the general theory of relativity more thoroughly.
In principle, gravitational waves could exist at any frequency. However, very low frequency waves would be impossible to detect, and very high frequency waves have no credible source able to generate detectable waves. Stephen W. Hawking and Werner Israel list different frequency bands for gravitational waves that could be plausibly detected, ranging from 10-7 Hz up to 1011 Hz.
Effects of a passing gravitational waveEdit
Imagine a perfectly flat region of spacetime, with a group of motionless test particles lying in a plane. Then, a weak gravitational wave arrives, passing through the particles along a line perpendicular to the plane of the particles. What happens to the test particles? Roughly speaking, they will oscillate in a "cruciform" manner, as shown in the animations. The area enclosed by the test particles does not change, and there is no motion along the direction of propagation. In the animation at the right, the wave would be passing from you, through the screen, and out the back.
The foregoing animation is the result of a pair of masses that orbit about each other (e.g., black holes) on a circular orbit or a rotating rod or dumbbell. In this case the amplitude, A, of the gravitational wave is a constant, but its plane of polarization changes or rotates (at twice the orbital or rotating-rod rate) and so the time-varying gravitational wave size or periodic spacetime strain h, exhibits a variation as shown in the animation. If the orbit is elliptical or the rotating rod’s centrifugal-force change varies during rotation, then the gravitational wave’s amplitude (that is, the amplitude of the periodic spacetime h), A, actually also varies with time according to an equation called the “quadrupole”.
Like other waves, there are a few useful characteristics describing a gravitational wave:
- Amplitude: Usually denoted , this is the size of the wave — the fraction of stretching or squeezing in the animation. The amplitude shown here is roughly (or 50%). Gravitational waves passing through the Earth are many billion times weaker than this — .
- Frequency: Usually denoted , this is the frequency with which the wave oscillates (1 divided by the amount of time between two successive maximum stretches or squeezes)
- Wavelength: Usually denoted , this is the distance along the wave between points of maximum stretch or squeeze.
- Speed: This is the speed at which a point on the wave (for example, a point of maximum stretch or squeeze) travels. For gravitational waves with small amplitudes, this is equal to the speed of light, .
The frequency, wavelength, and speed are related by the equation c = λ ν, just like the equation for a light wave. For example, the animations shown here oscillate roughly once every two seconds. This would correspond to a frequency of 0.5 Hz, and a wavelength of about 600,000 km, or 47 times the diameter of the Earth.
In the example just discussed, we actually assume something special about the wave. We have assumed that the wave is linearly polarized, with a "plus" polarization, written . Polarization of a gravitational wave is just like polarization of a light wave, except that the polarizations of a gravitational wave are at 45 degrees, as opposed to 90 degrees. In particular, if we had a "cross"-polarized gravitational wave, , the effect on the test particles would be basically the same, but rotated by 45 degrees, as shown in the second animation. Just as with light polarization, the polarizations of gravitational waves may also be expressed in terms of circularly polarized waves. Gravitational waves are polarized because of the nature of their sources. The polarization of a wave actually depends on the angle from the source, as we will see in the next section.
Sources of gravitational wavesEdit
In general terms, gravitational waves are radiated by objects whose motion involves acceleration, provided that the motion is not perfectly spherically symmetric (like a spinning, expanding or contracting sphere) or cylindrically symmetric (like a spinning disk).
A simple example is the spinning dumbbell. Set upon one end, so that one side of the dumbbell is on the ground and the other end is pointing up, the dumbbell will not radiate when it spins around its vertical axis but will radiate if it tumbles end-over-end. The heavier the dumbbell, and the faster it tumbles, the greater is the gravitational radiation it will give off. If we imagine an extreme case in which the two weights of the dumbbell are massive stars like neutron stars or black holes, orbiting each other quickly, then significant amounts of gravitational radiation would be given off.
Some more detailed examples:
- Two objects orbiting each other in a quasi-Keplerian planar orbit (basically, as a planet would orbit the Sun) will radiate.
- A spinning non-axisymmetric planetoid — say with a large bump or dimple on the equator — will radiate.
- A supernova will radiate except in the unlikely event that it is perfectly symmetric.
- An isolated non-spinning solid object moving at a constant speed will not radiate. This can be regarded as a consequence of the principle of conservation of linear momentum.
- A spinning disk will not radiate. This can be regarded as a consequence of the principle of conservation of angular momentum. On the other hand, this system will show gravitomagnetic effects.
