写真素材 - Stau and Föhn, Orographic lift. Strong upward currents of air are formed on the windward side (Stau). After crossing the ridge the air precipitates downwards the air heats up (Föhn)
Stau and Föhn, Orographic lift. Strong upward currents of air are formed on the windward side (Stau). After crossing the ridge the air precipitates downwards the air heats up (Föhn)