Scientifically, a Chinook wind is a föhn wind—a dry, warm, down-slope wind that occurs on the lee side of a mountain range. As moist air from the Pacific Ocean travels eastward, it is forced upward by the Rocky Mountains, cooling and condensing to release precipitation on the windward slopes. Having lost its moisture, the air descends on the eastern side, compressing and heating rapidly. This process can cause dramatic temperature spikes; it is not uncommon for the temperature to rise by 20 to 30 degrees Celsius (40 to 50 degrees Fahrenheit) in a matter of minutes.
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Cinevood's Stream App Hint - Free APK Download for Android - AppBrain This process can cause dramatic temperature spikes; it
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