- A spherically pulsating spherical star (non-zero monopole moment or mass, but zero quadrupole moment) will not radiate, in agreement with Birkhoff's theorem.
More technically, the third time derivative of the quadrupole moment (or the l-th time derivative of the l-th multipole moment) of an isolated system's stress-energy tensor must be nonzero in order for it to emit gravitational radiation. This is analogous to the changing dipole moment of charge or current necessary for electromagnetic radiation.
Power radiated by the Earth-Sun system Edit
We imagine a simple system of two masses — such as the Earth-Sun system — moving slowly compared to the speed of light. Assume that these two masses orbit each other in a circular orbit in the - plane. To a good approximation, the masses follow simple Keplerian orbits. However, such an orbit represents a changing quadrupole moment. That is, the system will give off gravitational waves.
Suppose that the two masses are and , and they are separated by a distance . The power given off (radiated) by this system is
where G is the Gravitational Constant and , T and v are the kinetic energy, the period time and velocity of the first mass. This is derived from Einstein's quadrupole equation. For a system like the Earth and the Sun, is very large (about 1.5×1011 m) and and are relatively very small (about 2×1030 and 6×1024 kg respectively). Substituting these values into the above equation gives about 313 watts of power radiated by the Earth-Sun system in the form of gravitational waves.
Wave amplitudes from the Earth-Sun systemEdit
We can also think in terms of the amplitude of the wave. Suppose that an observer is positioned at a distance from the center of mass of the system, at spherical coordinates . If the observer is well outside the system (in fact, we need ), the two polarizations of the wave will be
Here, we use the constant angular velocity of a circular orbit in Newtonian physics. Note that the polarization depends on the angle to the system. For example, if the observer is in the - plane then , and , so the polarization is always zero. We also see that the frequency of the wave given off is . If we put in numbers for the Earth-Sun system, we find
In this case, the minimum distance to find waves is light year, so typical amplitudes will be . That is, a ring of particles would stretch or squeeze by just percent.
Radiation from other sourcesEdit
Although the waves from the Earth-Sun system are minuscule, astronomers can point to other sources for which the radiation should be substantial. One important example is the Hulse-Taylor binary — a pair of stars, one of which is a pulsar. The characteristics of their orbit can be deduced from the Doppler shifting of radio signals given off by the pulsar. Each of the stars has a mass about 1.4 times that of the Sun. Also, their orbit is about one seventy-fifth the distance between the Earth and Sun — which means the distance between the two stars is just a few times larger than the diameter of our own Sun. This combination of greater masses and smaller separation means that the energy given off by the Hulse-Taylor binary will be far greater than the energy given off by the Earth-Sun system — roughly times as much.
The information about the orbit can be used to predict just how much energy (and angular momentum) should be given off in the form of gravitational waves. As the energy is carried off, the orbit will change; the stars will draw closer to each other. This effect of drawing closer is called an inspiral, and it can be observed in the pulsar's signals. The measurements on this system were carried out over several decades, and it was shown that the changes predicted by gravitational radiation in general relativity matched the observations very well. In 1993, Russell Hulse and Joe Taylor were awarded the Nobel Prize in Physics for this observation which was the first observational evidence for gravitational waves.
Inspirals are very important sources of gravitational waves. Any time two compact objects (white dwarfs, neutron stars, or black holes) come close to each other, they send out intense gravitational waves. As the objects come closer and closer to each other (that is, as becomes smaller and smaller), the gravitational waves become more and more intense. At some point these waves should become so intense that they can be directly detected by their effect on objects on the Earth. This direct detection is the goal of several large experiments around the world.
The only difficulty is that systems like the Hulse-Taylor binary are so far away. The amplitude of waves given off by the Hulse-Taylor binary as seen on Earth would be roughly . There are some sources, however, that astrophysicists expect to find with the somewhat larger amplitudes of .
Astrophysics and gravitational wavesEdit
Template:Unsolved During the past century, astronomy has been revolutionized by the use of new methods for observing the universe. Astronomical observations were originally made using visible light. Galileo Galilei pioneered the use of telescopes to enhance these observations. However, visible light is only a small portion of the electromagnetic spectrum, and not all objects in the distant universe shine strongly in this particular band. More useful information may be found, for example, in radio wavelengths. Using radio telescopes, astronomers have found pulsars, quasars, and other extreme objects which push the limits of our understanding of physics. Observations in the microwave band have opened our eyes to the faint imprints of the Big Bang, a discovery Stephen Hawking called the "greatest discovery of the century, if not all time". Similar advances in observations using gamma rays, x-rays, ultraviolet light, and infrared light have also brought new insights to astronomy. As each of these regions of the spectrum has opened, new discoveries have been made that could not have been made otherwise. Astronomers hope that the same holds true of gravitational waves.
