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Transverse Mountain Range |
Credit & Copyright:
Dr. Bruce G. Marcot
Explanation: Below us is a beautiful example of the rain shadow effect, whereby high mountains block moisture-laden air, forming an arid environment with scant rainfall. This week we are flying north along the Transverse Mountain Range of southern California -- more specifically, the San Bernadino Mountains. To the left (the west) is a low fog overcast coming in from off the Pacific coast and filling the Los Angeles Basin ... but it is neatly blocked by the San Bernadinos so that virtually none of this moisture gets to the east side to the arid interior of Lucerne and Apple Valleys. Rain shadows are found in many parts of the world where linear mountain ranges block moist prevailing winds. Here is another outstanding example I photographed on the arid southeastern "back" side of Mount Kenya in Kenya, east Africa:
Back in California, studies have shown how some rain shadow effects can lead to flooding on one side and protection of cities and people on the other, as with the rain shadow caused by the Santa Lucia Mountains protecting the city of Santa Cruz along the central coast range of the state (Ralph et al. 2003).
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Next week's picture:
El Tatio Geysers of the Atacama
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