Sediment Resuspension Due to Near‐Bed Turbulent Effects: A Deep Sea Case Study on the Northwest Continental Slope of Western Australia
- Submitting institution
-
University of East London
- Unit of assessment
- 12 - Engineering
- Output identifier
- 25
- Type
- D - Journal article
- DOI
-
10.1029/2018JC013819
- Title of journal
- Journal of Geophysical Research: Oceans
- Article number
- -
- First page
- 7102
- Volume
- 123
- Issue
- 10
- ISSN
- 2169-9275
- Open access status
- Compliant
- Month of publication
- -
- Year of publication
- 2018
- URL
-
-
- Supplementary information
-
-
- Request cross-referral to
- -
- Output has been delayed by COVID-19
- No
- COVID-19 affected output statement
- -
- Forensic science
- No
- Criminology
- No
- Interdisciplinary
- No
- Number of additional authors
-
3
- Research group(s)
-
4 - Flood Risk Modelling and Mapping
- Proposed double-weighted
- No
- Reserve for an output with double weighting
- No
- Additional information
- Prediction of coastal erosion rates requires in-depth understanding of sediment transport rates. Obtaining field measurements in deep water (-375 m), this study revealed that contemporary methods for predicting coastal erosion rates need to be improved. Currently, predictions are based on the mean velocity of sediment particles; this paper advances our understanding of particle movement at lower velocities, enabling development of new equations and models. The study is thus of great significance for practicing engineers and coastal managers. This research was undertaken in a partnership with the University of Western Australia, in which I acted as an external advisor.
- Author contribution statement
- -
- Non-English
- No
- English abstract
- -