Centripetal acceleration
Term · Meteorology and atmospheric science · MLC-T-MET-004235
The acceleration directed toward the center of curvature that is required to keep an object, such as an air parcel, moving along a curved path. In atmospheric dynamics, this acceleration is the result of an imbalance between the pressure gradient force and the Coriolis force. For a parcel in gradient wind balance, the centripetal acceleration is equal to V²/r, where V is the wind speed and r is the radius of the trajectory's curvature.
| Identifier | MLC-T-MET-004235 |
|---|---|
| Field | Meteorology and atmospheric science |
Record as JSON
{
"id": "MLC-T-MET-004235",
"term": "Centripetal acceleration",
"field": "Meteorology and atmospheric science",
"definition": "The acceleration directed toward the center of curvature that is required to keep an object, such as an air parcel, moving along a curved path. In atmospheric dynamics, this acceleration is the result of an imbalance between the pressure gradient force and the Coriolis force. For a parcel in gradient wind balance, the centripetal acceleration is equal to V²/r, where V is the wind speed and r is the radius of the trajectory's curvature.",
"url": "https://mlchart.com/terminology/meteorology/centripetal-acceleration/"
}
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