Audited ·Last updated 29 Jul 2026·7 citations·Tier 2·0 uses

Gravitational Time Dilation Calculator

Exact Schwarzschild time dilation between two static clocks, or one clock versus infinity. Microseconds per day, redshift, and the weak-field error.

Gravitational Time Dilation Calculator

Compare against what?
SI kilograms. Earth 5.97217 × 10²⁴ (PDG 2024) · Sun 1.98841 × 10³⁰ · Jupiter 1.89812 × 10²⁷ · a 10-solar-mass black hole 1.98841 × 10³¹. Must be greater than zero.
Distance from the centre of the mass, not the altitude above its surface. The default 26 561 750 m is the GPS orbit semi-major axis (Ashby 2003); Earth's equatorial radius is 6 378 137 m (WGS-84). Must be outside the event horizon.
Used in the two-clock route: the clock everything is compared against. Default 6 378 137 m, Earth's WGS-84 equatorial radius. If this is smaller than your clock's radius, your clock runs fast and the result is positive.
How long to accumulate the difference over. Only scales the total-seconds output; the microseconds-per-day and fractional figures are independent of it.
Clock gain (µs per day)
45.6519
How many microseconds per day your clock gains on the reference clock. Positive means your clock runs fast (it is higher in the potential). Gravitational term only — no motion, no oblateness, no rotation.
Fractional rate difference
0
Rate ratio dτ₁ ⁄ dτ₂
1
Total difference over the period (s)
0
Clock gain (s per year)
0.0167
Gravitational redshift z
-0
Schwarzschild radius of the body (m)
0.0089
r ÷ r_s for your clock
2,994,540,628.38
Weak-field approximation of the ratio
1
Weak-field relative error
0
Conventions and limits for this result
Exact Schwarzschild form, √(1 − r_s/r), for STATIC observers only: zero spin, zero charge, no frame dragging. A positive result means the clock at your chosen radius runs FAST relative to the reference clock. This is the GRAVITATIONAL term alone — kinematic (special-relativistic) time dilation from motion is NOT included, and for an orbiting clock it works the other way and partly cancels it. Nor is a planet's oblateness or the centrifugal potential of a rotating frame included: for a clock on Earth's surface, the point-mass value GM/(Rc²) used here is 0.227% smaller than the adopted geoid value. Because the ratio sits within about 10⁻⁹ of 1 for any weak field, read the fractional difference and the microseconds-per-day figure rather than the ratio itself — a double-precision number cannot carry the ratio's small digits.

Background.

A clock deeper in a gravitational field runs slow. Not apparently, not as a measurement artefact — it accumulates less proper time, permanently and cumulatively. This calculator gives the exact Schwarzschild answer: the ratio √(1 − r_s/r₁) ÷ √(1 − r_s/r₂) between two static clocks at different distances from a spherical mass, or between one static clock and a reference at infinity, expressed as a fractional rate, as microseconds per day, as seconds per year, and as the gravitational redshift of light travelling between them.

The page defaults to the example that made the effect an engineering problem rather than a curiosity. A GPS satellite at a semi-major axis of 26 561 750 m, compared with a clock on Earth's equator at 6 378 137 m, gains 45.65 microseconds per day. Left uncorrected, that error alone would move a GPS fix by about thirteen kilometres in a day. GPS satellites therefore ship with their clocks deliberately set slow — the interface specification IS-GPS-200 fixes the offset at Δf/f = −4.4647 × 10⁻¹⁰, so a 10.23 MHz oscillator is built to run at 10.22999999543 MHz.

That published number is not the one this page prints, and the difference is worth understanding before you use the result. **This calculator gives the gravitational term only.** GPS clocks are also moving, and kinematic special-relativistic dilation slows them by 7.21 microseconds a day, so the net is 38.58 µs/day — which is exactly what the −4.4647 × 10⁻¹⁰ factory offset absorbs. On top of that, the reference clock for GPS is not a point-mass surface but the rotating geoid, whose effective potential includes Earth's oblateness and the centrifugal term. Ashby's adopted value Φ₀/c² = 6.969290134 × 10⁻¹⁰ is 0.227% larger than the point-mass GM/(Rc²) = 6.953487 × 10⁻¹⁰ this page uses, which is why 45.65 here versus 45.79 in the GPS literature. Both numbers are correct for what they describe; the page states which one it is computing.

