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About Lecture 4: Bottom Roughness in Coastal Environments
This lecture discusses bottom roughness in coastal environments. It identifies four main types of roughness: sediment grains (Nikuradse roughness), biogenic structures from benthic organisms, saltating sediment grains, and bedforms such as ripples. Relationships have been developed to predict the physical and hydrodynamic roughness scales associated with each type. The roughness hierarchy and dominant type present depends on factors like sediment grain size, bed shear stresses, and wave versus current flow conditions. Being able to estimate bottom roughness is important for modeling sediment transport and seafloor morphology in coastal waters.
Detailed Information
| Author: | ['Oky Ikhramullah'] |
|---|---|
| Publication Year: | 2013 |
| Pages: | 5 |
| Language: | English |
| Format: | |
| Price: | FREE |
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