Laserfiche WebLink
<br />O~1238 <br /> <br />THEORY AND EXPERIMENTS IN THE PREDICTION OF <br />SMALL WATERSHED RESPONSE <br /> <br />The more complex modern society is becoming more involved with <br /> <br />problems associated with floods from small watersheds. The problem of <br /> <br />estimating flood peaks from small watersheds is an important element in <br /> <br />the design of storm sewers, highway drainage, diversion works, flood <br />retarding structures, bridges and culverts. The majority of such <br />hydraulic structures are constructed on small watersheds. Since small <br /> <br />streams have not been gaged as extensively in the past as have large <br /> <br />streams, more of the designs have to be prepared without the benefit of <br />stream flow records. There is a great need to develop more satisfactory <br />methods for obtaining design floods for these watersheds under the varied <br /> <br />changes taking place in the modern day life. <br /> <br />INTRODUCTION <br /> <br />In a small watershed the predominant storage element is the surface <br />detention storage. It is the storage element in the watershed which <br /> <br />produces the difference between the input - rainfall excess - and the <br /> <br /> <br />output - surface runoff. As the watershed increases in size, the <br /> <br />predominant storage element in the watershed becomes the channel storage. <br />The small watershed with its relatively important relationship to <br />the surface detention is therefore more sensitive to man made changes in <br /> <br />those things which influence the transit time of the overland flow. <br /> <br />Changes such as increasing or decreasing the surface roughness, the <br /> <br />length of overland flow, the overland flow slope are all changes which <br /> <br /> <br />should have a large effect on the flood response of the watershed to <br /> <br />storm rainfall. <br />