Quasigeostrophic equilibrium
Term · Meteorology and atmospheric science · MLC-T-MET-008245
A state in the atmosphere or ocean where the forces governing large-scale motion are nearly in geostrophic balance, with small departures allowing for slow evolution. This equilibrium is characterized by a near-balance between the Coriolis force and the pressure gradient force. It is a foundational concept in understanding the dynamics of mid-latitude weather systems.
| Identifier | MLC-T-MET-008245 |
|---|---|
| Field | Meteorology and atmospheric science |
| See also | Quasigeostrophic approximation |
Record as JSON
{
"id": "MLC-T-MET-008245",
"term": "Quasigeostrophic equilibrium",
"field": "Meteorology and atmospheric science",
"definition": "A state in the atmosphere or ocean where the forces governing large-scale motion are nearly in geostrophic balance, with small departures allowing for slow evolution. This equilibrium is characterized by a near-balance between the Coriolis force and the pressure gradient force. It is a foundational concept in understanding the dynamics of mid-latitude weather systems.",
"see_also": [
"quasigeostrophic approximation"
],
"url": "https://mlchart.com/terminology/meteorology/quasigeostrophic-equilibrium/"
}
Record 7,624 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.