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- W1977263237 abstract "The winter storms which invade northern California originate through the interaction of Polar Pacific Air with Tropical Pacific Air. This happens when the polar low-pressure areas are forced farther south than usual or the semi-permanent high-pressure areas just north of the Hawaiian Islands break down. Waves induced along this polar front or discontinuity-surface between these two areas travel eastward across California. The passage of a family of as many as five such waves or storms has been noted. The development of the frontal system associated with these storms or low-pressure areas is accompanied by heavy precipitation from the moisture-laden Tropical Pacific Air." @default.
- W1977263237 created "2016-06-24" @default.
- W1977263237 creator A5054725984 @default.
- W1977263237 date "1941-01-01" @default.
- W1977263237 modified "2023-10-05" @default.
- W1977263237 title "Storm-characteristics of the Sacramento basin" @default.
- W1977263237 doi "https://doi.org/10.1029/tr022i001p00111" @default.
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