The formula used is the exact one, not the familiar first-order approximation. Textbooks usually write 1 − GM/(rc²), which is the leading term of √(1 − r_s/r). For Earth the two are indistinguishable — they differ by about 6 × 10⁻¹⁹ — but they diverge fast in a strong field. At ten Schwarzschild radii the approximation is wrong by 1.4 × 10⁻³, at three Schwarzschild radii by 2.1 × 10⁻², and at 1.0001 r_s it is wrong by a factor of 49, returning 0.50 where the exact answer is 0.0100. This calculator computes both, prints their relative difference, and warns you whenever you are inside ten horizon radii.

There are limits on what "static" means here. The Schwarzschild solution describes a non-rotating, uncharged mass, and this page describes observers who hover at a fixed radius rather than orbiting. A rotating body drags spacetime (the Kerr metric) and an orbiting clock carries a velocity term; neither is included. There is also a hard domain edge. No static observer can exist at or inside the event horizon, where the tick rate reaches zero and the redshift diverges, so a radius at or below r_s raises an error rather than returning a number — that is not a numerical guard, it is the physics.

Two independent measurements calibrate the page's arithmetic. Chou and colleagues at NIST measured a fractional clock-rate change of (4.1 ± 1.6) × 10⁻¹⁷ when one optical clock was raised 33 centimetres above another; this engine returns 3.5977 × 10⁻¹⁷ for exactly that geometry, inside their error bar and equal to the Newtonian gh/c². At the other extreme, the Sun's surface produces a gravitational redshift of z = 2.1225 × 10⁻⁶, the value spectroscopists have quoted for a century as an equivalent 636 m/s Doppler shift. One tabletop, one stellar, six orders of magnitude apart, both reproduced.

What is gravitational time dilation calculator?

Gravitational time dilation is the difference in the rate at which two clocks accumulate proper time because they sit at different gravitational potentials. In the Schwarzschild geometry of a static, spherically symmetric mass, a clock held at radius r ticks at √(1 − r_s/r) times the rate of coordinate time, where r_s = 2GM/c² is the Schwarzschild radius. Comparing two such clocks gives the ratio this calculator returns.

It is not an illusion and it is not symmetric, unlike the reciprocal time dilation of special relativity between two inertial frames. Bring the two clocks back together and the one that spent time deeper in the well will genuinely show less elapsed time. This has been measured directly — with aircraft-borne caesium clocks (Hafele–Keating, 1971), with rocket-borne masers (Gravity Probe A, 1976), and in the laboratory over a height difference of 33 centimetres (Chou et al., 2010).

The same factor governs gravitational redshift. Light emitted at radius r₁ with proper frequency ν arrives at radius r₂ with its frequency scaled by exactly the clock-rate ratio, so z = 1/ratio − 1. Light climbing out of a potential well is redshifted; light falling in is blueshifted. Pound and Rebka measured this over 22.5 metres of a Harvard tower in 1959.

What it is not: it is not kinematic (velocity) time dilation, which is a separate special-relativistic effect that this page deliberately excludes; it is not frame dragging, which requires the Kerr metric; and the radius it takes is a distance from the centre of the mass, not an altitude above a surface.

How to use this calculator.

  1. Choose whether to compare two clocks at different radii, or one clock against a reference at infinity.
  2. Enter the mass of the gravitating body in kilograms.
  3. Enter the radius of your clock, measured from the centre of the mass — not its altitude above the surface.
  4. In the two-clock route, enter the reference radius as well. A reference below your clock gives a positive result: your clock runs fast.
  5. Set the elapsed period if you want a total in seconds; the microseconds-per-day and fractional outputs do not depend on it.
  6. Read the fractional rate difference rather than the ratio — the ratio is so close to 1 in any weak field that a floating-point number cannot show its digits.
  7. Check the conventions note before quoting anything. It states that only the gravitational term is included, and flags strong-field results where the familiar approximation fails.

The formula.

dτ⁄dt = √(1 − r_s ⁄ r) · ratio = √(1 − r_s⁄r₁) ⁄ √(1 − r_s⁄r₂) · r_s = 2GM⁄c² · z = 1⁄ratio − 1 · weak field: 1 − (GM⁄c²)(1⁄r₁ − 1⁄r₂)

The Schwarzschild line element gives the proper time of a clock at rest at radius r as dτ = √(1 − r_s/r) dt, where t is the coordinate time kept by a clock infinitely far away and r_s = 2GM/c². Comparing two static clocks divides one such factor by the other, and the coordinate time cancels: ratio = √(1 − r_s/r₁) ÷ √(1 − r_s/r₂). Setting r₂ to infinity reduces the denominator to 1. Everything else on the page is a restatement: the fractional difference is ratio − 1, the microseconds per day is that times 86 400 × 10⁶, the seconds per year is that times a Julian year of exactly 31 557 600 s, and the redshift is z = 1/ratio − 1 because a light wave's period is stretched by exactly the inverse of the emitting clock's rate.

