In-Depth Notes on Waves and Sound
Waves
Definition: A wave is a disturbance or oscillation that transfers energy through space and matter.
Amplitude ($y$): Displacement or density of the wave.
Wavelength ($\lambda$): Size of the wave.
Wave Velocity: Determined by time taken for one wavelength to pass a point.
Mathematical Descriptions of Waves
Period ($T$): The time for one wavelength to pass a point.
Formula: T = \frac{\lambda}{v}
Frequency ($f$): Number of wavelengths per second.
Formula: f = \frac{v}{\lambda}
Types of Waves
Longitudinal Waves: Particle displacement is parallel to wave direction (e.g., sound waves).
Transverse Waves: Particle displacement is perpendicular to wave direction (e.g., water waves).
Superposition: When two waves meet, they combine to form a new wave (interference).
Constructive Interference: Results in an increase in amplitude.
Destructive Interference: Results in a decrease in amplitude.
The Huygens Principle
Describes how waves propagate.
Formula: S = \frac{LR}{D}
Where $S$ = spread, $L$ = wavelength, $R$ = distance from the opening, $D$ = size of the opening.
Sound Waves
Frequency and Pitch: Higher frequency leads to a higher pitch.
Compression Waves: Movement of molecules creating pressure variations (sound).
Sound travels faster in stiffer materials rather than denser ones.
Beats
Occur due to interference between two sound waves.
Sound Intensity and Decibels
Threshold of Hearing: Intensity level below which sound cannot be perceived.
Example of intensity: I[dB] = 10 \log \frac{2.5 \times 10^{-4}}{1.0 \times 10^{-12}} = 84 dB
Common Sounds:
Rock band (110 dB), Whisper (30 dB), Threshold of pain (140 dB).
Doppler Effect
A change in frequency and wavelength of a wave in relation to an observer moving relative to its source.
Observed with moving vehicles (siren or horn) as the sound source approaches and recedes.
Sound Channel and UFOs
SOFAR Channel: A horizontal layer in the ocean where the speed of sound is at a minimum, allowing sound waves to travel long distances without losing energy.
Earthquakes
Consist of both compression waves (P-waves) which arrive first and shear waves (S-waves) which arrive second.
Equations describing the magnitude of earthquakes:
M = \log \frac{A}{A_0} (\delta)
Where $M$ = magnitude, $A$ = amplitude, $A_0$ = reference amplitude, and $\delta$ = distance from the epicenter.
Water Waves
Behavior of waves is influenced by water depth.
Shallow Water Waves: Wave interacts with the sea floor.
Deep Water Waves: Wave does not interact with the sea floor.
Critical Wave Depth Relationships:
Shallow-water waves behave differently than deep-water waves due to depth.
Tsunamis
Waves caused by underwater disturbances.
Warning time for a tsunami 1000 miles away is about 2.6 hours.
Velocity formula: v \approx \pi 3000m \approx 171m/s \approx 386mph.