Gravitational Redshift

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Core Idea

Gravitational redshift is the decrease in frequency (increase in wavelength) of light as it climbs out of a gravitational potential well, and the corresponding blueshift as light falls in. For the Schwarzschild metric, a photon emitted at radius r_e with frequency ν_e is observed at radius r_o with frequency ν_o = ν_e √[(1 - r_s/r_e)/(1 - r_s/r_o)], where r_s = 2GM/c². In the weak-field limit, the fractional shift is Δν/ν ≈ ΔΦ/c², where ΔΦ is the difference in Newtonian gravitational potential. Equivalently, clocks at lower gravitational potentials tick more slowly than clocks at higher potentials. Gravitational redshift was predicted by Einstein from the equivalence principle alone (before the full theory was complete), confirmed by the Pound-Rebka experiment (1959), and is an essential correction in the GPS satellite system.

Explainer

Gravitational redshift can be understood through the equivalence principle without any detailed knowledge of the Schwarzschild metric. Consider a photon emitted upward in a uniformly accelerating elevator. By the time the photon reaches the ceiling, the ceiling is moving faster than the floor was when the photon was emitted (the elevator accelerated during the photon's transit). The ceiling detector therefore sees the photon Doppler-shifted to a lower frequency. By the equivalence principle, the same effect occurs in a uniform gravitational field: a photon climbing up through height Δh acquires a redshift Δν/ν = gΔh/c². This argument was Einstein's original derivation, published in 1907 — eight years before the full field equations.

In the full Schwarzschild geometry, the redshift formula is exact: ν_o/ν_e = √[(1 - r_s/r_e)/(1 - r_s/r_o)]. For an observer at infinity (r_o → ∞) receiving light from radius r_e, this becomes ν_∞/ν_e = √(1 - r_s/r_e). At the event horizon (r_e = r_s), the redshift becomes infinite — photons emitted at the horizon are infinitely redshifted to zero frequency by the time they reach a distant observer. This infinite redshift is why a distant observer sees an infalling object fade and freeze at the horizon rather than crossing it. The formula reduces to the weak-field approximation Δν/ν ≈ ΔΦ/c² when r_s/r << 1, which is the regime relevant for Earth (r_s/R_Earth ≈ 1.4 × 10⁻⁹) and the Sun (r_s/R_Sun ≈ 4.2 × 10⁻⁶).

The equivalence between gravitational redshift and gravitational time dilation is exact. A clock at radius r in the Schwarzschild geometry ticks at a rate dτ = √(1 - r_s/r) dt relative to coordinate time t. Two clocks at different radii r₁ and r₂ therefore have a proper-time ratio dτ₁/dτ₂ = √[(1 - r_s/r₁)/(1 - r_s/r₂)], which is exactly the frequency ratio of light exchanged between them. The lower clock ticks slower, and photons emitted by it arrive at the higher clock with a proportionally lower frequency. These are not two separate effects but one phenomenon viewed from two perspectives: the photon's frequency is determined by the emitter's clock rate as seen by the receiver.

Experimental confirmation of gravitational redshift spans an impressive range of precision. The Pound-Rebka experiment (1959) measured the redshift of ⁵⁷Fe gamma rays over 22.6 meters in the Harvard physics building, confirming the predicted shift of about 2.5 × 10⁻¹⁵ to 10% accuracy. Hydrogen maser clocks flown on rockets (Gravity Probe A, 1976) confirmed the redshift to 7 × 10⁻⁵ precision. Most dramatically, the GPS satellite system provides a continuous, operational test: satellite atomic clocks at 20,200 km altitude gain about 45 μs/day from gravitational time dilation (offset by -7 μs/day from special-relativistic velocity effects), requiring a net correction of about 38 μs/day. Without this relativistic correction, GPS position errors would accumulate at roughly 10 km per day. Modern optical atomic clocks can detect the gravitational redshift between two laboratories separated by just 30 cm of vertical height, pushing precision to the 10⁻¹⁸ level.