Gravitational waves have two important and unique properties. First, there is no need for any type of matter to be present nearby in order for the waves to be generated by a binary system of uncharged black holes, which would emit no electromagnetic radiation. Second, gravitational waves can pass through any intervening matter without being scattered. Whereas light from distant stars may be blocked out by interstellar dust, for example, gravitational waves will pass through unimpeded. These two features allow gravitational waves to carry information about astronomical phenomena never before observed by humans.
The sources of gravitational waves described above are in the low-frequency end of the gravitational-wave spectrum (10-7 to 105 Hz). An astrophysical source at the high-frequency end of the gravitational-wave spectrum (above 105 Hz and probably 1010 Hz) generates relic gravitational waves that are theorized to be faint imprints of the Big Bang like the cosmic microwave background. At these high frequencies it is potentially possible that the sources may be “man made” that is, gravitational waves generated and detected in the laboratory.
Energy, momentum, and angular momentum carried by gravitational wavesEdit
Waves familiar from other areas of physics such as water waves, sound waves, and electromagnetic waves are able to carry energy, momentum, and angular momentum. By carrying these away from a source, waves are able to rob that source of its energy, linear or angular momentum. Gravitational waves perform the same function. Thus for example a binary system loses angular momentum as the two orbiting objects spiral towards each other - the angular momentum is radiated away by gravitational waves. The waves can also carry off linear momentum, a possibility that has some interesting implications for Astrophysics. Consider for instance a cluster of stars with a binary black hole system in the center. The holes orbit each other, but their center of mass doesn't move with respect to the cluster at first. However, as the binary inspirals, the radiated gravitational waves carry away linear momentum in some direction. In keeping with Newton's third law of motion, the binary will gain some linear momentum in the opposite direction. Thus, it may be shot out of the cluster.
Gravitational wave detectorsEdit
Though the Hulse-Taylor observations were very important, they were only indirect evidence for gravitational waves. A more interesting observation would be a direct measurement of the effect of a passing gravitational wave. Not only would a direct measurement of gravitational waves rule out other possible (however unlikely) reasons for changes to the orbit of an inspiraling system, it would also provide us more information on the system. Perhaps more importantly, such a detection could give us information about things we can't see with radio or light waves — such as black holes. This would provide us with a rigorous test for Einstein's theory of general relativity.
The great challenge of this type of detection, though, is the extraordinarily small effect the waves would produce on a detector. The amplitude of any wave will fall off as the inverse of the distance from the source (the term in the formulas for above). Thus, even waves from extreme systems like merging binary black holes die out to very small amplitude by the time they reach the Earth. Astrophysicists expect that some gravitational waves passing the Earth may be as large , but generally no bigger. For an object 1 meter in length, this means that its ends would move by meters relative to each other. This distance is about 1 billionth of the width of a typical atom, and roughly one one-hundred-thousandth the width of a proton.
A simple device to detect this motion is called a Weber bar — a large, solid piece of metal with electronics attached to detect any vibrations. This type of instrument was the first type of gravitational wave detector. The idea is to wait for a passing gravitational wave to "ring up" a bar at its resonant frequency, which would basically amplify the wave naturally. Alternatively, a nearby supernova might be strong enough to be seen without resonant amplification. Modern forms of the Weber bar are still operated, cryogenically cooled, with superconducting quantum interference devices to detect the motion. Unfortunately, Weber bars are not sensitive enough to detect anything but extremely powerful gravitational waves.
A more sensitive version is the laser interferometer, with separate masses placed many hundreds of meters to several kilometers apart acting as two ends of a bar. Ground-based interferometers are now operating, and taking data. Currently, the most sensitive is LIGO — the Laser Interferometer Gravitational Wave Observatory. This is actually a set of three devices: one in Livingston, Louisiana; the other two (in the same vacuum tubes) at the Hanford site in Richland, Washington. Each consists of two light storage arms which are 2 to 4 kilometers in length. These are at 90 degree angles to each other, and consist of large vacuum tubes running the entire 4 kilometers. A passing gravitational wave will then slightly stretch one arm as it shortens the other. This is precisely the motion to which an interferometer is most sensitive.
