Katabatic Wind
A downslope wind driven by gravity acting on air that has become colder and denser than its surroundings over elevated ground.
Cooling over a plateau, snowfield, glacier or mountain slope creates dense air that drains into valleys and coastal waters. Terrain can channel and accelerate the flow, sometimes producing sudden strong gusts near shore.
Katabatic describes the driving mechanism, not automatically the wind’s temperature at its destination or a particular compass direction. Forecasts, topography and local warning signs remain important.
