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Estimation of peak streamflows for unregulated rural streams in Kansas
Peak streamflows were estimated at selected recurrence intervals (frequencies) ranging from 2 to 200 years using log-Pearson Type III distributions for 253 streamflow-gaging stations in Kansas. The annual peak-streamflow data, through the 1997 water year, were from streamflow-gaging stations with unregulated flow in mostly rural basins. A weighted least-squares regression model was used to generalize the coefficients of station skewness. The resulting generalized skewness equation provides more reliable estimates than the previously developed equation for Kansas. A generalized least-squares regression model then was used to develop equations for estimating peak streamflows for sites without stream gages for selected frequencies from selected physical and climatic basin characteristics for sites without stream gages. The equations can be used to estimate peak streamflows for selected frequencies using contributing-drainage area, mean annual precipitation, soil permeability, and slope of the main channel for ungaged sites in Kansas with a contributing-drainage area greater than 0.17 and less than 9,100 square miles. The errors of prediction for the generalized least-squares-generated equations range from 31 to 62 percent.
Suggested Citation
Rasmussen, P.P., Perry, C.A., 2000, Estimation of peak streamflows for unregulated rural streams in Kansas: U.S. Geological Survey Water-Resources Investigations Report 2000-4079, iv, 33 p., (2 folded) :ill., col. maps ;28 cm., https://doi.org/10.3133/wri004079.
Publication type
Report
Publication Subtype
USGS Numbered Series
Title
Estimation of peak streamflows for unregulated rural streams in Kansas
Series title
Water-Resources Investigations Report
Series number
2000-4079
DOI
10.3133/wri004079
Year Published
2000
Language
ENGLISH
Publisher
U.S. Department of the Interior, U.S. Geological Survey ;
Information Services [distributor],