Expanding the square root to first order in r_s/r gives the familiar textbook form 1 − GM/(rc²). The calculator computes this alongside the exact value and reports the relative difference between them, so the approximation's failure is visible rather than assumed. At Earth's surface the difference is about 2 × 10⁻¹⁹, which is far below anything measurable. At ten Schwarzschild radii it is 1.4 × 10⁻³. At three Schwarzschild radii — the innermost stable circular orbit — the exact factor is √(2/3) = 0.8165 while the approximation says 0.8333, a 2.1% error. At 1.0001 r_s the exact factor is 0.009999 and the approximation says 0.5000, wrong by a factor of 49.

Units and dimensions. Mass in kilograms, both radii in metres from the centre of the mass, elapsed period in days. The ratio, the fractional difference, r/r_s and z are all dimensionless; r_s comes out in metres because GM/c² has dimensions (m³ kg⁻¹ s⁻² × kg) ÷ (m² s⁻²) = m. The dimensional guard the test suite runs is that at exactly four Schwarzschild radii the ratio must equal √3/2 and at three it must equal √(2/3), both pure numbers with no constants in them.

Rounding stage. No intermediate rounding: forty significant digits throughout, rounded once at the return boundary. The two near-unity ratios round to eighteen decimal places, which is already beyond what an IEEE-754 double can represent — a double near 1.0 resolves about 2 × 10⁻¹⁶, so for Earth-scale problems the ratio's meaningful digits do not survive at all. That is precisely why the fractional difference is computed as a separate quantity in high precision and returned at twelve significant digits, and why the page tells you to read it instead of the ratio.

Significant figures. Five digits at most. Everything inherits G's 2.2 × 10⁻⁵ relative uncertainty, and any real-world application inherits much larger modelling error from the effects this page excludes.

Invalid-domain behaviour. A radius at or inside the Schwarzschild radius raises a field error naming the horizon radius, because the tick rate is exactly zero at r = r_s, the redshift is infinite there, and inside it no observer can hover at any cost — the radial direction is timelike. Zero or negative mass, zero or negative radius, and a zero or negative elapsed period each raise their own field error. One threshold attaches a note rather than an error: a clock inside ten Schwarzschild radii is flagged as strong-field, with the exact and approximate values shown side by side. That ten-radius edge is a presentation convention chosen for this page, not a published threshold.

A worked example.

Example

Put a clock on the surface of the Sun and compare it with one infinitely far away. The Sun's Schwarzschild radius is r_s = 2GM/c² = 2953.25 m, and its nominal radius is 6.957 × 10⁸ m, so r/r_s = 235 571. The tick-rate factor is √(1 − 1/235571) = 0.99999787749503932, meaning the solar clock runs slow by a fractional 2.1225 × 10⁻⁶ — it loses 0.18338 seconds every day, or 67 seconds a year. The same factor read as a redshift gives z = 1/0.999997877 − 1 = 2.1225 × 10⁻⁶. Multiplied by c, that is an equivalent Doppler velocity of 636 m/s, which is the number solar spectroscopists have quoted since the 1920s and the quantity that had to be disentangled from convective motions before the solar gravitational redshift could be confirmed. The weak-field approximation is off by only 2.3 × 10⁻¹² here, because even the Sun's surface is 235 000 horizon radii out. Now the two checks that pin the engine to published measurements, neither of which was used to build it. **Tabletop.** Chou, Hume, Rosenband and Wineland (Science, 2010) raised one aluminium-ion optical clock 33 centimetres above another and measured a fractional rate change of (4.1 ± 1.6) × 10⁻¹⁷. Enter Earth's mass 5.97217 × 10²⁴ kg with r₁ = 6 378 137.33 m and r₂ = 6 378 137 m and this calculator returns 3.5977 × 10⁻¹⁷ — inside their uncertainty, and identical to the Newtonian gh/c² with g = GM/R² = 9.7983 m/s². Over a day the raised clock gains 3.1 picoseconds. **Orbital.** The page's default configuration — Earth's mass, a GPS satellite at 26 561 750 m against a ground clock at 6 378 137 m — returns +45.652 µs/day. The independent cross-check runs like this. Ashby's adopted geoid potential is Φ₀/c² = 6.969290134 × 10⁻¹⁰; this page's own GM/(r c²) at the satellite is 1.66971 × 10⁻¹⁰; the difference, 5.29958 × 10⁻¹⁰, is +45.788 µs/day of gravitational gain. The Keplerian orbital speed √(GM/r) = 3873.83 m/s gives a kinematic term v²/2c² = 8.34853 × 10⁻¹¹ = −7.213 µs/day. Their difference is 4.464732 × 10⁻¹⁰ — and IS-GPS-200 specifies the satellite clock offset as exactly 4.4647 × 10⁻¹⁰, agreement to five significant figures with a US government signal specification. In microseconds per day that is 38.575. So the page's 45.652 and the literature's 45.788 differ by 0.3%, entirely because the geoid's effective potential includes Earth's oblateness and the centrifugal term while a point-mass Schwarzschild model does not. That is a real limitation of the model, quantified rather than hidden, and it is stated in the note attached to every result.

