Volume 9 Issue 3
Jul.  2016
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Article Navigation >  Water Science and Engineering  > 2016  >  9(3): 249-255
Sheng-tang Zhang, Yin Liu, Miao-miao Li, Bo Liang. 2016: Distributed hydrological models for addressing effects of spatial variability of roughness on overland flow. Water Science and Engineering, 9(3): 249-255. doi: 10.1016/j.wse.2016.07.001
Citation: Sheng-tang Zhang, Yin Liu, Miao-miao Li, Bo Liang. 2016: Distributed hydrological models for addressing effects of spatial variability of roughness on overland flow. Water Science and Engineering, 9(3): 249-255. doi: 10.1016/j.wse.2016.07.001
shu

Distributed hydrological models for addressing effects of spatial variability of roughness on overland flow

doi: 10.1016/j.wse.2016.07.001

  • aCollege of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, PR China

  • bCollege of Mining and Safety Engineering, Shandong University of Science and Technology, Qingdao 266590, PR China

Funds:  This work was supported by the National Natural Science Foundation of China (Grants No. 41471025 and 40971021) and the Natural Science Foundation of Shandong Province (Grant No. ZR2014DM004).
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  • Corresponding author: Sheng-tang Zhang
  • Received Date: 2015-05-10
  • Rev Recd Date: 2015-12-02
    Abstract
  • In this study, we investigated the origin of the overland flow roughness problem and divided the current overland flow roughness research into three types, as follows: the first type of research takes into account the effects of roughness on the volume and velocity of surface runoff, flood peaks, and the scouring capability of flows, but has not addressed the spatial variability of roughness in detail; the second type of research considers that surface roughness varies spatially with different land usage types, land-cover conditions, and different tillage forms, but lacks a quantitative study of the spatial variability; and the third type of research simply deals with the spatial variability of roughness in each grid cell or land type. We present three shortcomings of the current overland flow roughness research, including (1) the neglect of roughness in distributed hydrological models when simulating the overland flow direction and distribution, (2) the lack of consideration of spatial variability of roughness in hydrological models, and (3) the failure to distinguish the roughness formulas in different overland flow regimes. To solve these problems, distributed hydrological model research should focus on four aspects in regard to overland flow: velocity field observations, flow regime mechanisms, a basic roughness theory, and scale problems.

     

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