MLchartDataset catalogue

Quasi-hydrostatic approximation

Term · Meteorology and atmospheric science · MLC-T-MET-008248

An assumption in atmospheric dynamics where the vertical acceleration is considered negligible compared to the gravitational force and the vertical pressure gradient force. This simplifies the equations of motion by reducing the vertical momentum equation to a hydrostatic balance. It is valid for atmospheric motions with horizontal scales much larger than their vertical scales, such as synoptic-scale weather systems.

Table 1. Record
IdentifierMLC-T-MET-008248
FieldMeteorology and atmospheric science
Synonymsquasi-hydrostatic assumption; hydrostatic approximation
See alsoFiltering approximations
Record as JSON
{
  "id": "MLC-T-MET-008248",
  "term": "Quasi-hydrostatic approximation",
  "field": "Meteorology and atmospheric science",
  "definition": "An assumption in atmospheric dynamics where the vertical acceleration is considered negligible compared to the gravitational force and the vertical pressure gradient force. This simplifies the equations of motion by reducing the vertical momentum equation to a hydrostatic balance. It is valid for atmospheric motions with horizontal scales much larger than their vertical scales, such as synoptic-scale weather systems.",
  "synonyms": [
    "quasi-hydrostatic assumption",
    "hydrostatic approximation"
  ],
  "see_also": [
    "filtering approximations"
  ],
  "url": "https://mlchart.com/terminology/meteorology/quasi-hydrostatic-approximation/"
}

Record 7,627 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.