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- W139347020 abstract "Scale problems result in uncertainty in hydrological modelling and is far from being solved. A distributed hydrological model BTOPMC (Block- wise use of TOPMODEL with Muskingum-Cunge method) analyses the effects of sub-basin scale on runoff in the Fuji-kawa and the Nakagawa basins in Japan. Study basins were subdivided into natural sub-basins using the Pfafstetter method. Results indicate that smaller average sub-basin size produces higher peak discharge, larger baseflow and total runoff for floods, while similar effects on annual runoff do not show any determined tendency and are not obvious. This shows the effect of averaging scale of the topographic index. Furthermore, threshold values of average sub-basin areas were found for study basins, around which simulation results seem stabilized, indicating that there may exist a proper sub-basin scale for BTOPMC, at which uncertainty due to subdivision level can be reduced to quite a low level." @default.
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- W139347020 date "2003-01-01" @default.
- W139347020 modified "2023-09-22" @default.
- W139347020 title "Effects of sub-basin scale on runoff simulation in distributed hydrological model: BTOPMC" @default.
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