Research Spotlight: What controls bedrock channel geometry?

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چکیده

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منابع مشابه

Controls and limits on bedrock channel geometry

[1] Data on channel geometry in naturally incising bedrock rivers reveal variable relationships between channel width, slope, and erosion rate. To explain the range of relationships between these parameters, we propose an optimized channel geometry model. The model reproduces previous theoretical and numerical modeling scaling relationships; however, to explain the field data, the model must in...

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Research Spotlight

Introduction Recent natural and man-made disastrous events underscore the importance of emergency evacuation planning and management for buildings and facilities (Averill et al., 2005). Although building codes include provisions for egress design, their prescriptive nature poses many limitations in terms of providing effective evacuation for specific buildings, each of which is unique. Human be...

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Lithologic and Tectonic Controls on Bedrock Channel Form at the Northwest Himalayan Front

Recognition that channel form reflects a river's ability to erode rock has spawned stream-power models that estimate patterns of incision by approximating energy dissipation within a channel. Most commonly, these models assume channel width exponentially scales with drainage area, in part, because drainage area is easily extracted from digital elevation models (DEMs). However, this assumption i...

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Controls on the channel width of rivers: Implications for modeling fluvial incision of bedrock

On the basis of the Manning equation and basic mass conservation principles, we derive an expression for scaling the steadystate width (W) of river channels as a function of discharge (Q), channel slope (S), roughness (n), and width-to-depth ratio (!): W " [!(! # 2)2/3]3/8Q3/8S$3/16n3/8. We propose that channel width-todepth ratio, in addition to roughness, is a function of the material in whic...

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Tectonic and lithologic controls on bedrock channel profiles and processes in coastal California

[1] Recent theoretical models suggest that topographic characteristics of bedrock channels are products of interactions among tectonics, substrate resistance, and the climatically modulated erosive ability of the river. The degree to which these factors influence the form of channel profiles is poorly quantified at present. Here we investigate bedrock channels developed across the southern flan...

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ژورنال

عنوان ژورنال: Eos, Transactions American Geophysical Union

سال: 2011

ISSN: 0096-3941,2324-9250

DOI: 10.1029/2011eo050011