Geostrophic momentum approximation
Term · Meteorology and atmospheric science · MLC-T-MET-005954
A simplification in atmospheric dynamics where the advection of momentum is calculated using geostrophic velocities, rather than the true wind velocities. This approximation is valid for large-scale, slow-moving atmospheric flows where the Coriolis force and pressure gradient force are nearly balanced. It is often applied in theoretical models of synoptic-scale weather systems.
| Identifier | MLC-T-MET-005954 |
|---|---|
| Field | Meteorology and atmospheric science |
Record as JSON
{
"id": "MLC-T-MET-005954",
"term": "Geostrophic momentum approximation",
"field": "Meteorology and atmospheric science",
"definition": "A simplification in atmospheric dynamics where the advection of momentum is calculated using geostrophic velocities, rather than the true wind velocities. This approximation is valid for large-scale, slow-moving atmospheric flows where the Coriolis force and pressure gradient force are nearly balanced. It is often applied in theoretical models of synoptic-scale weather systems.",
"url": "https://mlchart.com/terminology/meteorology/geostrophic-momentum-approximation/"
}
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