Laplace equation
Term · Meteorology and atmospheric science · MLC-T-MET-006871
A second-order partial differential equation, ∇²φ = 0, where ∇² is the Laplacian operator and φ is a scalar function. This equation describes steady-state phenomena where there are no sources or sinks, such as the distribution of electric potential in a charge-free region or the steady-state temperature distribution in a medium without heat sources. In meteorology, it can be applied to problems involving potential flow.
| Identifier | MLC-T-MET-006871 |
|---|---|
| Field | Meteorology and atmospheric science |
| See also | Poisson equation |
Record as JSON
{
"id": "MLC-T-MET-006871",
"term": "Laplace equation",
"field": "Meteorology and atmospheric science",
"definition": "A second-order partial differential equation, ∇²φ = 0, where ∇² is the Laplacian operator and φ is a scalar function. This equation describes steady-state phenomena where there are no sources or sinks, such as the distribution of electric potential in a charge-free region or the steady-state temperature distribution in a medium without heat sources. In meteorology, it can be applied to problems involving potential flow.",
"see_also": [
"Poisson equation"
],
"url": "https://mlchart.com/terminology/meteorology/laplace-equation/"
}
Record 5,439 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.