Item talk:Q70460
From geokb
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"name": "Estimating the magnitude of bankfull flows for streams in Idaho",
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"abstract": "Methods for estimating magnitudes of peak\nflows with recurrence intervals of 1.5 and 2.33\nyears were developed for ungaged sites on streams\nthroughout Idaho. These peak flows represent the\nmagnitudes at and near bankfull stage and are\nneeded for quantification of water rights required\nto maintain or restore fish and wildlife habitats and\nriparian vegetation. Data from a previous report\ndetailing methods for estimating magnitudes with\nrecurrence intervals of 2 to 500 years were used in\nthis study.\n\nGeneralized least-squares regression techniques\nwere used to calculate the final coefficients\nand measures of accuracy for the regression equations\nfor each of nine regions. The equations relate\nbasin and climatic characteristics to peak flows\nwith recurrence intervals of 1.5 and 2.33 years. The\nbasin and climatic characteristics used to develop\nthe equations included drainage area, mean basin\nelevation, forested area, mean annual precipitation,\nbasin slope, north-facing slopes greater than 30 percent,\nand slopes greater than 30 percent. Average\nstandard errors of the regression model ranged from\n+150 to -60.1 percent, and average standard errors\nof prediction ranged from +165 to -62.2 percent.\nThe range of prediction errors was narrowest,\n-48.9 to -32.9 percent, for region 5.\nA computer program was developed to automate\nthe calculations required for the regional\nregression calculations. Results from this program\ncomprised calculated peak flows, site-specific standard\nerrors of prediction, and the 90-percent confidence intervals for the estimates.",
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