Rossby regime

{
  "id": "MLC-T-MET-008611",
  "term": "Rossby regime",
  "field": "Meteorology and atmospheric science",
  "definition": "An atmospheric flow regime where the dynamics are primarily governed by the propagation and interaction of Rossby waves, characterized by a relatively small Rossby number. In this regime, the Coriolis force and pressure gradient force are largely in balance, leading to quasi-geostrophic motion. This regime is typical of large-scale atmospheric circulation in mid-latitudes.",
  "url": "https://mlchart.com/terminology/meteorology/rossby-regime/"
}