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115 pages, Paperback
First published October 1, 1962
A cross section of California, illustrating how San Francisco's summer weather is famously dominated by advection fog. Three key factors:
1) The jet stream (upper arrows) move relatively warm moist air to the coast of California.
2) The water just offshore is coming from the far north (due to the Coriolis effect) and chills the moist air above it, creating a long-lasting marine layer.
3) High summer temperatures in the Central Valley create a low pressure system as the air rises, pulling that marine layer air up the Sacramento River Valley past San Francisco (and other low passes in the Coastal Range).
The result is fog and winds whenever temperatures are high inland. (Click on the picture below to see this phenomena if you aren’t familiar with it.)

Exactly what the title says, except far more interesting and well-written than it sounds.