Maloja Wind
The Maloja Wind is a Foehn-type mountain wind that occurs in the upper Engadin, an alpine valley located in Switzerland. The wind blows up-valley during the nighttime and down-valley during the day, a deviation of the typical direction of mountain and valley winds. The phenomenon is caused by wind from the Val Bregaglia crossing the Maloja Pass and intruding into the Engadin. The Maloja Wind occasionally produces a weather phenomenon known as the Maloja Snake, a low-lying cloud so named for its long, serpentine shape.
Description
Maloja Wind
The Maloja Wind is a Foehn-type wind that occurs in the upper Engadin in Switzerland. The wind blows up-valley during the nighttime and down-valley during the day, contradicting the typical direction of mountain and valley winds.The phenomenon is caused by wind from the Val Bregaglia crossing the valley's terminus at Maloja Pass and intruding into the adjoining Engadin. The roughly 1 km-wide Maloja Pass creates a box canyon that blocks moist air from the southern Po Valley from entering the Engadin. When combined with the height difference between Val Bregaglia and the Engadin, the rising air from the latter creates a pressure gradient between the high pressure Val Bregaglia and the low pressure Engadin. The air eventually rises over the Maloja Pass and into the Engadin.
The Maloja Wind reaches a velocity of 20 to 30 knots, with the variation resulting from atmospheric conditions as the wind develops. It is generally less intense in evenings due to reduced insolation.