radius M695,700,000
elapsed Days1
mass Kg1,988,410,000,000,000,000,000,000,000,000
solve ForversusInfinity
reference Radius M6,378,137

Frequently asked questions.

What is the gravitational time dilation formula?
For a static clock at radius r outside a spherical mass M, the exact Schwarzschild result is dτ/dt = √(1 − r_s/r) with r_s = 2GM/c². Comparing two static clocks gives √(1 − r_s/r₁) ÷ √(1 − r_s/r₂). The familiar textbook version, 1 − GM/(rc²), is the first term of expanding that square root; it is excellent in any weak field and badly wrong close to a horizon. This calculator uses the exact form and shows you the approximation alongside it.
Why does GPS need a relativistic correction?
Because the satellite clocks run fast enough to destroy the navigation solution within hours. GPS positioning works by timing signals, so a timing error of Δt becomes a range error of cΔt. The gravitational effect alone is about 45.7 µs/day; the net effect after subtracting the kinematic term is 38.6 µs/day, which corresponds to roughly 11.6 kilometres of range error accumulated in a single day. The system handles it by building the satellite oscillators to run slow: IS-GPS-200 specifies a fractional offset of −4.4647 × 10⁻¹⁰, so a nominal 10.23 MHz clock is manufactured at 10.22999999543 MHz.
Why does this page give 45.65 µs/day when the GPS literature says 45.7?
Because they are computing slightly different things, and the 0.3% gap is real. This page models Earth as a point mass in the Schwarzschild metric, giving GM/(Rc²) = 6.953487 × 10⁻¹⁰ at the surface. The GPS literature compares against the rotating geoid, whose effective potential also contains Earth's oblateness (the J₂ term) and the centrifugal potential of the rotating frame; Ashby's adopted value for that is Φ₀/c² = 6.969290134 × 10⁻¹⁰, 0.227% larger. Neither is wrong — one is a point-mass idealisation and the other is a real planet. The page states which it is using, and the difference is quantified in the conventions note.
Does this include time dilation from motion?
No, deliberately. This is the gravitational term only. Kinematic time dilation from velocity is a separate special-relativistic effect that works in the opposite direction for an orbiting clock and partially cancels the gravitational gain. For GPS the split is +45.7 µs/day gravitational and −7.2 µs/day kinematic, netting +38.6. If you need the total for a moving clock you must add the velocity term yourself, using √(1 − v²/c²) for the local speed measured in the frame you care about.
What happens at the event horizon?
The tick rate √(1 − r_s/r) reaches exactly zero and the redshift diverges, so a distant observer sees an infalling clock slow asymptotically and its light redden without bound. Inside the horizon there is no static solution at all — the radial direction becomes timelike, so no observer can hover at any radius no matter how much thrust they have. The calculator therefore raises an error for any radius at or inside r_s rather than returning a number, and names the horizon radius in the message. That is the physics, not a numerical guard.
Has gravitational time dilation actually been measured?
Repeatedly, over eighteen orders of magnitude of field strength. Pound and Rebka detected the gravitational redshift over 22.5 metres of a Harvard tower in 1959. Hafele and Keating flew caesium clocks around the world in 1971 and recovered the predicted combination of gravitational and kinematic effects. Gravity Probe A flew a hydrogen maser to 10 000 km in 1976 and confirmed the prediction to about 1.4 × 10⁻⁴. Chou and colleagues at NIST measured it in 2010 across a 33-centimetre height difference on a laboratory table, obtaining (4.1 ± 1.6) × 10⁻¹⁷ where this calculator returns 3.60 × 10⁻¹⁷. And GPS corrects for it continuously in every receiver on Earth.
Why is the rate ratio displayed as 1.000000000…?
Because in any weak field it genuinely is that close to 1, and a double-precision floating-point number cannot represent the difference. Near 1.0 a double resolves about 2 × 10⁻¹⁶, while Earth-surface dilation is around 7 × 10⁻¹⁰ and the 33-centimetre laboratory effect is 3.6 × 10⁻¹⁷ — below the resolution entirely. That is why the calculator computes the fractional difference as its own high-precision quantity and returns it separately. Read the fractional difference and the microseconds per day; treat the ratio as decoration.
When does the weak-field approximation stop working?
Sooner than most people expect, and the page shows you exactly where. The relative error of 1 − GM/(rc²) against the exact √(1 − r_s/r) is about 2 × 10⁻¹⁹ at Earth's surface, 1.4 × 10⁻³ at ten Schwarzschild radii, 2.1 × 10⁻² at three Schwarzschild radii (the innermost stable circular orbit, where the exact factor is √(2/3) = 0.8165 and the approximation says 0.8333), and a factor of 49 at 1.0001 r_s. The calculator prints both values and their relative difference on every result, and adds a strong-field warning inside ten horizon radii — an edge chosen for this page rather than taken from a published standard.
Does a spinning body change the answer?
Yes, and this page does not model it. Schwarzschild geometry assumes zero spin. A rotating mass drags spacetime around with it, described by the Kerr metric, which adds frame-dragging terms and makes the answer depend on the observer's angular position and direction of motion. For Earth the effect is tiny — Gravity Probe B measured the frame-dragging precession at about 37 milliarcseconds per year — but near a rapidly spinning black hole it dominates. Treat this page as exact for a non-rotating body and as an approximation for a rotating one.

