Favogn
Term · Meteorology and atmospheric science · MLC-T-MET-005549
A warm, dry, downslope wind occurring on the leeward side of the Alps. This wind results from air descending and warming adiabatically after losing its moisture on the windward slopes. The term is the Romansh name for the Foehn wind, specifically as it is experienced in the valleys of the Graubünden canton of Switzerland.
| Identifier | MLC-T-MET-005549 |
|---|---|
| Field | Meteorology and atmospheric science |
Record as JSON
{
"id": "MLC-T-MET-005549",
"term": "Favogn",
"field": "Meteorology and atmospheric science",
"definition": "A warm, dry, downslope wind occurring on the leeward side of the Alps. This wind results from air descending and warming adiabatically after losing its moisture on the windward slopes. The term is the Romansh name for the Foehn wind, specifically as it is experienced in the valleys of the Graubünden canton of Switzerland.",
"url": "https://mlchart.com/terminology/meteorology/favogn/"
}
Record 3,442 of 10,703 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.