MLchartDataset catalogue

Frontal inversion

Term · Meteorology and atmospheric science · MLC-T-MET-001089

  1. A temperature inversion that occurs at the boundary between two air masses of different temperatures, typically found above a cold air mass where warmer air is overriding it. This stable layer inhibits vertical air movement and can trap pollutants or moisture below it. It is a common feature associated with warm fronts and occluded fronts.

  2. A temperature inversion that develops aloft when warm air overruns the cold air behind a front.

Table 1. Record
IdentifierMLC-T-MET-001089
FieldMeteorology and atmospheric science
ReferencesNWS Glossary
Record as JSON
{
  "id": "MLC-T-MET-001089",
  "term": "Frontal inversion",
  "field": "Meteorology and atmospheric science",
  "definitions": [
    "A temperature inversion that occurs at the boundary between two air masses of different temperatures, typically found above a cold air mass where warmer air is overriding it. This stable layer inhibits vertical air movement and can trap pollutants or moisture below it. It is a common feature associated with warm fronts and occluded fronts.",
    "A temperature inversion that develops aloft when warm air overruns the cold air behind a front."
  ],
  "references": [
    "NWS Glossary"
  ],
  "url": "https://mlchart.com/terminology/meteorology/frontal-inversion/"
}

Record 3,889 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.