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- W2552203440 abstract "The detailed precipitation pattern observed during the 1971–75 period revealed similar general features found in long-term records. The summer rainfall increased from west to east across St. Louis, reaching a maximum east and north of the Mississippi River. The precipitation maximum was located northeast and east of the urban heat island centered on the commercial district of the St. Louis inner city. The heat island was associated with a humidity deficit in the same general area. Annual precipitation patterns showed a great deal of similarity, particularly the east side location of the maximum. The diurnal distribution of rainfall reflected the diurnal cycle typical of the climatic regime of the area. The shape of the diurnal curve for stations within the area of maximum rainfall was similar to that for those located in the rainfall minimum west of St. Louis. Since the diurnal structure of the rainfall distribution was independent of the rainfall amount, it suggests repeated enhancement of precipitation within storms moving across the urban area. The surface winds were perturbed as revealed by the unique signature of wind speed cross-sections showing increases then decreases across the city. The same signature appeared in both daytime and nighttime winds indicating that the perturbation was not primarily caused by the heat island which maximized at night. Severe weather events including heavy rainstorms, hail and wind gusts all showed a maximum in the region of the east side rainfall maximum. Thunder, a frequent precursor of severe weather, also showed a maximum in occurrence and intensity over the city and east of the Mississippi River." @default.
- W2552203440 created "2016-11-30" @default.
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- W2552203440 date "1981-01-01" @default.
- W2552203440 modified "2023-10-18" @default.
- W2552203440 title "Surface Weather Conditions" @default.
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- W2552203440 doi "https://doi.org/10.1007/978-1-935704-29-4_2" @default.
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