MLchartDataset catalogue

Saturation level

Term · Meteorology and atmospheric science · MLC-T-MET-008659

The altitude at which a rising parcel of unsaturated air becomes saturated, typically due to adiabatic cooling. At this level, the air's temperature cools to its dew point temperature, and condensation begins to occur. The saturation level is a key indicator for cloud base formation.

Table 1. Record
IdentifierMLC-T-MET-008659
FieldMeteorology and atmospheric science
Record as JSON
{
  "id": "MLC-T-MET-008659",
  "term": "Saturation level",
  "field": "Meteorology and atmospheric science",
  "definition": "The altitude at which a rising parcel of unsaturated air becomes saturated, typically due to adiabatic cooling. At this level, the air's temperature cools to its dew point temperature, and condensation begins to occur. The saturation level is a key indicator for cloud base formation.",
  "url": "https://mlchart.com/terminology/meteorology/saturation-level/"
}

Record 8,183 of 10,702 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.