Along-valley winds
Term · Meteorology and atmospheric science · MLC-T-MET-003451
Air currents that flow parallel to the orientation of a valley, driven by thermal differences between the valley atmosphere and the surrounding terrain. During the day, anabatic winds blow up-valley as the valley floor heats faster, while at night, katabatic winds flow down-valley as the valley cools more rapidly. These winds are a type of mesoscale circulation.
| Identifier | MLC-T-MET-003451 |
|---|---|
| Field | Meteorology and atmospheric science |
| See also | Anabatic wind; Katabatic wind |
Record as JSON
{
"id": "MLC-T-MET-003451",
"term": "Along-valley winds",
"field": "Meteorology and atmospheric science",
"definition": "Air currents that flow parallel to the orientation of a valley, driven by thermal differences between the valley atmosphere and the surrounding terrain. During the day, anabatic winds blow up-valley as the valley floor heats faster, while at night, katabatic winds flow down-valley as the valley cools more rapidly. These winds are a type of mesoscale circulation.",
"see_also": [
"anabatic wind",
"katabatic wind"
],
"url": "https://mlchart.com/terminology/meteorology/along-valley-winds/"
}
Record 423 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.