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<br />; <br /> <br />FLOJD:I'.W yODEL (HEC- 2) COCiCEPTS <br /> <br />_ \.. is :-:e:eSS2.1-Y that the bc.sis and li-r.itations of the mathei-:12tic JT,odel <br />,'~-:=C- ='. ,,- '~::-.~:2Y;::;~OOC:' ::'. C'~-C2T to correc:'ly apply the flooGhay conceDt. <br /> <br />...:Y':- _ ::::. . :.~..:c -, <br /> <br />,;- _..~,- ~~.: <br /> <br />.. ~ ~ ',' <br />..,,~ "'c_ ~-~. -,--~~',-L: <br /> <br />C:I1C cC:~~~3tions are graduall)' varisd <br /> <br />ste~::c:.>' ~l:',.:. <br /> <br />c ;:1c.': 13 CDe di-::er.,Si':Jr,21 <br />o Pressure is hydrostatic <br />G Channel slope' is minor (less than 10 percent) <br />o O1"-,,,l'l ~oW1dar;, is rigid (e.g., no enlargl'ment fro:;] sedinent <br />tra:1sportation) <br /> <br />..,_ ~C-2 ?,o;r::L-;j \,,'as designed to detemine flood profiles for natural <br />channels ',,:i th \'<irying horizontal roughness and velocity. This model <br />.,-e.,-:'eCO:,,5 ,",e ~e5t ?....ai~a'::cle, l-:ork3.~le mathematical model for detennining <br />1':2:er S1..:rr2:e profiles. <br /> <br />During the cO:TIputation of water surface profi les and floodl,ay widths, many <br />co~ditions arise Ivhich require judgement. Among these are: <br /> <br />o Ccr.di t iO:1s h'r.ere the basic asswnptions don't hold <br />r U~-~rt"in-\' o~ o'o-a <br />_ ..Lt... c.... .1-. .L uL <br />o In2dequ2te data <br /> <br />The cO:lputatio:1S and data should be reviewed continually during the floodl.;ay <br />determination process. Thence, make adjustments by: <br /> <br />o .~,pplying SOUJld judgements <br />o Using HEC-2 cO:TIputations as a guide <br /> <br />" <br />