Indirect circulation
Term · Meteorology and atmospheric science · MLC-T-MET-006504
An atmospheric circulation where the air parcels move in a direction opposite to what would be expected from thermal forcing, meaning warm air sinks and cold air rises. This type of circulation requires an external energy source to maintain itself against buoyancy forces. The Ferrel cell in the mid-latitudes is an example of an indirect circulation.
| Identifier | MLC-T-MET-006504 |
|---|---|
| Field | Meteorology and atmospheric science |
Record as JSON
{
"id": "MLC-T-MET-006504",
"term": "Indirect circulation",
"field": "Meteorology and atmospheric science",
"definition": "An atmospheric circulation where the air parcels move in a direction opposite to what would be expected from thermal forcing, meaning warm air sinks and cold air rises. This type of circulation requires an external energy source to maintain itself against buoyancy forces. The Ferrel cell in the mid-latitudes is an example of an indirect circulation.",
"url": "https://mlchart.com/terminology/meteorology/indirect-circulation/"
}
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