Coasts, Marine Structures and Breakwaters: Adapting to Change 2010
DOI: 10.1680/cmsb.41318.0054
|View full text |Cite
|
Sign up to set email alerts
|

Effect of protruding roughness elements on wave overtopping

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2022
2022
2024
2024

Publication Types

Select...
2

Relationship

0
2

Authors

Journals

citations
Cited by 2 publications
(1 citation statement)
references
References 0 publications
0
1
0
Order By: Relevance
“…The description of an ocean surface roughness, including asymmetric surface effects, has been studied both theoretically and experimentally [1]- [3]. To a first approximation, an ocean surface can be considered as a linear superposition of statistically independent time records of free waves described by their energy spectrum [4], [5]; however, the non-linearity of wave interactions [6], such as surf beats [7], wave breaking [8], and energy transfer between wave components [9], which are important in later stages of wave development and determine the equilibrium state [10], [11], could not be accounted for [12]- [14]. Therefore, statistical formulations utilizing high-order energy cumulants of the scattering process in the presence of wind-waves have been used to describe the continuous interactions and energy exchanges, comprising the ocean and atmosphere, hereinafter referred to as random ocean media (ROM) [15], [16].…”
Section: Introductionmentioning
confidence: 99%
“…The description of an ocean surface roughness, including asymmetric surface effects, has been studied both theoretically and experimentally [1]- [3]. To a first approximation, an ocean surface can be considered as a linear superposition of statistically independent time records of free waves described by their energy spectrum [4], [5]; however, the non-linearity of wave interactions [6], such as surf beats [7], wave breaking [8], and energy transfer between wave components [9], which are important in later stages of wave development and determine the equilibrium state [10], [11], could not be accounted for [12]- [14]. Therefore, statistical formulations utilizing high-order energy cumulants of the scattering process in the presence of wind-waves have been used to describe the continuous interactions and energy exchanges, comprising the ocean and atmosphere, hereinafter referred to as random ocean media (ROM) [15], [16].…”
Section: Introductionmentioning
confidence: 99%