Predicting the Runoff from Storm Rainfall, Volume 30U.S. Department of Commerce, Weather Bureau, 1951 - 10 pagina's The estimation of the volume of runoff to be expected from a given volume of rainfall is a fundamental problem in flood forecasting. Such estimates are necessary before the unit hydrograph or other techniques can be used to predict the streamflow hydrograph. The authors describe the technique now used at the River Forecast Centers of the U.S. Weather Bureau for evaluating the effect of season, antecedent conditions, duration of rainfall and rainfall amount in determining the portion of the rainfall contributing to storm runoff. Special problems encountered in flood forecasting are emphasized. The technique, developed and tested over several years, yields a high degree of accuracy in estimated runoff. Although prepared by empirical procedures, the close agreement between relations for basins of similar hydrologic characteristics suggests that rational parameter have been adopted. The similarity between relations also simplifies the work required for their preparation. |
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Pagina 1
... estimated runoff . Although prepared by empirical procedures , the close agreement between relations for basins of similar hydrologic characteristics suggests that rational parameters have been adopted . The similarity between relations ...
... estimated runoff . Although prepared by empirical procedures , the close agreement between relations for basins of similar hydrologic characteristics suggests that rational parameters have been adopted . The similarity between relations ...
Pagina 6
... estimated for successive time periods throughout an extended storm . This can be accomplished by computing .20 8 59 35 .1.0 18 . ERROR ( Observed minus computed recharge ) O .10 - , 20 7 . Note : To correct positive errors shift week ...
... estimated for successive time periods throughout an extended storm . This can be accomplished by computing .20 8 59 35 .1.0 18 . ERROR ( Observed minus computed recharge ) O .10 - , 20 7 . Note : To correct positive errors shift week ...
Pagina 9
... estimated water equivalent can be sub- tracted from the observed storm precipitation . Snow on the ground at the beginning of the storm should be included in the storm precip- itation ( rather than antecedent precipitation ) if it is ...
... estimated water equivalent can be sub- tracted from the observed storm precipitation . Snow on the ground at the beginning of the storm should be included in the storm precip- itation ( rather than antecedent precipitation ) if it is ...
Veelvoorkomende woorden en zinsdelen
American Geophysical Union amount and duration antecedent index ANTECEDENT PRECIPITATION INDEX application approximations assumed average BASIN RECHARGE Inches cedent precipitation chart sequence coaxial method compute the runoff computed recharge computed value computing runoff considered correlation of runoff curve families curve-families dependent variable DERIVED RELATIONS determined by entering distribution of antecedent duration of rainfall estimated Ezekiel family of curves flood forecasting graphical correlation horizontal scale hydrologic inch per hour index value indicate Infiltration Approach initial index Jug Bridge labeling the points logarithmic recession M. A. KOHLER moisture conditions moisture deficiency Monocacy River OBSERVED BASIN RECHARGE observed recharge period PRECIPITATION INDEX Inches R. K. LINSLEY rain rainfall amount relation for basin relation for Monocacy River at Jug river forecasts runoff depths season or week shown in figure snowfall STORM DURATION Hours STORM PRECIPITATION Inches storm rainfall STORM RUNOFF Inches Streamflow tion U. S. Weather Bureau week curves week number yield