Foehn cloud
Term · Meteorology and atmospheric science · MLC-T-MET-005670
A type of cloud, often lenticular or wave-shaped, that forms on the lee side of mountains due to the lifting and cooling of air as it encounters the mountain barrier, even as the air descends and warms further downwind. These clouds are indicative of a foehn wind event. They can appear as stationary, stacked layers.
| Identifier | MLC-T-MET-005670 |
|---|---|
| Field | Meteorology and atmospheric science |
| See also | Bishop wave; Chinook arch; Contessa di vento; Moazagotl |
Record as JSON
{
"id": "MLC-T-MET-005670",
"term": "Foehn cloud",
"field": "Meteorology and atmospheric science",
"definition": "A type of cloud, often lenticular or wave-shaped, that forms on the lee side of mountains due to the lifting and cooling of air as it encounters the mountain barrier, even as the air descends and warms further downwind. These clouds are indicative of a foehn wind event. They can appear as stationary, stacked layers.",
"see_also": [
"Bishop wave",
"chinook arch",
"contessa di vento",
"Moazagotl"
],
"url": "https://mlchart.com/terminology/meteorology/foehn-cloud/"
}
Record 3,694 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.