Even with such long arms, a gravitational wave will only change the distance between the ends of the arms by about meters at most. This is still only a fraction of the width of a proton. Nonetheless, LIGO's interferometers are now running routinely at an even better sensitivity level. LIGO's should be able to detect gravitational waves as small as , but needs to wait until a gravitational wave with at least that amplitude passes. Upgrades to LIGO and other detectors such as VIRGO, GEO 600, and TAMA 300 should increase the sensitivity still further — by a factor of up to 100. Another highly sensitive interferometer (LCGT) is currently in the design phase.
All detectors are limited at high frequencies by shot noise, which occurs because the lasers cannot produce photons at an absolutely constant rate. Since there may not be a normal number of photons arriving in a given time interval (for instance in such cases as the laser being momentarily not intense enough), it will be impossible to tell whether a measurement is due to real data, or just random fluctuations in the number of photons. The more independent detectors produce equivalent measurements for any given time period, the more certain experimenters can be that they are getting valid results, i.e., results not influenced by momentary lags in production of photons by a given laser.
All ground-based detectors are also limited at low frequencies by seismic noise, and must be very well isolated from seismic disturbances. Passing cars and trains, falling trees, earthquakes, and even waves crashing on the shore hundreds of miles away are all very significant sources of noise in real interferometers.
Space-based interferometers, such as LISA, are also being developed. LISA's design calls for test masses to be placed five million kilometers apart, in separate spacecraft, with lasers running between them. Because of the distance between the spacecraft, it will be impossible to create light storage arms. Also, the arms will be at 60 degree angles to each other, rather than 90 degree angles. Still, the principle will be the same. Although LISA will not be affected by seismic noise, it will be affected by other noise sources, including noise from cosmic rays and solar wind and — of course — shot noise.
There are other prospects such as MiniGRAIL, a spherical gravitational wave antenna based at Leiden University. Some scientists even want to use the moon as a giant gravitational wave detector. The moon should be somewhat pliable to the contortions caused by gravitational waves, and the hope is that the motion of the moon caused by these waves will be detectable, much like the motion of a Weber bar.
The detectors of gravitational waves described in the foregoing are in the low-frequency end of the gravitational-wave spectrum (10-7 to 105 Hz). There are currently two fabricated high-frequency gravitational wave (HFGW) detectors: one at Birmingham University, England and the other at INFN Genoa, Italy. In addition there are some under development at Chongqing University, China. The Birmingham HFGW high-frequency gravitational wave detector measures changes in the polarization state of a microwave beam (caused by the presence of a gravitational wave or GW) circulating in a closed loop about one meter across. Two have been fabricated and they are currently expected to be sensitive to HFGWs having periodic spacetime strains of , given as an amplitude spectral density. The INFN Genoa detector, or resonant antenna, consists of two coupled, superconducting, spherical, harmonic oscillators a few centimeters in diameter. The oscillators are designed to have (when uncoupled) almost equal resonant frequencies. In theory the system is currently expected to have a sensitivity to HFGWs having periodic spacetime strains of with an expectation to reach a sensitivity of .
The Chongqing University detectors are based upon the GW theory first put forth by Gertsenshtein in 1962. These Chinese detectors aim at the selection and detection of relic high-frequency gravitational waves with the predicted typical parameters νg ~ 1010 Hz (10 GHz) and h ~ 10-30-10-31. The usual Gertsenshtein effect involves the generation of gravitational waves by electromagnetic waves under the influence of a strong static magnetic field. In this case the gravitational waves produced will have the same frequency as the electromagnetic waves producing them. The inverse Gertsenshtein effect, which is alluded to at the end of the paper involves what is termed a synchro-resonance condition. Thus in the Chinese detectors a strong electromagnetic beam (essentially a focused microwave, so called “Gaussian beam”) at the expected frequency, phase and bandwidth of the relic gravitational waves is passed through a strong static magnetic field. There are then produced electromagnetic “detection” photons due to the gravitational waves. These detection photons move off at right angles to the electromagnetic beam and to the direction of the magnetic field. According to theory they move off in both directions and the experimental plan is that they be intercepted by two very sensitive microwave receivers or detectors. Noise is suppressed by keeping the detector at very low temperature (less than 0.048 K) and including superconductor interior baffles and a superconductor enclosure called a “Faraday cage,” both composed of a mosaic of high-temperature superconductor tiles (e.g., YBCO). Similar to the Advanced LIGO, LISA, et al. detectors, these Chinese detectors are in the design phase.
