Climatological Assessment of Urban Effects on Precipitation at St. Louis
- 1 August 1972
- journal article
- Published by American Meteorological Society in Journal of Applied Meteorology
- Vol. 11 (5) , 823-842
- https://doi.org/10.1175/1520-0450(1972)011<0823:caoueo>2.0.co;2
Abstract
An investigation was made of urban effects on precipitation in and downwind of St. Louis through use of long-term climatic records within a radius of 50–75 mi of the city. Based upon radar climatological studies, two potential urban effect areas and two no-effect (control) areas were designated. Analyses were then performed to assess the urban effect on 1) total monthly and seasonal precipitation; 2) the frequency and intensity of daily precipitation; 3) the frequency of thunderstorms, hailstorms, and severe rainstorms; 4) wet-dry period rainfall; and 5) weekday-weekend precipitation (indicator of industrial-induced effect). Evidence of urban effects was found in all seasons, but appear to he strongest in late spring and summer. Results indicated an urban-induced increase in average summer rainfall ranging from 6 to 15% for distances up to 25 mi downwind of the city. The urban-increase mechanism apparently is most active on days of moderate to heavy intensifies in the natural rainfall. The urban ... Abstract An investigation was made of urban effects on precipitation in and downwind of St. Louis through use of long-term climatic records within a radius of 50–75 mi of the city. Based upon radar climatological studies, two potential urban effect areas and two no-effect (control) areas were designated. Analyses were then performed to assess the urban effect on 1) total monthly and seasonal precipitation; 2) the frequency and intensity of daily precipitation; 3) the frequency of thunderstorms, hailstorms, and severe rainstorms; 4) wet-dry period rainfall; and 5) weekday-weekend precipitation (indicator of industrial-induced effect). Evidence of urban effects was found in all seasons, but appear to he strongest in late spring and summer. Results indicated an urban-induced increase in average summer rainfall ranging from 6 to 15% for distances up to 25 mi downwind of the city. The urban-increase mechanism apparently is most active on days of moderate to heavy intensifies in the natural rainfall. The urban ...Keywords
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