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Wave Energy and Intensity

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Wave Properties: Wavelength, Frequency, and AmplitudeEnergy Transport and Wave Intensity+1 more→→Coastal Processes: Wave Refraction, Erosion, and DepositionOcean Surface Waves: Generation and Properties+2 more
wave energy intensity amplitude inverse square law power

Core Idea

The energy carried by a wave is proportional to the square of its amplitude: E ∝ A². Intensity (power per unit area, I = P/A) is likewise proportional to A². For a point source radiating in three dimensions, intensity decreases as the inverse square of distance: I ∝ 1/r². This inverse-square law is a purely geometric result — the same power spreads over a larger spherical surface as r increases. Amplitude therefore decreases as 1/r.

How It's Best Learned

Measure the loudness (approximately ∝ intensity) of a sound source at distances 1m, 2m, and 4m from the source. Verify that intensity roughly quarters each time distance doubles.

Common Misconceptions

Explainer

From kinetic energy, you know that energy scales with the square of velocity: KE = ½mv². Waves carry energy by making particles oscillate, and the maximum speed of those oscillating particles is proportional to amplitude A — a larger displacement means faster oscillatory motion. Combining these two ideas gives the foundational result: wave energy is proportional to the square of amplitude, E ∝ A². This quadratic relationship is the reason a wave twice as tall carries four times the energy, not twice. The same logic applies to intensity — the power delivered per unit area of wavefront — so I ∝ A² as well. Doubling the amplitude of a sound wave quadruples its perceived loudness in physical terms, which is why acoustics uses a logarithmic decibel scale to make the range of human hearing manageable.

Intensity is defined as power per unit area: I = P/A (where A here is area, not amplitude). Imagine a point source radiating power uniformly in all directions. At distance r, that fixed total power P is spread over the surface area of a sphere: 4πr². Since I = P/(4πr²), intensity falls off as 1/r². This is the inverse-square law, and it is a purely geometric result — the energy doesn't disappear, it just spreads over an ever-larger surface as the wavefront expands. Double the distance from a campfire and the warmth you feel drops to one-quarter; move three times as far and it drops to one-ninth.

The amplitude consequence follows directly. Since I ∝ A² and I ∝ 1/r², combining them gives A ∝ 1/r. Amplitude decreases linearly with distance for a spherical wave in three dimensions. This is why you can shout across a room but not across a football field — the same vocal power spreads over a sphere that is thousands of times larger in area. Whispers carry even less power to begin with, making the 1/r² fall-off doubly unforgiving.

It is important to note the geometric assumption embedded in the inverse-square law. It holds for waves that radiate isotropically into three dimensions. Surface waves on water, confined to two dimensions, spread over a circular perimeter 2πr rather than a spherical surface 4πr², so intensity falls as 1/r instead of 1/r². Waves on a string are one-dimensional — they carry the same intensity everywhere along the string, ignoring damping. Whenever you apply the inverse-square law, verify that the wave is genuinely radiating in three-dimensional open space; beams, waveguides, and acoustic horns deliberately break the 3D assumption to prevent the energy loss that would otherwise occur.

Practice Questions 5 questions

Prerequisite Chain

Understanding Zero → The Number Zero → Counting to Five → Counting to 10 → Counting to 20 → Counting a Set of Objects Up to 20 → Cardinality: The Last Number Counted → Matching Numerals to Quantities → Subitizing Small Quantities → Addition Within 10 → Number Bonds to 10 → Addition Within 20 → Doubles and Near Doubles → Doubles Facts Within 10 → Near Doubles Facts Within 20 → Mental Math Strategies for Addition → Mental Math: Adding and Subtracting Tens → Addition Within 100 → Repeated Addition as Multiplication → Multiplication as Equal Groups → Multiplication: Arrays → Basic Multiplication Facts (0s, 1s, 2s, 5s, 10s) → Multiplication Facts Within 100 → Division as Equal Sharing → Division as Grouping (Measurement Division) → Division: Grouping (Repeated Subtraction) Model → Division: Fair Sharing Model → Division as Equal Sharing → Division as Grouping → Basic Division Facts → Division Facts Within 100 → Multiplication and Division Fact Families → Relationship Between Multiplication and Division → Division Facts as Inverse of Multiplication → Remainders and Quotients in Division → Division Word Problems → Multi-Step Word Problems → Solving Multi-Step Word Problems → Multiplication Word Problems → Division Word Problems → Introduction to Long Division → Factors and Multiples → Prime and Composite Numbers → Equivalent Fractions → Relating Fractions and Decimals → Decimal Place Value → Integers and the Number Line → Comparing and Ordering Integers → Absolute Value → Adding Integers → Subtracting Integers → Multiplying Integers → Dividing Integers → Unit Rates → Proportions → Percent Concept → Converting Between Fractions, Decimals, and Percents → Operations with Rational Numbers → Two-Step Equations → Solving Multi-Step Equations → Equations with Variables on Both Sides → Angle Pairs: Complementary, Supplementary, and Vertical → Parallel Lines and Transversals → Corresponding Angles → Alternate Interior Angles → Triangle Angle Sum Theorem → Exterior Angle Theorem → Triangle Inequality Theorem → Similar Triangles: AA Similarity → Similar Triangles: SSS and SAS Similarity → Proportions in Similar Triangles → Right Triangle Trigonometry Introduction → Sine, Cosine, and Tangent Ratios → Trigonometric Ratios Review → Radian Measure → Converting Between Degrees and Radians → The Unit Circle → Graphing Sine and Cosine → Graphing Tangent and Reciprocal Trigonometric Functions → Derivatives of Trigonometric Functions → Antiderivatives → Indefinite Integrals → Basic Integration Rules → Riemann Sums → Definite Integral Definition → Fundamental Theorem of Calculus Part 1 → Fundamental Theorem of Calculus Part 2 → U-Substitution → Separable Equations (Intro) → Separable Differential Equations → Integrating Factor Method for First-Order Linear ODEs → First-Order Linear Ordinary Differential Equations → Second-Order Linear Homogeneous Differential Equations → Characteristic Equation Method for Linear ODEs → Repeated Roots and Reduction of Order → Wronskian and Linear Independence → Method of Undetermined Coefficients → Higher-Order Linear Differential Equations → Systems of First-Order Linear Differential Equations → Separation of Variables for Partial Differential Equations → The Wave Equation and Vibrating Strings → The One-Dimensional Wave Equation → Harmonic Waves and Sinusoidal Form → Particle Velocity in Wave Motion → Energy Transport and Wave Intensity → Wave Energy and Intensity

Longest path: 106 steps · 660 total prerequisite topics

Prerequisites (3)

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