Orographic rainfall

{
  "id": "MLC-T-MET-007739",
  "term": "Orographic rainfall",
  "field": "Meteorology and atmospheric science",
  "definition": "Rainfall that occurs when moist air is forced to rise over mountains, leading to adiabatic cooling, condensation, and the formation of rain. This process is a major contributor to precipitation totals in many mountainous areas worldwide. The intensity and distribution of orographic rainfall are influenced by mountain height, slope, and prevailing wind direction.",
  "see_also": [
    "rainfall"
  ],
  "url": "https://mlchart.com/terminology/meteorology/orographic-rainfall/"
}