Can Bankfull Discharge and Bankfull Channel Characteristics of an Alluvial Meandering River be Cospecified From a Flow Duration Curve?-Reference-Cited by-同舟云学术

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Can Bankfull Discharge and Bankfull Channel Characteristics of an Alluvial Meandering River be Cospecified From a Flow Duration Curve?

Published:2019-10 Issue:10 Volume:124 Page:2381-2401
ISSN:2169-9003
Container-title:Journal of Geophysical Research: Earth Surface
language:en
Short-container-title:J. Geophys. Res. Earth Surf.

Author:

Naito Kensuke¹²^ORCID,Parker Gary¹³^ORCID

Affiliation:

1. Department of Civil and Environmental Engineering University of Illinois at Urbana‐Champaign Urbana IL USA

2. Centro de Investigacion y Tecnologia del Agua Universidad de Ingenieria y Tecnologia Lima Peru

3. Department of Geology University of Illinois at Urbana‐Champaign Urbana IL USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JF004971

Reference94 articles.

1. Spatial and temporal dynamics of sediment accumulation and exchange along Strickland River floodplains (Papua New Guinea) over decadal-to-centennial timescales

2. The distribution and strength of riparian tree roots in relation to riverbank reinforcement

3. Meander geometry arising from varying flows

4. The influence of riparian vegetation on stream width, eastern Pennsylvania, USA

5. Bank stability and channel width adjustment, East Fork River, Wyoming

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