Response of braiding channel morphodynamics to peak discharge changes in the Upper Yellow River | |
Schuurman, Filip1; Ta, Wanquan2; Post, Sander1; Sokolewicz, Marius1; Busnelli, Marcela1; Kleinhans, Maarten3 | |
刊名 | EARTH SURFACE PROCESSES AND LANDFORMS
![]() |
2018-06-30 | |
卷号 | 43期号:8页码:1648-1662 |
关键词 | Yellow River discharge regulation Delft3D braiding floodplain |
ISSN号 | 0197-9337 |
DOI | 10.1002/esp.4344 |
通讯作者 | Schuurman, Filip(filip.schuurman@rhdhv.com) |
英文摘要 | The braiding intensity and dynamics in large braiding rivers are well known to depend on peak discharges, but the response in braiding and channel-floodplain transformations to changes in discharge regime are poorly known. This modelling study addresses the morphodynamic effects of increasing annual peak discharges in braiding rivers. The study site is a braiding reach of the Upper Yellow River. We estimated the effects on the larger-scale channel pattern, and on the smaller-scale bars, channel branches and floodplains. Furthermore, we determined the sensitivity of the channel pattern to model input parameters. The results showed that the dominant effect of a higher peak discharge is the development of chute channels on the floodplains, formed by connecting head-cut channels and avulsive channels. Widening of the main channel by bank erosion was found to be less dominant. In addition, sedimentation on the bars and floodplains increased with increasing peak discharge. The model results also showed that the modelled channel pattern is especially sensitive to parametrization of the bed slope effect, whereas the effect of median grain size was found to be relatively small. Copyright (c) 2018 John Wiley & Sons, Ltd. |
收录类别 | SCI |
WOS关键词 | GRAVEL-BED RIVER ; JAMUNA RIVER ; SAND ; VEGETATION ; EVOLUTION ; DYNAMICS ; PATTERNS ; DESERT ; MODEL ; REACH |
WOS研究方向 | Physical Geography ; Geology |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
语种 | 英语 |
出版者 | WILEY |
WOS记录号 | WOS:000435270900007 |
内容类型 | 期刊论文 |
URI标识 | http://www.corc.org.cn/handle/1471x/2557813 |
专题 | 寒区旱区环境与工程研究所 |
通讯作者 | Schuurman, Filip |
作者单位 | 1.Royal HaskoningDHV, Dept Rivers & Coasts, Amersfoort, Netherlands 2.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Key Lab Desert & Desertificat, Lanzhou, Gansu, Peoples R China 3.Univ Utrecht, Fac Geosci, Dept Phys Geog, Utrecht, Netherlands |
推荐引用方式 GB/T 7714 | Schuurman, Filip,Ta, Wanquan,Post, Sander,et al. Response of braiding channel morphodynamics to peak discharge changes in the Upper Yellow River[J]. EARTH SURFACE PROCESSES AND LANDFORMS,2018,43(8):1648-1662. |
APA | Schuurman, Filip,Ta, Wanquan,Post, Sander,Sokolewicz, Marius,Busnelli, Marcela,&Kleinhans, Maarten.(2018).Response of braiding channel morphodynamics to peak discharge changes in the Upper Yellow River.EARTH SURFACE PROCESSES AND LANDFORMS,43(8),1648-1662. |
MLA | Schuurman, Filip,et al."Response of braiding channel morphodynamics to peak discharge changes in the Upper Yellow River".EARTH SURFACE PROCESSES AND LANDFORMS 43.8(2018):1648-1662. |
个性服务 |
查看访问统计 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。
修改评论