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<br /> "T1 <br /> -. <br /> co t <br /> c <br /> ca :;; <br /> ~ 0 <br /> . LL <br /> ---4 .... <br /> 0 <br /> '< Q) <br /> "C Ol <br /> -. <1l <br /> n - <br />I\) S>> CJ) <br /> - Ol <br /> ::I: c <br /> '< l/) <br /> 0- <1l <br /> ~ <br /> a u <br /> co c <br /> ;1 t <br /> "C <br /> ::r <br /> <br /> <br /> <br />- <br />C <br />:::J <br />o <br />E <br /><! <br />Cll <br />- <br />c <br />Cll <br />a: <br /> <br />Rainfall <br /> <br /> <br /> <br />. Tr . <br />__Tw-e <br />. T wp . <br /> <br />/-Falling <br />j( Limb <br /> <br />Flood Stage---u----nu-n- <br />Bankfull Stage ____________n__ <br /> <br />Low <br />- Stage <br /> <br />Hydrograph <br /> <br /> <br />- Passing of Time _ <br /> <br />The relation between a flood hydrograph and land development along a stream is shown, The hydrograph with <br />rainfall amounts is shown in the darker tones with adjacent scales, A distorted cross section of land development <br />is in lighter tones, The vertical scale is the same as the stage for the hydrograph, No horizontal scale is proved <br />for cross section, <br /> <br />, <br /> <br />. <br />