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- a strong high-pressure system forms in the desert in the Southwestern U.S.
(e.g. Nevada)
- air sinks in a high-pressure system and warms
- since warm air can hold more moisture than cold air, the sinking
air picks up the little moisture that is provided in the desert
- the relative humidity becomes therefore very low
- using the right-hand rule, airflow in the northern hemisphere in a high-pressure
system is clockwise (anti-cyclonic)
- the resulting winds in San Diego therefore blow from the east
- as the air has to cross the mountains before it reaches the coast, it additionally loses some of its moisture during "orographic lifting" (cooling while going from the desert floor to the mountain top) that it cannot regain in the dry region between the mountains and the coast
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