Urban, Topographic and Diurnal Effects on Rainfall in the St. Louis Region
Open Access
- 1 May 1978
- journal article
- Published by American Meteorological Society in Journal of Applied Meteorology
- Vol. 17 (5) , 565-577
- https://doi.org/10.1175/1520-0450(1978)017<0565:utadeo>2.0.co;2
Abstract
Analyses were made of the summer rainfall distribution (June-August) in 17 areas within the METROMEX network in St. Louis region. These were selected to represent areas subject to various types and degrees of inadvertent weather modification, plus a no-effect (control) area. The purpose was to determine the magnitude and relative intensity of urban and topographic effects on rain enhancement. Results indicated the urban enhancement was greater than that associated with hills and river bluffs in the experimental region. The urban enhancement maximized northeast of the St. Louis urban-industrial complex where it was computed to be approximately 30–35%. The bluffs effect was calculated to be approximately 14%, and the hill effect was 9% for all rainstorms combined during the five summers. The urban and topographic enhancements were most pronounced in heavy storms, defined as those producing gage amounts of 25 mm or more. The enhancement maximized in June in the region of maximum urban effect, but oc... Abstract Analyses were made of the summer rainfall distribution (June-August) in 17 areas within the METROMEX network in St. Louis region. These were selected to represent areas subject to various types and degrees of inadvertent weather modification, plus a no-effect (control) area. The purpose was to determine the magnitude and relative intensity of urban and topographic effects on rain enhancement. Results indicated the urban enhancement was greater than that associated with hills and river bluffs in the experimental region. The urban enhancement maximized northeast of the St. Louis urban-industrial complex where it was computed to be approximately 30–35%. The bluffs effect was calculated to be approximately 14%, and the hill effect was 9% for all rainstorms combined during the five summers. The urban and topographic enhancements were most pronounced in heavy storms, defined as those producing gage amounts of 25 mm or more. The enhancement maximized in June in the region of maximum urban effect, but oc...Keywords
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