Moist adiabatic ascent and orographic precipitation
An ascending air parcel expands as pressure falls and can cool toward saturation.
Key knowledge
An ascending air parcel expands as pressure falls and can cool toward saturation. Once condensation occurs, latent heat release offsets part of the expansion cooling, so the saturated-parcel lapse differs from a dry adiabatic lapse. Ascent over topography can concentrate precipitation on windward slopes and leave drier descending air downwind.
Conditions and scope
- The saturated lapse is not one universal constant; it depends on thermodynamic conditions and condensate treatment.
- Parcel lapse rate and the environmental temperature profile are different quantities; entrainment and radiation can invalidate an isolated-parcel approximation.
Sources · 1
References
Sources retain their recorded scope. A source link alone does not establish verification of every statement.
Evidence and review
Read the dry/saturated ascent and leeward moisture-loss paragraphs; excluded conflation of environmental and adiabatic lapse rates and fixed illustrative lapse numbers.
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Entry details
Permanent link to this entry ↗- Record identity
- uni-earth-moist-ascent
- Revision
- core.1
- Structured reference record
- University core expansion