Laserfiche WebLink
<br />e <br /> <br />. <br /> <br />.. <br /> <br />e <br /> <br />. <br /> <br />e <br /> <br />MANUALS-CORPS OF ENGINEERS <br />U. S. ARMY <br /> <br />EM 1110--2--1406 <br />31 Aug 59 <br /> <br />ENGINEERING AND DESIGN <br />FLOOD-HYDROGRAPH ANALYSES AND COMPUTATIONS <br />INTRODUCTION <br /> <br />1. PURPOSE AND SCOPE. This manual describes and illustrates certain methods of deriving <br />fundamental hydrologic factors by analyzing observed hydrographs of stream flow and related meteoro- <br />logical events and suggests methods of utilizing these deduced factors in computing hypothetical hydro- <br />graphs of runoff for conditions differing, in specified respects, from those prevailing during the observed <br />floods. This manual is also issued for guidance in hydrologic studies for Corps of Engineers water <br />resource development projects. <br /> <br />2. REFERENCES. a. Reference is made in the text to EM 111O-2~1408, Routing of Floods Through <br />River Channels, This manual was last published under a now superseded numbering system as Part <br />CXIV, Chapter 8, dated September 1953. <br />b. Appendix II consists of a selected bibliography. References in the text to items in the bibliog, <br />raphy are indicated by numbers in an exponrntial position. Other references are also given in the text. <br /> <br />3. RESCISSION. a, Engineering Manual for Civil Works Construction, Part CXIV, Chapter 5, <br />March 1948; Hydrologic and Hydraulic Analyses, Flood,Hydrograph Analy,es and Computations (EM <br />1110--2-; 1405). <br />b. Civil Works Engineer Bulletin No. 49-22, Unit Hydrograph Compilations, 7 December 1949. <br /> <br />4. TYPES OF ANALYSES COVERED. a. Analysis of a flood hydrograph as discussed herein includes- <br />(I) Estimates of the intensity, depth and areal distribution of precipitation causing the runoff <br />(and rate of snowmelt, where this is significant); <br />(2) Computation of difference between precipitation and direct runoff, expressed herein as <br />initial loss and infiltration index; <br />(3) Determination of the combined effect of drainage area and channel characteristics on the <br />regimen of runoff, expressed herein in terms of "unit hydrographs." <br />b. The computation of hypothetical hydrographs, based on data derived from natural hydrograph <br />analyses and supplementary studies, includes: <br />(I) Determination of desigp,storm rainfall values, the areal distribution and sequence of occur- <br />rence of unit increments that would produce critical rates of runoff, or rates corresponding to specified <br />lesser magnitudes aceording to the purpose of the estimate. In certain cases, rainfall values correspond- <br />ing to certain average frequencies of occurrence may be adopted as design storms in order to serve as a <br />basis for estimating economic benefits; <br />(2) Selection of infiltration indices and initial loss values to correspond with the given drainage <br />area and assumptions regarding season of the year, antecedent rainfall and other considerations affecting <br />volume of runoff; <br />(3) Selection of unit hydrographs to represent the probable order of runoff from adopted <br />design storm rainfall-excess; <br />(4) Computation of hypothetical hydrographs by combining factors referred to above. <br />c. The previous issue of this manual (Part CXIV, Chapter 5) contained a section entitled "Flood <br />Flow Contributions from Melting Snow." This material has been eliminated from this manual and the <br />subject will be treated in an expanded manual entitled "Runoff from Snowmelt" (EM 1110--2-1406). <br /> <br />5. BASIC CONSIDERATIONS. a. The characteristics of natural drainage basins and meteorological <br />influenees affecting runoff are too complex and variable to be evaluated accurately by mechanical com- <br /> <br />1 <br />