Downdrift

In phonetics, downdrift (also known as 'automatic downstep') is the cumulative lowering of pitch in the course of a sentence due to interactions among tones in a tonal language. The usual cause of downdrift is when the tones in three successive syllables are H L H. In this case the second high tone tends to be lower than the first. The effect can accumulate so that with each low tone, the pitch of the high tones becomes slightly lower, until the end of the intonational phrase, when the pitch is 'reset'.^[1]

Two basic types of downdrift are found. In one, called discrete downdrift, in which when downstep occurs all tones shift downward, so that their relative difference in pitch remains constant; in the other, called tone terracing, the pitch of the low tone remains at the lower end of the speaker's vocal range, while the other tones shift downward, so that their difference in pitch narrows.

Pitch reset is required in the first instance because the tones approach the lower end of the speaker's comfort range, and in the second because the tonal distinctions of the language start being lost.

Further information: Downstep

References

↑ Connell (2001).

External links

Connell, Bruce (2001). Downdrift, Downstep, and Declination. Typology of African Prosodic Systems Workshop, Bielefeld University, Germany.

Suprasegmentals

Timing	Syllable Mora Metrical foot Vowel reduction

Tone	Tone contour Pitch accent Register Downstep Upstep Downdrift Tone terracing Floating tone Tone sandhi Tone letter

Stress	Secondary stress Vowel reduction Accent

Length	Chroneme Gemination Vowel length Extra-short

Prosody	Intonation (pitch) Pitch contour Pitch reset Stress Rhythm Loudness Prosodic unit Pausa

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