Geostrophic balance

{
  "id": "MLC-T-MET-005944",
  "term": "Geostrophic balance",
  "field": "Meteorology and atmospheric science",
  "definition": "A condition in fluid dynamics where the horizontal pressure gradient force is precisely offset by the Coriolis force. This equilibrium leads to a steady flow that is parallel to lines of constant pressure, known as isobars. Geostrophic balance is a theoretical idealization that provides a good first-order description of large-scale atmospheric and oceanic circulation patterns.",
  "url": "https://mlchart.com/terminology/meteorology/geostrophic-balance/"
}