期刊
RIVER RESEARCH AND APPLICATIONS
卷 27, 期 9, 页码 1159-1167出版社
WILEY
DOI: 10.1002/rra.1479
关键词
river ice; sedimentary link; conceptual model; spatial pattern; gravel-bed river
资金
- NSERC
This paper proposes a conceptual model relating the large-scale distribution of river ice types and dynamics to the longitudinal sequence of river forms and flows typically encountered along the sedimentary links of gravel-bed rivers. Sedimentary links are discrete river segments each characterized by a node of coarse sediment recruitment followed by a gradual downstream fining of substrate and an associated reduction of channel slope. Because these downstream changes in substrate and slope are associated with changes in channel morphology and hydraulics, they create a longitudinal sequence of river environments moving from steep, fast flowing and highly turbulent boulder bed channels at the head of links to meandering low-gradient sand channels with calm flows at the downstream end. We describe and show examples of how these spatial variations in the geomorphology and flow characteristics of gravel-bed rivers should interact with river ice processes to produce a predictable 'most probable' large-scale pattern of river ice types and dynamics. Copyright (C) 2011 John Wiley & Sons, Ltd.
作者
我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。
推荐
暂无数据