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South coordinate must be a number between -90 and 90.

West coordinate must be a number between -180 and 180.

North coordinate must be a number between -90 and 90.

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Longitude coordinate must be a number between -180 and 180.

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South coordinate must be a number between -90 and 90.

West coordinate must be a number between -180 and 180.

North coordinate must be a number between -90 and 90.

East coordinate must be a number between -180 and 180.

Latitude coordinate must be a number between -90 and 90.

Longitude coordinate must be a number between -180 and 180.

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Long:

Start:

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South coordinate must be a number between -90 and 90.

West coordinate must be a number between -180 and 180.

North coordinate must be a number between -90 and 90.

East coordinate must be a number between -180 and 180.

Latitude coordinate must be a number between -90 and 90.

Longitude coordinate must be a number between -180 and 180.

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All Fields Title Author Description Keyword Subject Publication Date Access Author Affiliation Contributor Geolocation - Box Geolocation - Place Geolocation - Point Item URL Publisher License Source repository Series

South coordinate must be a number between -90 and 90.

West coordinate must be a number between -180 and 180.

North coordinate must be a number between -90 and 90.

East coordinate must be a number between -180 and 180.

Latitude coordinate must be a number between -90 and 90.

Longitude coordinate must be a number between -180 and 180.

Select a geolocation place from the options dropdown or remove this field

All Fields: Title: Author: Description: Keyword: Subject: Publication Date: Access: Author Affiliation: Contributor: Geolocation - Box: Geolocation - Place: Geolocation - Point: Item URL: Publisher: License: Source repository: Series:

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Data and code for Bed and Bank Stress Partitioning in Bedrock Rivers

Federated Research Data Repository / dépôt fédéré de données de recherche

Li, Tingan; Venditti, Jeremy G.; Rennie, Colin D.; Nelson, Peter — 2021-10-30 The is the data and code for Bed and Bank Stress Partitioning in Bedrock Rivers submitted to Journal of Geophysical Research, Earth Surface. The data includes the velocity profiles, the topography, the width, and the shear stress distributions obaserved in the Fraser Canyons, the raw data is from the dataset https://doi.org/10.20383/101.0277; The data also includes the modelled ratio of wall to bed stress as a function of bank angles, bottom channel width and discharge, calculated from the Ray-Isovel Model; The Matlab code of the Ray-Isovel Model can be found from the file RIM, which was written by our coauther Peter Nelson. The main function of the model is fraser.m, you can run fraser.m using an example. If you want to change inputs, you can open getinput_fin1.m, and change varibles, for example ks, qw, bank angles.

Data and code for A Model for Lateral Erosion of Bedrock Channel Banks by Bedload and Suspended Load

Venditti, Jeremy G.; Li, Tingan; Sklar, Leonard; Lamb, Michael — 2022-10-12

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(Source Repository: FRDR) AND (Author: Li, Tingan)

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SFU Research Data (FRDR)4

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Li, Tingan2
Cyr, Frédéric4
Hopkinson, Christopher D.4
Lindsay, Matthew B.J.4
Liu, Juewen4
Morrissey, Christy A.4
Schoepfer, Valerie A.4
Chasmer, Laura3

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