yθ360°720°

Variable Adjuster

Amplitude (A)2
0.54
Frequency (B)1
0.54
Phase Shift (C)
0360

Auto-Sweep Engine

2x

Sine & Cosine Waves

WAVE

Sinusoidal waves demonstrate how circular motion transitions into a linear coordinate wave over time. A point rotating at a constant rate maps its vertical (sine) or horizontal (cosine) displacement directly to the wave curve.

y=Asin(Bθ+C)y = A \sin(B\theta + C)

Whiteboard Solver Steps

Step 1

Wave Equation Setup

A sinusoidal wave is characterized by its mathematical function: - AA is the Amplitude (vertical scaling / height of peaks): current A=2A = 2. - BB is the Frequency multiplier (how squished or stretched the wave cycles are): current B=1B = 1. - CC is the Phase shift (horizontal displacement / left-right shift): current C=0=0.0000 radC = 0^\circ = 0.0000\text{ rad}.

y=Asin(Bθ+C)ory=Acos(Bθ+C)y = A \sin(B\theta + C) \quad \text{or} \quad y = A \cos(B\theta + C)
Step 2

Wave Period & Wavelength Calculation

The period (TT) is the horizontal span required to complete one full cycle of the wave. Since a base cycle of sine/cosine spans 360360^\circ (2π2\pi radians), a frequency of B=1B = 1 means the wave completes a full cycle in exactly 360.0360.0^\circ.

T=360B=3601=360.0(or 2πB rad)T = \frac{360^\circ}{B} = \frac{360^\circ}{1} = 360.0^\circ \quad (\text{or } \frac{2\pi}{B} \text{ rad})
Step 3

Evaluate Wave Equation

By feeding angular input values (θ\theta) into the trigonometric function, we calculate the vertical displacement (yy) at each stage, plotting the continuous wave curve across the grid.

y(θ)=2×sine(1θrad+0.0000)y(\theta) = 2 \times \text{sine}(1 \cdot \theta_{rad} + 0.0000)