- Main article: Einstein@Home
In some sense, the easiest signals to detect should be constant sources. Supernovae and neutron star or black hole mergers should have larger amplitudes and be more interesting, but their waves will be more complicated. The waves given off by a spinning, bumpy neutron star would be "monochromatic" — like a pure tone in acoustics. It would not change very much in amplitude or frequency.
The Einstein@Home project is a distributed computing project similar to SETI@home intended to detect this type of simple gravitational wave. By taking data from LIGO and GEO, and sending it out in little pieces to thousands of volunteers for analysis on their home computers, Einstein@Home can sift through the data far more quickly than would be possible otherwise. Searches for gravitational waves from other types of systems require large supercomputers running for long periods.
A simple computer program can be downloaded to any home computer, and acts as a screen saver to use computer time that would otherwise be wasted. The program automatically downloads the data, analyzes it while the screen saver is running, and sends the final results back to a central computer.
Einstein's equations form the fundamental law of general relativity. The curvature of spacetime can be expressed mathematically using the metric tensor — denoted . The metric holds information regarding how distances are measured in the space under consideration. Because the propagation of gravitational waves through space and time change distances, we will need to use this to find the solution to the wave equation.
With some simple assumptions, Einstein's equations can be rewritten to show explicitly that they are just wave equations. To begin with, we adopt some coordinate system, like . We define the "flat-space metric" to be the quantity which — in this coordinate system — has the components we would expect for the flat space metric. For example, in these spherical coordinates, we have
This flat-space metric has no physical significance; it is a purely mathematical device necessary for the analysis. Tensor indices are raised and lowered using this "flat-space metric".
This is the crucial field, which will represent the radiation. It is possible (at least in an asymptotically flat spacetime) to choose the coordinates in such a way that this quantity satisfies the "de Donder" gauge conditions (conditions on the coordinates):
where represents the flat-space d'Alembertian operator, and represents the stress-energy tensor plus quadratic terms involving . This is just a wave equation for the field with a source, despite the fact that the source involves terms quadratic in the field itself. That is, it can be shown that solutions to this equation are waves traveling with velocity 1 in these coordinates.
The equations above are valid everywhere — near a black hole, for instance. However, because of the complicated source term, the solution is generally too difficult to find analytically. We can often assume that space is nearly flat, so the metric is nearly equal to the tensor. In this case, we can neglect terms quadratic in , which means that the field reduces to the usual stress-energy tensor . That is, Einstein's equations become
If we are interested in the field far from a source, however, we can treat the source as a point source; everywhere else, the stress-energy tensor would be zero, so
Now, this is the usual homogeneous wave equation — one for each component of . Solutions to this equation are well known. For a wave moving away from a point source, the radiated part (meaning the part that dies off as far from the source) can always be written in the form , where is just some function. It can be shown that — to a linear approximation — it is always possible to make the field traceless. Now, if we further assume that the source is positioned at , the general solution to the wave equation in spherical coordinates is
where we now see the origin of the two polarizations.
Relation to the sourceEdit
If we know the details of a source — for instance, the parameters of the orbit of a binary — we can relate the source's motion to the gravitational radiation observed far away. With the relation
Though it is possible to expand the Green's function in tensor spherical harmonics, it is easier to simply use the form
where the positive and negative signs correspond to ingoing and outgoing solutions, respectively. Generally, we are interested in the outgoing solutions, so
If the source is confined to a small region very far away, to an excellent approximation we have:
Now, because we will eventually only be interested in the spatial components of this equation (time components can be set to zero with a coordinate transformation), and we are integrating this quantity — presumably over a region of which there is no boundary — we can put this in a different form. Ignoring divergences with the help of Stokes' theorem and an empty boundary, we can see that
Inserting this into the above equation, we arrive at
Finally, because we have chosen to work in coordinates for which , we know that . With a few simple manipulations, we can use this to prove that
With this relation, the expression for the radiated field is
In the linear case, , the density of mass-energy.
