35  Reading the Spectrogram (macOS)

The spectrogram in the Tabbing song view gives you a rich and powerful visualization of your music. Compared with the flat view of a typical audio waveform, the spectrogram shows you the intensity of notes over time.

By viewing music with the spectrogram, you can deduce all kinds of information that is not at all possible in a waveform display. Here are some examples of spectrograms collected from a Stevie Ray Vaughan guitar performance, demonstrating various techniques that can be gleaned from the spectrogram.

35.1 Vibrato

Vibrato is quite easy to detect, as it typically has a very obvious pattern to it. Capo’s spectrogram doesn’t just tell you that the bend is there—you are also able to deduce both the depth and rate of the vibrato using the spectrogram.

Figure 35.1: The characteristic wobble of a deep, even vibrato.

35.2 Bends

A bend can sometimes look similar to vibrato if it’s done quickly, but the telltale sign of a bend is that two distinct notes have a clear connection between them. By comparison, you won’t see the start and end note held for very long in vibrato, and the pitches often over- or under-shoot the target.

Figure 35.2: Clean bends between two notes will most often appear with this characteristic shape.

35.3 Slides

A slide is usually easier to hear than to see, but Figure 35.3 captures a good clear example of them.

Figure 35.3: The notes in a slide have clear gaps in their path, and the notes all sit cleanly in the semitone spacing—that’s the individual frets getting hit as the player’s finger slides down the fretboard.
Tip

If you’re unsure whether you’re looking at a slide or a bend, the bend will have a more continuous path from the start to the end pitch, because nothing stops the string from producing the notes in between the semitones.

Another dead giveaway is the distance: you’ll rarely find bends that go past 2 semitones, and even fewer go past 3.

35.4 Chords

When a chord is strummed on a guitar, you will often see notes being produced in a group such as the ones pictured below. Using the spectrogram to identify chords like this can help you identify a particular voicing of a chord you hear.

Warning

It’s easy to mistake a set of harmonics for chords, so use your ears to guide your choices.

chords

35.5 Harmonics

When you play a note on most instruments, it will generate many frequencies—not just the one you played. For example, C4 (middle C) has a frequency of 261.6Hz. But if you play a C4 on a piano, you are also creating energy at its 2nd harmonic (523.3Hz, an octave up), its 3rd harmonic (784.9Hz, or G5—a perfect fifth up), and so on.

Most of the time, the loudness of these harmonics drops off. But each instrument will contribute differently to this harmonic energy. In some cases, the fundamental frequency (e.g., 261.6Hz in a C4) doesn’t appear at all!

This is most common with distorted guitars as illustrated in Figure 35.4. While there is clear energy shown from C#6 to D#6, your ears (correctly) interpret this as a C#5/D#5 bend. In situations like these, you follow your ears and mark the entries for a C#5/D#5 bend, despite no clear indication of any energy there.

Figure 35.4: A repeated bend from C#6 to D#6. Harmonics appear 7 semitones (a perfect fifth) up, and 12 semitones (an octave) above the fundamental note that’s being played. The rich harmonic character of the note is characteristic of a distorted guitar tone.