References& sources.

  1. [1]Ashby, N. (2003), "Relativity in the Global Positioning System", Living Reviews in Relativity 6, 1; open-access full text retrieved 2026-07-29 via PubMed Central. Source of the adopted geoid potential Φ₀/c² = 6.969290134 × 10⁻¹⁰ used for Terrestrial Time, of the GPS semi-major axis a = 2.656175 × 10⁷ m used as this page's default orbital radius, and of the statement that "the standard clock in orbit is beating too fast, primarily because its frequency is gravitationally blueshifted", with the adjusted proper frequency of 10.229 999 995 43 MHz. Peer-reviewed; open access.
  2. [2]Chou, C. W., Hume, D. B., Rosenband, T. and Wineland, D. J. (2010), "Optical Clocks and Relativity", Science 329, 1630–1633. Measured a fractional clock-rate change of (4.1 ± 1.6) × 10⁻¹⁷ for a 33 cm change in height between two aluminium-ion optical clocks. This is the second, independent authority used to verify the engine at the weak-field extreme: the page returns 3.5977 × 10⁻¹⁷ for exactly that geometry. Peer-reviewed; paywalled at Science, abstract freely visible; the NIST press release describing the same result is open.
  3. [3]US Space Force / GPS Directorate, Interface Specification IS-GPS-200, "Navstar GPS Space Segment / Navigation User Interfaces", §3.3.1.1 SV Carrier and Clock Rates. Specifies that the space-vehicle clock rates are offset by Δf/f = −4.4647 × 10⁻¹⁰, equivalent to Δf = −4.5674 × 10⁻³ Hz on the 10.23 MHz reference, giving 10.229 999 995 43 MHz, "to compensate for relativistic effects". A government signal specification and therefore independent of the physics literature; consulted 2026-07-29 via the official GPS.gov / NAVCEN document set. Freely published.
  4. [4]NIST/CODATA 2022 fundamental constants, retrieved 2026-07-29: G = 6.674 30(15) × 10⁻¹¹ m³ kg⁻¹ s⁻² (relative standard uncertainty 2.2 × 10⁻⁵) and c = 299 792 458 m s⁻¹ (exact). Standards body; open access.
  5. [5]Particle Data Group (Workman et al.), Review of Particle Physics, "Astrophysical Constants and Parameters", Table 2.1, revised August 2023; 2024 PDF retrieved 2026-07-29. Source of the default Earth mass 5.97217(13) × 10²⁴ kg and the solar mass 1.98841(4) × 10³⁰ kg, and independently prints the Schwarzschild radii of both bodies (8.870056 mm and 2.9532501 km), which this page reproduces. Open access.
  6. [6]Pound, R. V. and Rebka, G. A. (1960), "Apparent Weight of Photons", Physical Review Letters 4, 337. The first terrestrial measurement of the gravitational frequency shift, over 22.5 m. Peer-reviewed; paywalled at APS. Historical reference — no number is taken from it.
  7. [7]Vessot, R. F. C., et al. (1980), "Test of Relativistic Gravitation with a Space-Borne Hydrogen Maser", Physical Review Letters 45, 2081. Gravity Probe A, confirming the gravitational redshift to about 1.4 × 10⁻⁴. Peer-reviewed; paywalled at APS. Cited for the measurement history only.

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