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Wet Meadows: Hypotheses 1-8 (2)
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Wet Meadows: Hypotheses 1-8 (2)
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Last modified
1/26/2010 4:37:45 PM
Creation date
6/8/2009 9:52:19 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8461.100
Description
Adaptive Management Workgroup
State
CO
Basin
South Platte
Water Division
1
Date
6/5/2006
Author
PRRIP
Title
Wet Meadow: Hypotheses 1-8
Water Supply Pro - Doc Type
Report/Study
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Detectability/ Time needed for <br />Graph Source of Level of certainty sensitivity measuring a <br />number Description of hypothesis information, if any (feasibility) (feasibility) response <br /> Indlrectly narrowing hydre,oiic curn ;or (preferred width less High because based on empirical <5 years, as luny as <br />Mechanical than 3,000 ft) by consohdaGng channels under proDOSed flow Empincal observations on observations on CenUal Platte Easily detectable, there is at least a flow <br />#1 repime and balancina the sediment budqet will convert the Central Platte River. Feasibiliry: medium, <br />tik <br />lih <br />d t <br />t braiding index easily <br />t gfeater than 05 dunng. <br /> anastomosed reaches of the Platte River between Overton uncer <br />ain <br />e <br />oo <br />o compu <br />ed that period <br /> and Grand Island to a braided channel morphology. <br />successfully constrain flaw. <br /> Reducing the number of channels in a transect to 3 or iess High because based on empirical <5 years, as long as <br />Mechanical under prooosed flow reoime and balanced sediment budQet Empirical obseroations on observations on Central Platte Easily detectable, there is at least a flow <br />#2 will convert anastomosed reaches of the Platte River the Central Platte River. Assumes certain percent braiding index easily greater than 05 during <br /> between Overton and Grand Island to a braided channel distnbution of flow among computed that penod <br /> morphology. channels. <br /> None yet, need to develop <br />Mecharncal Increasing the Braiding Index to greater than 3 in the mam this relationship from Low because there is no basis EasUy detectable with <br /> <br />#3 <br />channel wdl prpmote In the Platte River between Overton and <br />observations on the lower <br />for these numbers yet <br />air photos 5.10 yrs <br /> Grand Island a total main channel wetted width exceedmg Platte River <br /> 500 to 750 ft. <br /> Narrowing the hydrauhc corndor through consolidated flows Easily detectable for <br />Mechanical <br />to three or less channels m a transect, and a balanced <br />None yet Low because there is no basis individual flow by <br />5 10 yrs <br />? sediment budget, will tncrease the area of In-channel bars. for these numbers yet ground survey and aU <br /> photos at index f1ow. <br />Note: #4 is revised version of hypothesis we debated adding on sand bar movement. Changed focus from bar movement to more bars <br />N6on of braidmg index for main channet (as used here) is: Average number of <br />based on limded measurements hom 1998 inha-red air photos.
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