WORD OF THE WEEK 💬 Foehn — (Or föhn.) A warm, dry, downslope wind descending the lee side of the Alps as a result of synoptic-scale, cross-barrier flow over the mountain range. The winds are often strong and gusty, sometimes forming downslope windstorms as a result of mountain wave activity. The air in the near-surface flow originates at or above the main crest height of the Alpine barrier, and achieves its warmth and dryness as a result of adiabatic descent. Read more about foehn through the A
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Spain - Sept. 2025 "Foehn Effect" Foehn Effect is a type of wind pattern that pushes a warm, unstable air mass upwards over mountains where it cools and condenses into a low cloud layer. This effect is usually accompanied on the leeward side by a strong adiabatic warming when the dry air separates out as it descends down the mountainside. The adiabatic warming occurs as a result of the air mass being compressed by increasing atmospheric pressure as it descends down the mountain. Video credit: Jo
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This river of clouds is actually a meteorological phenomenon known as a foehn (German for hairdryer). It happens when humid cold air masses are blown down by a wind perpendicular to a mountain range. | Yahoo News
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