Articles | Volume 20, issue 12
Hydrol. Earth Syst. Sci., 20, 5063–5071, 2016
https://doi.org/10.5194/hess-20-5063-2016

Special issue: Modeling hydrological processes and changes

Hydrol. Earth Syst. Sci., 20, 5063–5071, 2016
https://doi.org/10.5194/hess-20-5063-2016

Research article 21 Dec 2016

Research article | 21 Dec 2016

Effects and consideration of storm movement in rainfall–runoff modelling at the basin scale

Shahram Khalighi Sigaroodi and Qiuwen Chen

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Cited articles

Choi, J., Socolofsky, S. A., and Olivera, F.: Hourly disaggregation of daily rainfall in Texas using measured hourly precipitation at other locations, J. Hydrol. Eng., 13, 476–487, 2008.
Costabile, P., Costanzo, C., and Macchione, F.: A storm event watershed model for surface runoff based on 2D fully dynamic wave equations, Hydrol. Process., 27, 554–569, 2012.
de Lima, J. L. M. P. and Singh, V. P.: The influence of the pattern of moving rainstorms on overland flow, Adv. Water Resour., 25, 817–828, 2002.
de Lima, J. L. M. P., Singh, V. P., and de Lima, M. I. P.: The influence of storm movement on water erosion: storm direction and velocity effects, Catena, 52, 39–56, 2003.
Gyasi-Agyei, Y.: Stochastic disaggregation of daily rainfall into one-hour time scale, J. Hydrol., 309, 178–190, 2005.
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Short summary
The paper presents original research about storm movement effects on runoff modelling at the basin scale instead of the conventional laboratory scale. It is essential to find that neglecting storm movement may bring artifacts to parameters when calibrating hydrological models; slow movement of storm has a more significant effect on hydrograph; storm movement on hydrograph modelling becomes visible only when the study area is divided into sub-basins.