Sinusoidal Response: Magnitude and Phase Angle

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Core Idea

When a linear system is excited by sinusoidal input u(t) = A sin(ωt), steady-state output is y(t) = A|G(jω)| sin(ωt + ∠G(jω)). The magnitude |G(jω)| and phase ∠G(jω) of the transfer function at frequency ω completely characterize the system's steady-state sinusoidal response.

Explainer

You already know from transfer functions that G(s) maps Laplace-domain inputs to Laplace-domain outputs. Sinusoidal response is what happens when you evaluate this on the imaginary axis — substituting s = jω. At any frequency ω, G(jω) is a complex number. The magnitude |G(jω)| tells you how much the system scales the amplitude of a sinusoidal input at that frequency; the phase angle ∠G(jω) tells you how much the output lags or leads the input.

The result is clean: for a stable linear system driven by u(t) = A sin(ωt), the steady-state output is always y(t) = A|G(jω)| sin(ωt + ∠G(jω)). The system cannot generate new frequencies — it can only amplify or attenuate and shift in time. This follows from linearity and the eigenfunction property of complex exponentials: sinusoids are the natural "eigenfunctions" of linear time-invariant systems, in the same way that eigenvectors are the natural inputs for linear transformations.

To compute |G(jω)| and ∠G(jω) at a specific frequency, substitute s = jω into G(s) and treat the result as a complex number. For a transfer function G(s) = (s + 2)/((s + 1)(s + 5)), evaluating at ω = 3 gives G(3j) = (3j + 2)/((3j + 1)(3j + 5)). Compute numerator and denominator separately, multiply out the denominator, then divide. The magnitude is the ratio of absolute values: |numerator|/|denominator|. The phase is the difference of arguments: ∠numerator − ∠denominator. At low frequencies (ω → 0), G(jω) → G(0), the DC gain. At high frequencies, physical systems with more poles than zeros have magnitude that falls off because the denominator grows faster.

This sinusoidal characterization is the foundation for all frequency-domain design methods. Every point on a Bode plot — the magnitude in dB and phase in degrees — is just |G(jω)| and ∠G(jω) evaluated at many values of ω. The Nyquist plot traces the path of G(jω) in the complex plane as ω sweeps from 0 to ∞. These plots become your primary tools for assessing stability margins, understanding bandwidth, and designing compensators. The ability to read magnitude and phase directly from G(jω) at any specific frequency is the entry skill for all of that analysis.

Practice Questions 5 questions

Prerequisite Chain

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 CircuitsSecond-Order Transient Circuit ResponseFeedback Control FundamentalsLaplace Transform Methods for ControlTransfer Functions and System ModelingSinusoidal Response: Magnitude and Phase Angle

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