Preprints
https://doi.org/10.5194/hess-2021-470
https://doi.org/10.5194/hess-2021-470
 
29 Sep 2021
29 Sep 2021
Status: this discussion paper is a preprint. It has been under review for the journal Hydrology and Earth System Sciences (HESS). The manuscript was not accepted for further review after discussion.

A Time-Varying Distributed Unit Hydrograph considering soil moisture content

Bin Yi1,2, Lu Chen1,2, Hansong Zhang3, Ping Jiang4, Yizhuo Liu1,2, and Hongya Qiu1,2 Bin Yi et al.
  • 1School of Civil and Hydraulic Engineering, Huazhong University of Science and Technology, Wuhan, 430074, China
  • 2Hubei Key Laboratory of Digital Valley Science and Technology, Wuhan 430074, China
  • 3PowerChina Huadong Engineering Corporation Limited, Hangzhou 310014, China
  • 4Meizhou Hydrological Bureau, Guangdong Province, Meizhou 514000, China

Abstract. The distributed unit hydrograph (DUH) method has been widely used for flood routing simulation, because it can well characterize the underlying surface characteristics and various rainfall intensities. The core of the DUH is the calculation of flow velocity. However, the current velocity formula assumed a global equilibrium of the watershed and ignored the impact of time-varying soil moisture content on flow velocity, which leads to a larger flow velocity value. The goal of this study is to identify a soil moisture content factor, which was derived based on the water storage capacity curve, to explore the responses of DUH to soil moisture content in unsaturated areas. Thus, an improved distributed unit hydrograph based on time-varying soil moisture content was proposed in this paper. The proposed method considered the impact of both the time-varying rainfall intensity and soil moisture content on the flow velocity, and the watershed is assumed not to be equilibrium but vary with the soil moisture. The Qin River Basin was selected as a case study, and results of the time-varying distributed unit hydrograph (TDUH) and current DUH methods were used as comparisons with that of proposed method. Influence mechanism of time-varying soil moisture content on the flow velocity and flood forecasts were explored. Results show that the proposed method performs the best among the three methods. The shape and duration of the unit hydrograph can be mainly related to the soil moisture content at initial stage of a storm. When the watershed is approximately saturated, the grid flow velocity is majorly dominated by the excess rainfall.

Bin Yi et al.

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on hess-2021-470', Anonymous Referee #1, 21 Oct 2021
    • AC1: 'Reply on RC1', Bin Yi, 10 Nov 2021
  • RC2: 'Comment on hess-2021-470', Jasper Vrugt, 26 Oct 2021
    • AC2: 'Reply on RC2', Bin Yi, 03 Dec 2021

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on hess-2021-470', Anonymous Referee #1, 21 Oct 2021
    • AC1: 'Reply on RC1', Bin Yi, 10 Nov 2021
  • RC2: 'Comment on hess-2021-470', Jasper Vrugt, 26 Oct 2021
    • AC2: 'Reply on RC2', Bin Yi, 03 Dec 2021

Bin Yi et al.

Bin Yi et al.

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Short summary
An improved Gis-derived distributed unit hydrograph routing method considering time-varying soil moisture content was proposed for flood routing. The proposed method considered the changes of time-varying soil moisture content and rainfall intensity. The response of underlying surface to the soil moisture content was considered as an important factor in this study. The DUH, TDUH and proposed routing methods were used for flood forecasts, and the simulated results were compared and discussed.