Abstract

Abstract. Sediment and runoff changes of seven hydrological stations along the Lower Yellow River (LYR) (Huayuankou Station, Jiahetan Station, Gaocun Station, Sunkou Station, Ai Shan Station, Qikou Station and Lijin Station) from 1980 to 2003 were alanyzed at multiple time scale. The maximum value of monthly, daily and hourly sediment load and runoff conservations were also analyzed with the annually mean value. Mann–Kendall non-parametric mathematics correlation test and Hurst coefficient method were adopted in the study. Research results indicate that (1) the runoff of seven hydrological stations was significantly reduced in the study period at different time scales. However, the trends of sediment load in these stations were not obvious. The sediment load of Huayuankou, Jiahetan and Aishan stations even slightly increased with the runoff decrease. (2) The trends of the sediment load with different time scale showed differences at Luokou and Lijin stations. Although the annually and monthly sediment load were broadly flat, the maximum hourly sediment load showed decrease trend. (3) According to the Hurst coefficients, the trend of sediment and runoff will be continue without taking measures, which proved the necessary of runoff-sediment regulation scheme.

Highlights

  • Climate changes and human activities have great influence on fluvial geomorphology (Zhang et al, 2006)

  • We can conclude that the runoff of the seven hydrological stations are shown obviously downward trend at different time scale

  • It can be observed that the trend of the runoff changes at seven stations in the Lower Yellow River (LYR) are relatively consistent

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Summary

Introduction

Climate changes and human activities have great influence on fluvial geomorphology (Zhang et al, 2006). It is of great importance to understand the sediment and runoff changes for reservoir operation, flood mitigation and fluvial management. Sedimentation resulted in that the river bed of lower yellow river (LYR) is higher than the surrounding lands, which posed a huge flood risk of the residents. Since 2002, a Runoff-Sediment Regulation Scheme (WSRS) has been implemented by the Yellow River Conservancy Commission (YRCC) to reduce the siltation in LYR and transport sediment to sea (Xia et al, 2016). Many researchers tried to analyse the influence of the WSRS. Analysis of the sediment and runoff changes of LYR before WSRS is a critical step for these researches

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