Barotropic vorticity equation
Term · Meteorology and atmospheric science · MLC-T-MET-003835
A simplified form of the vorticity equation that describes the evolution of absolute vorticity in a two-dimensional, incompressible, and inviscid fluid. This equation assumes that density depends only on pressure, meaning there are no horizontal temperature or density gradients. It is often used to model large-scale atmospheric flows where vertical variations are negligible, such as in forecasting the movement of longwaves in the upper troposphere.
| Identifier | MLC-T-MET-003835 |
|---|---|
| Field | Meteorology and atmospheric science |
| See also | Equivalent barotropic model |
Record as JSON
{
"id": "MLC-T-MET-003835",
"term": "Barotropic vorticity equation",
"field": "Meteorology and atmospheric science",
"definition": "A simplified form of the vorticity equation that describes the evolution of absolute vorticity in a two-dimensional, incompressible, and inviscid fluid. This equation assumes that density depends only on pressure, meaning there are no horizontal temperature or density gradients. It is often used to model large-scale atmospheric flows where vertical variations are negligible, such as in forecasting the movement of longwaves in the upper troposphere.",
"see_also": [
"equivalent barotropic model"
],
"url": "https://mlchart.com/terminology/meteorology/barotropic-vorticity-equation/"
}
Record 1,005 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.