(meteorology) A temperature inversion produced by the adiabatic warming of a layer of subsiding air; this inversion is enhanced by vertical mixing in the air layer below the inversion.
subsidence inversion
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(səb′sīd·əns in′vər·zhən)
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 | foehn phase (meteorology) |
| inversion |
| Temperature inversion (meteorology and climatology) |
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Mentioned in
- foehn phase (meteorology)
- inversion
- Temperature inversion (meteorology and climatology)
- Convection
- Inversion (meteorology)
- Great Langton
- Northallerton