Practice Questions 4 questions

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Counting to 10Counting to 20Understanding ZeroThe Number ZeroCounting to FiveOne-to-One CorrespondenceCombining Small Groups Within 5Addition Within 10Addition Within 20Two-Digit Addition Without RegroupingTwo-Digit Addition with RegroupingAddition Within 100Repeated Addition as MultiplicationMultiplication Facts Within 100Division as Equal SharingDivision as Grouping (Measurement Division)Division: Grouping (Repeated Subtraction) ModelDivision: Fair Sharing ModelDivision as Equal SharingDivision as GroupingBasic Division FactsDivision Facts Within 100Two-Digit by One-Digit DivisionDivision with RemaindersRemainders and Quotients in DivisionDivision Word ProblemsIntroduction to Long DivisionFactors and MultiplesPrime and Composite NumbersEquivalent FractionsRelating Fractions and DecimalsDecimal Place ValueReading and Writing DecimalsComparing and Ordering DecimalsAdding and Subtracting DecimalsMultiplying DecimalsDividing DecimalsDividing FractionsMixed Number ArithmeticOrder of OperationsInteger Order of OperationsVariable ExpressionsCombining Like TermsOne-Step EquationsTwo-Step EquationsSolving Multi-Step EquationsEquations with Variables on Both SidesAngle Pairs: Complementary, Supplementary, and VerticalParallel Lines and TransversalsCorresponding AnglesAlternate Interior AnglesTriangle Angle Sum TheoremExterior Angle TheoremTriangle Inequality TheoremSimilar Triangles: AA SimilaritySimilar Triangles: SSS and SAS SimilarityProportions in Similar TrianglesRight Triangle Trigonometry IntroductionTrigonometric Ratios ReviewRadian MeasureConverting Between Degrees and RadiansThe Unit CircleGraphing Sine and CosineGraphing Tangent and Reciprocal Trigonometric FunctionsDerivatives of Trigonometric FunctionsAntiderivativesIterated Integrals and Fubini's TheoremDouble Integrals in Cartesian CoordinatesDouble Integrals over Rectangular RegionsDouble Integrals in Polar CoordinatesDouble Integrals: Definition and SetupIterated Integrals and Fubini's TheoremDouble Integrals over Rectangular RegionsDouble Integrals over General RegionsApplications of Double Integrals: Area, Mass, and MomentsTriple Integrals in Cartesian CoordinatesTriple Integrals in Cylindrical and Spherical CoordinatesChange of Variables and the Jacobian DeterminantApplications of Triple Integrals: Volume and MassVector Fields and Their RepresentationsLine Integrals of Vector FieldsGreen's TheoremSurface Integrals and Flux of Vector FieldsSurface Integrals and Flux of Vector FieldsDivergence Theorem: Flux and OutflowDivergence TheoremElectric FluxGauss's LawConductors in Electrostatic EquilibriumCapacitance and CapacitorsDielectricsDielectric Constant and Relative PermittivityElectric Field Inside Dielectric MaterialsDielectric Materials and PolarizationDielectric Susceptibility and PermittivityEnergy Density in Electric FieldsElectric Current and Current DensityElectrical Resistance and ResistivityOhm's Law and Circuit ElementsElectromotive Force (EMF) and BatteriesKirchhoff's Circuit Laws: Voltage and CurrentDC Circuit Network Analysis MethodsTransient Response in RC CircuitsRC CircuitsLC and RLC CircuitsAC Circuits: FundamentalsImpedance and ReactanceAC Power and ResonanceElectromagnetic WavesPostulates of Special RelativitySpacetime Diagrams and Minkowski GeometryCurved Spacetime and the Metric TensorTensor Calculus in General RelativityChristoffel SymbolsThe Riemann Curvature TensorRicci Tensor and Scalar CurvatureEinstein Field EquationsThe Schwarzschild SolutionGravitational Redshift

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