Determination of Channel-Morphology Characteristics, Bankfull Discharge, And Various Design-Peak Discharges in Western Montana 2004
Determination of Channel-Morphology Characteristics, Bankfull Discharge, And Various Design-Peak Discharges in Western Montana 2004
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Channel-morphology data together with vari- ous design-peak discharge data (Parrett and Johnson, 2004) for each site are shown in table 1 ; selected basin and climatic vari- ables for each site are shown in table 2 (at back of report).
Additional data were collected during the site visit. Dis- charge was either determined from the most recent stage-dis- charge relation or measured with a current meter. Current- meter measurements were made in accordance with methods described by Rantz and other...s (1982).
Determination of Bankfull Discharge at Gaged Sites Bankfull discharge and its associated recurrence interval were determined at each of the 41 gaged sites. For each study reach, the bankfull-stage, water-surface, and thalweg eleva- tions, along with associated channel-distance data, were used to construct longitudinal profiles. Under the hydraulic condition of gradually varied flow, which is the most common hydraulic condition in natural streams (Jobson and Froehlich, 1988), bankfull-stage, water-surface, and thalweg profiles tend to be parallel.
What to read after Determination of Channel-Morphology Characteristics, Bankfull Discharge, And Various Design-Peak Discharges in Western Montana 2004?
You can find similar books in the "Read Also" column, or choose other free books by Montana.Dept. of Transportation to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Channel-morphology data together with vari- ous design-peak discharge data (Parrett and Johnson, 2004) for each site are shown in table 1 ; selected basin and climatic vari- ables for each site are shown in table 2 (at back of report).
Additional data were collected during the site visit. Dis- charge was either determined from the most recent stage-dis- charge relation or measured with a current meter. Current- meter measurements were made in accordance with methods described by Rantz and other...s (1982).
Determination of Bankfull Discharge at Gaged Sites Bankfull discharge and its associated recurrence interval were determined at each of the 41 gaged sites. For each study reach, the bankfull-stage, water-surface, and thalweg eleva- tions, along with associated channel-distance data, were used to construct longitudinal profiles. Under the hydraulic condition of gradually varied flow, which is the most common hydraulic condition in natural streams (Jobson and Froehlich, 1988), bankfull-stage, water-surface, and thalweg profiles tend to be parallel.
What to read after Determination of Channel-Morphology Characteristics, Bankfull Discharge, And Various Design-Peak Discharges in Western Montana 2004?
You can find similar books in the "Read Also" column, or choose other free books by Montana.Dept. of Transportation to read onlineMoreLess
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