Isothermal

{
  "id": "MLC-T-MET-010573",
  "term": "Isothermal",
  "field": "Meteorology and atmospheric science",
  "definition": "Describing a process or a region in which temperature remains constant. An isothermal layer in the atmosphere is a vertical zone where temperature does not change with an increase in altitude, creating a stable atmospheric condition. This contrasts with the typical tropospheric lapse rate, where temperature decreases with height at an average of 6.5°C per kilometer.",
  "url": "https://mlchart.com/terminology/meteorology/isothermal/"
}