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<br />-. <br /> <br />"' <br /> <br />f) <br /> <br />, <br />\ <br /> <br />l'lENERAL MOllELING CONSIDERATIONS <br /> <br />The soli t flow option requires that the cross section numhers (Xl card) <br /> <br />comtinually inerea~e in yalue from ~strpam to uDStream. It is rPCCm\ll~nde~ <br /> <br />that statil'lft values in f~et or miles ....asu~ed along th~ main channel he us..n for <br /> <br />crosR section nu~rs. This is imoortant ~ause the REC-2 program uses the <br /> <br />cross section numbers sPecified on the split flow rpaehes to ~termine what <br /> <br />water surface or energy qrade line elevations to use in ~ptp.nftininq the amount <br /> <br />of flow 10At. Ear:h splil: flow reach is located based on cross section n'Jlllhers <br /> <br />at thl!! downstream and upstream ends of thl!! ~each. <br /> <br />If the downstream and <br /> <br />~stream split flow locations do not match a cross section number, the program <br /> <br />will linearly interpolate between cross s-.ction numbers to ~termine the water <br /> <br />surfaces or energy qrade tine eleyations. A wise practice would be to start and <br /> <br />end t~ split flow ~eaclles at cross section numbers that appear in the HBC-2 <br /> <br />hydraulie model. <br /> <br />Split Flow Reaeh L.-nqth Consideration. <br /> <br />The overflow reaches should be kept as sbort as possible. TIle lon<ler th" <br /> <br />split flow reaehes, the less accurate will he tile split flows and bac~water <br /> <br />answers. The split flow problem can be compar..n to the integration of a curYe <br /> <br />by the Trapezoidal Rule, which is an approximate methoil of slJMiyiding the curyp <br /> <br />into a number of straioht line s~nts and ealculatinq the areall under eaeh <br /> <br />straiqht line seqm~nt and then addino up t~ subareas to calculate the total <br /> <br />area under the curve. The smaller th~ straiqht line segments an~ the larqer the <br /> <br />nllmber of s~ts, the II\Ore accurate will be the ealculateCl area. The same <br /> <br />11 <br />