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<br />I <br />I <br /> <br />. <br />, <br />, <br />" <br />I <br />I <br />I <br />I <br />I <br /> <br />Head Lose. The effect of obstruction~, such ~g narro~ bripge <br />openings or buildings that limit the area through which water <br />~uot flow, r~ising ths surf~ee of the water wp~tr8~rn from the <br />~bstruction. <br />!ntcrm~diate Recional flood. ~ flood having an average frequency <br />of occurrence in ths order of once in 100 years although the flood <br />~ay occur in any year. It is based on statistical analyaes of <br />stree~flow :ecords available for the watarahod and analyse" of <br />rainfall and r~n"ff characteristics in the "general region of the <br />watsI:shed." <br /> <br />CLOSSARYOf TERM5 <br /> <br />flood. An overflow of laoda, not normally covered ty w~ter, tMat <br />e~e used Or w5able by man, Floods h~ve tWQ ecsential character- <br />istics: the inundation of land is te~po~ary; and the land is <br />~dja~ent to and inundated by overflo~ from a river or strea~, or <br />an o~ean, lake, or other body of standing ~ater. <br />Normally, a ~flood" is ~onsidered es any te'nporery <br />rise in streamflo~ or stage, bwt not the ponding of surf~C6 <br />water, that results in sigoificant adverse effects in tha vicinity. <br />Adverso effects may inolude d~ages from overflow of lend area~, <br />temporary backwater effacts in sewers and local drainage channels, <br />croatian of unsanit~ry condition~ or other unfavor~bl~ situations <br />by deposition of materials in etre~ channels d~ring flood reces- <br />sions, rise of gro~nd watet coincident with increased "treamflo~, <br />and other problems. <br />Flood Cra~t. The wa~imum stage or elevation reached by tha woters <br />of a flood at a given location. <br />flood Plain. The relatively flat are~ or lo~ land5 adjoining <br />the channel of a river, stream or watercourse. or ocean, lake, <br />or other body of ~tanding water. ~hich hoo be~n or may b~ covered <br />by fl<lod~.ater. <br />Flood Profile. A graph showing the relationShip of water ourface <br />elevation to location, the l~tter generally expressed a~ di~tance <br />~bove mouth far a etraa~ of watar flowing in ~n open cMann~l. <br />!t is generally drawn to show eurfaco clavation for tho cr~rrt of <br />a specific flood, but may bsprepe.red for conditions et a given <br />time or staga. <br />flood 5to~~. T~~ st~gn or elnvation et ahich ovo~flo~ of the <br />n8tLIral banks of a strea'" or body of water begins in th~ rea~h <br />or erS8 in which the slev~tion is ~e3surad. <br /> <br />I <br />I <br />( <br /> <br />L9ft or Rioht Bank, TMe bank On the left or right side of a river, <br />strea~, or watercourse, looking downstroom. <br />Standard Proiect flood. The fl<lod that may be expected from the <br />most severe combination of meteorological and hydrologioal con_ <br />ditions that is considered reasonably charactoristic of the geo_ <br />graphical area in whi~h the drainage basin is loosted. exclLIding <br />extremely rore co~bination". Peak discMarges for thsse floods ore <br />generally abo~t 4:% to 50% of the probabl~ ~oximurn floods for the <br />se~e basing. Such floods, as used by the Corps of [nginBers, orG <br />intended as practicsble expressions of the degree of protection <br />that ohould te sought in the design of flood control works, the <br />failure of which might ba disestrous. <br />Under clearance. The lo~e6t point of s bridge or other str~cture <br />over or scross s river, stream, or ~atercourse that limits the <br />opening through which ..at~r flows. This is referred to "s "lo~ <br />steel" in some r~gions. <br /> <br />;0 <br /> <br />~1 <br /> <br />, <br />