Geostrophic
Term · Meteorology and atmospheric science · MLC-T-MET-005940
Describing a state of atmospheric or oceanic flow where the Coriolis force exactly balances the pressure gradient force. This balance results in winds or currents flowing parallel to isobars or isopycnals, respectively. Geostrophic flow is an idealized condition often approximated in large-scale atmospheric and oceanic dynamics, particularly away from the equator and boundary layers.
| Identifier | MLC-T-MET-005940 |
|---|---|
| Field | Meteorology and atmospheric science |
| See also | Geostrophic wind; Geostrophic equilibrium; Geostrophic balance |
Record as JSON
{
"id": "MLC-T-MET-005940",
"term": "Geostrophic",
"field": "Meteorology and atmospheric science",
"definition": "Describing a state of atmospheric or oceanic flow where the Coriolis force exactly balances the pressure gradient force. This balance results in winds or currents flowing parallel to isobars or isopycnals, respectively. Geostrophic flow is an idealized condition often approximated in large-scale atmospheric and oceanic dynamics, particularly away from the equator and boundary layers.",
"see_also": [
"geostrophic wind",
"geostrophic equilibrium",
"geostrophic balance"
],
"url": "https://mlchart.com/terminology/meteorology/geostrophic/"
}
Record 4,084 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.