On geomorphological dispersion in natural catchments and the geomorphological unit hydrograph

1994 ◽  
Vol 30 (7) ◽  
pp. 2311-2323 ◽  
Author(s):  
John D. Snell ◽  
Murugesu Sivapalan
1998 ◽  
Vol 2 (1) ◽  
pp. 1-8 ◽  
Author(s):  
A. Y. Shamseldin ◽  
J. E. Nash

Abstract. The theory of the geomorphological unit hydrograph (GUH) is examined critically and it is shown that the inherent assumption that the operation of the drainage network may be modelled by a corresponding network of linear reservoirs so restricts the instantaneous unit hydrograph (IUH) shape that the effects of further restrictions, reflecting the constraints imposed by the geomorphological laws of the channel network, cannot easily be identified. Without such identification, the geomorphological unit hydrograph theory is untestable and must remain only a plausible hypothesis providing an indication of a two-parameter IUH whose shape and scale factors must still be related empirically to appropriate catchment characteristics.


2015 ◽  
Vol 41 (1) ◽  
pp. 27-37 ◽  
Author(s):  
Riccardo Rigon ◽  
Marialaura Bancheri ◽  
Giuseppe Formetta ◽  
Alban de Lavenne

2015 ◽  
Vol 48 (2) ◽  
pp. 91-103
Author(s):  
Joo-Cheol Kim ◽  
◽  
Kwansue Jung ◽  
Dong Kug Jeong

1985 ◽  
Vol 16 (1) ◽  
pp. 1-10 ◽  
Author(s):  
V. P. Singh ◽  
C. Corradini ◽  
F. Melone

The geomorphological instantaneous unit hydrograph (IUH) proposed by Gupta et al. (1980) was compared with the IUH derived by commonly used time-area and Nash methods. This comparison was performed by analyzing the effective rainfall-direct runoff relationship for four large basins in Central Italy ranging in area from 934 to 4,147 km2. The Nash method was found to be the most accurate of the three methods. The geomorphological method, with only one parameter estimated in advance from the observed data, was found to be little less accurate than the Nash method which has two parameters determined from observations. Furthermore, if the geomorphological and Nash methods employed the same information represented by basin lag, then they produced similar accuracy provided the other Nash parameter, expressed by the product of peak flow and time to peak, was empirically assessed within a wide range of values. It was concluded that it was more appropriate to use the geomorphological method for ungaged basins and the Nash method for gaged basins.


1997 ◽  
Vol 194 (1-4) ◽  
pp. 366-384 ◽  
Author(s):  
Bing Zhao ◽  
Yeou-Koung Tung ◽  
Keh-Chia Yeh ◽  
Jinn-Chuan Yang

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