To a very good approximation, the density of a simple binary can be described by a pair of delta-functions, which eliminates the integral. Explicitly, if the masses of the two objects are and , and the positions are and , then
We can use this expression to do the integral above:
Using mass-centered coordinates, and assuming a circular binary, this is
where . Plugging in the known values of , we obtain the expressions given above for the radiation from a simple binary.
- General Relativity
- Linearised Einstein field equations
- LIGO, VIRGO, GEO 600, and TAMA 300 — Gravitational wave detectors
- LISA the proposed Laser Interferometer Space Antenna.
- Big Bang Observer (BBO), proposed successor to LISA.
- Sticky bead argument, for a physical way to see that gravitational radiation should carry energy.
- pp-wave spacetime, for an important class of exact solutions modeling gravitational radiation.
- Hawking Radiation, for gravitationally induced electromagnetic radiation from black holes
- ↑ 1.0 1.1 Hawking, S. W. and Israel, W., General Relativity: An Einstein Centenary Survey, Cambridge University Press, Cambridge, 1979, 98.
- ↑ 2.0 2.1 Landau, L. D. and Lifshitz, E. M., The Classical Theory of Fields. Fourth Revised English Edition, Pergamon Press., 1975, 356-357.
- ↑ Einstein, A., “The quadrupole formula.” Sitzungsberichte, Preussische Akademie der Wisserschaften, 154, (1918).
- ↑ L. P. Grishchuk (1976), “Primordial Gravitons and the Possibility of Their Observation,” Sov. Phys. JETP Lett. 23, p. 293.
- ↑ Braginsky, V. B., Rudenko and Valentin, N. Section 7: “Generation of gravitational waves in the laboratory,” Physics Report (Review section of Physics Letters), 46, No. 5. 165-200, (1978).
- ↑ Li, Fangyu, Baker, R. M L, Jr., and Woods, R. C., “Piezoelectric-Crystal-Resonator High-Frequency Gravitational Wave Generation and Synchro-Resonance Detection,” in the proceedings of Space Technology and Applications International Forum (STAIF-2006), edited by M.S. El-Genk, American Institute of Physics Conference Proceedings, Melville NY 813: 2006.
- ↑ For a review of early experiments using Weber bars, see Levine, J. (April 2004). "Early Gravity-Wave Detection Experiments, 1960-1975". Physics in Perspective (Birkhäuser Basel) 6 (1): 42–75. doi:10.1007/s00016-003-0179-6.
- ↑ Gertsenshtein, M. E., “Wave resonance of light and gravitational waves,” Soviet Physics JETP, 14, No. 1, 84-85, (1962).
- ↑ Einstein@Home
- ↑ 10.0 10.1 Thorne, Kip (April 1980). "Multipole expansions of gravitational radiation". Reviews of Modern Physics 52.
- ↑ C. W. Misner, K. S. Thorne, and J. A. Wheeler (1973). Gravitation, W. H. Freeman and Co..
- Chakrabarty, Indrajit, "Gravitational Waves: An Introduction". arXiv:physics/9908041 v1, Aug 21, 1999.
- Landau, L. D. and Lifshitz, E. M., The Classical Theory of Fields (Pergamon Press),(1987).
- Will, Clifford M., The Confrontation between General Relativity and Experiment. Living Rev. Relativity 9 (2006) 3.
- Caltech's Physics 237-2002 Gravitational Waves by Kip Thorne Video plus notes: Graduate level but does not assume knowledge of General Relativity, Tensor Analysis, or Differential Geometry; Part 1: Theory (10 lectures), Part 2: Detection (9 lectures)
- www.astronomycast.com January 14th, 2008 Episode 71: Gravitational Waves
- Laser Interferometer Gravitational Wave Observatory. LIGO Laboratory, California Institute of Technology.
- Einstein's Messengers - The LIGO Movie by NSF
- Home page for Einstein@Home project, a distributed computing project processing raw data from LIGO Laboratory, searching for gravity waves
- The National Center for Supercomputing Applications -- a numerical relativity group
- Caltech Relativity Tutorial -- A basic introduction to gravitational waves, and astrophysical systems giving off gravitational waves
- Resource Letter GrW-1: Gravitational waves -- a list of books, journals and web resources compiled by Joan Centrella for research into gravitational waves
- Mathematical and Physical Perspectives on Gravitational Radiation -- written by B F Schutz of the Max Planck Institute explaining the significance and background of some key concepts in gravitational radiation
- Binary BH Merger -- estimating the radiated power and merger time of a BH binary using dimensional analysis