Regional Winds Essay - 312 Words

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Regional Winds

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Text Preview Nichole Peterson
Intro to Weather and Climate
16 April 2014
Regional Winds

Pressure differences create temperature differences that drive small regional wind circulations. There are many different kind of winds because there are different temperatures. There are many types of wind including valley breeze and mountain breeze that are very common. Valley breeze occurs early in the day when the sun is facing the mountain side more than the ground in the valley. The air on the mountain warms up and creates an upslope breeze. A mountain breeze happens when the ground at night is cooled more quickly and is colder than the air above it. The air that is in contact with the ground cools then the air slides down the mountain sides and moves into the valleys. Another type of wind is a chinook wind which can cause clouds to form. A chinook wind is a warm dry downslope wind. Air going up and over the mountain is cooled too and then below the dew point. Moisture that is in the air condenses and then releases heat into the rising air on the left side of the mountain. Since the air is cooled to and below its dew point it creates clouds. Once the air reaches the top and starts to descend it gets compressed and causes the air to get warmer. Santa Ana winds are the most known winds. They come from the Great Basin and blow hot wind across California in the fall. High pressure forms over the Great Basin which develops wind circulation and causes some cool air to move downhill toward the coast. The air is then compressed and then warms. These winds can turn any small fire into a huge fire that's why there are many huge wildfires in California. Winds in the desert can also form dust storms or haboobs which happen a lot in Arizona. Show More

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