During the summer, a high-pressure system often parks itself over the region, sinking air that warms as it descends. Sinking Air and Compressed Heat The process begins with atmospheric dynamics aloft.
Understanding the Central Valley Heat Trap and Sinking Air
According to the laws of physics, compressing a gas increases its temperature, so this descending air warms significantly before it even reaches Bakersfield. Furthermore, high-pressure systems encourage clear skies, allowing maximum solar radiation to reach the ground throughout the day.
Urban Heat and Surface Characteristics Human activity and the built environment in Bakersfield further amplify the natural heat. The Central Valley Heat Trap At the heart of the explanation lies the Central Valley geography, where Bakersfield sits roughly in the middle.
The Central Valley Geography and Atmospheric Dynamics Behind the Heat
As air descends from the mountains into the valley, it compresses due to increasing atmospheric pressure. Moreover, prolonged drought conditions reduce soil moisture, making the ground less effective at cooling through evaporation.
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