Laserfiche WebLink
<br />GLOSSMY OF Tm~S <br /> <br />Flood Profile <br />A graph showing The relationship of water surface elevation <br />to location, the I~tter gonarally expressed as d i stence above mouth <br />for a stream of water f lowing in ~n open channel. It is general I y <br />drawn to sho" ~",rfacc elevation for the crest of ,1 spa<:: if Ie 11000, <br />but ~ay be prepared lor conditions at a given tiMe or s~age. <br /> <br />Backwater <br /> <br />The resulting high ,~"ter sur-face in a gi~f.m stre<wn due to <br />J downstre~ ob5truction or high sta~s in an lntersect1ng stream. <br /> <br />Flood <br /> <br />An overflow of lands not normally covered ~y water and that <br />are used or usable ~y man. Floods haV9 t"o essenTI~1 characferistics: <br />the 1m ndation of I and i5 tanporary; and the land is adjacent to ~nd <br />inundated ~y overf low from a river, stream, ocean, lake, or other <br />~ody of standing water. <br />Nonnal iy II "flood" is considered as any tW1pOrary rise in <br />5tre~mf low or stage, but not the pond ing of surface water, that rcsu Its <br />in signlficent adverse effects in the vicinity. Adverse effects ~y <br />Include damage~ from overflow of land areas, temporary backwater <br />eff0Cts in se"ers and local drainage channels, creation of unsanitary <br />conditions or other unf~vorable situations by deposition of materials <br />in stream chanr'lels dYri n9 f lood rece~sions, ri 5" of grwnJ water <br />coincident with increased stre~m flow, and other problems. <br /> <br />FloodSlago <br />The stage or ellwation at whiCh oyerflo" of the natural <br />banks of a streilmor body of "ater begIns in the reoch or area In <br />Which the elevation is measured. <br /> <br />HydrClqraph <br />A graph ~howing flow values agaillst time at a gIven point, <br />usuallymM5ured in cUbic feet per 5BCOnd. Tho area under the curve <br />indicatos total volume of flow. <br /> <br />Flood Crest <br />The maxirr.."" stage of eleviltlon nmchoo by tho w"ter~ of il <br />flood ~t a gIven locet1on. <br /> <br />IntermL~i~te Rogion~1 Flood <br />A flood h~vin9 an avera~e frc~c"cy af occurrenCe In the <br />order 0/ once io 100 ye~rs althcuyh the flood may occur in "'y ye~r. <br />It Is based on sta~lstical analyses of streamflow rer-ords avallahle <br />for the watershed and analyses 01 rainfall anj r1JM,f/ "hM'aat"rlstiCs <br />i" Lou ~'ln..rdi ,....'<] ion 0; fhe "dters",,,J. <br /> <br />Left""nk <br /> <br />The dre~s adjoining a river, stream, waterCC'-Jrso, oc<)~n, <br />lako, or other body of stallding w~ter th<lt hdve be"n or ""'y be cov"re<:l <br />by f lO<':Jw~t..r. <br /> <br />ihe b~nk on the left side of a river. stroam, or w"tercO;Jrsc, <br />lookln] downstream. <br /> <br />floodPlain <br /> <br />RlqhtBank <br />The b<lnkon the right side of a river, <br />lookIng dDwnstream. <br /> <br />strCdm.orwaterCClJrso <br />, <br /> <br />" <br /> <br />" <br />