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During the winter, mountain valleys are prone to the development of "temperature inversions". They are called "inversions" because they are "upside-down" situations. Typically the temperature of the atmosphere gets colder as you get farther away from the Earth's surface. However, during an inversion, air at the surface is much colder than the air above it. Its a winter thing . . . The photo on top shows an inversion that was present in the Helena Valley of Montana for several days during late December of 2001. The boundary between the colder air below and the warmer clear air above is very distinct. The bottom photo shows the same valley several weeks later. The "Sleeping Giant" can be seen on the horizon. Like a big baked potato . . . CLICK HERE to watch a 2-minute YouTube video, showing a temperature inversion in the Helena Valley during late December 2009. Term: inverted |
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*More about inversions |
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*Inversion in Hawaii |
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The Nature Conservancy of Montana |
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Next picture of the week |
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Earth Science Teacher at Helena High School |