A painted one-minute tour of the analyzer's physics: semitone ratios, cents, beats and wavelength, then the history and sources behind each number.
Why does a song tuned to four thirty-two hertz sound slightly different? This analyzer puts the modern standard, A four forty, side by side with lower historic tunings. Every other note is built from A. Each semitone multiplies the frequency by the twelfth root of two, so retuning A slides the whole keyboard by the same ratio. Musicians measure that slide in cents, a hundred to a semitone. Four thirty-two sits about thirty-two cents below four forty, a third of a semitone. Baroque pitch, four fifteen, is about one semitone lower. Play both A's together and you hear beats. The two waves drift in and out of step, so the loudness swells eight times a second: the difference between four forty and four thirty-two. Temperature changes the wave, not the note. Warm air carries sound faster, so one cycle of A four forty stretches from about seventy-five centimeters at freezing to about eighty-one on a forty degree day. Four forty is simply the shared reference, written into an international standard. Turn on dual play and listen for the beats yourself.
A 1939 international conference recommended A = 440 Hz. ISO adopted it in 1955 and reaffirmed it in 1975 as ISO 16, which asks for tuning within 0.5 Hz.
France fixed A at 435 Hz in 1859 (the diapason normal). Baroque ensembles today often play at A = 415 Hz, about a semitone below modern pitch. 'Scientific pitch' sets C = 256 Hz, which puts A near 430.54 Hz.
Hertz counts cycles per second, and the second is a human-defined unit. A432 is a legitimate tuning choice, but nothing in acoustics makes it more natural than 440.
An octave is 1,200 cents and a semitone 100. Adults reliably hear a 25-cent difference side by side, and under good conditions people can detect about 5 to 6 cents, so A432 against A440 is clearly audible when compared directly.
Two tones a few hertz apart swell and fade at a rate equal to their difference. Tuning removes the beats: when the swelling stops, the two pitches match.
Wavelength equals the speed of sound divided by frequency. The tool uses v = 331.3 + 0.606 × T (m/s, T in °C), so heat changes the wavelength while the pitch you hear stays the same.
Sets A = 440 Hz for the note A in the treble stave.
History of A440, the 1859 French diapason normal, Baroque pitch, scientific pitch and 'Verdi tuning'.
Definition of the cent and research on how small a pitch difference people can hear.
Why the beat frequency equals the difference between the two frequencies.
How the speed of sound depends on the gas and its temperature.
All numbers in the video come from the analyzer's own formulas: equal temperament from A4, cents = 1200 × log2(f2/f1), beat rate = |f1 − f2|, and the tool's speed-of-sound approximation.