2011
DOI: 10.2208/jscejhe.67.155
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Application of a Quasi-3d Numerical Model to a Flood Flow Observed in the Lower Tone River in September, 1998

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“…On the other hand, the channel bed elevation of Hyakken-gawa was considered to be almost the same as that of the present high water channel, and the channel cross sections were obtained by removing the data for the low water channel from the recent surveying data. Manning's roughness was assumed to be 0.28 and 0.35 for the Asahi River and Hyakken-gawa Floodway, respectively, based on existing studies [8,9].…”
Section: Calculation Condition 41 Topographymentioning
confidence: 99%
“…On the other hand, the channel bed elevation of Hyakken-gawa was considered to be almost the same as that of the present high water channel, and the channel cross sections were obtained by removing the data for the low water channel from the recent surveying data. Manning's roughness was assumed to be 0.28 and 0.35 for the Asahi River and Hyakken-gawa Floodway, respectively, based on existing studies [8,9].…”
Section: Calculation Condition 41 Topographymentioning
confidence: 99%