Wave-Current Sediment Interaction is a sediment transport modeling phenomenon representing the coupled hydrodynamic process in which oscillatory wave motions and unidirectional current flows jointly influence the entrainment, transportation, and deposition of sediments in coastal and marine environments.
170
Publications
7.3K
Citations
493
Authors
235
Institutions
Publications per year
2017–2026
32
Parents
Publications
170
1–5 of 170
Authors
493
- XL
5
h-index
- YJ
5
h-index
- OS
4
h-index
- RB
3
h-index
- DJ
3
h-index
1–5 of 493
Institutions
235
United States Geological Survey
Reston, United States
10 h-index
18 publications
1.1K citations
National Oceanography Centre
Southampton, United Kingdom
9 h-index
17 publications
1K citations
Ocean University of China
Qingdao, China
8 h-index
37 publications
1.3K citations
University of Southampton
Southampton, United Kingdom
6 h-index
13 publications
542 citations
State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering
Nanjing, China
6 h-index
10 publications
292 citations
Centre National de la Recherche Scientifique
Paris, France
6 h-index
22 publications
899 citations
Woods Hole Oceanographic Institution
Falmouth, United States
6 h-index
9 publications
544 citations
Chinese Academy of Sciences
Beijing, China
5 h-index
11 publications
493 citations
1–8 of 235
Venues
- Marine Geology
24 publications · 1.4K citations
20
h-index
- Continental Shelf Research
16 publications · 641 citations
15
h-index
- Coastal Engineering
13 publications · 593 citations
13
h-index
- Journal of Sedimentary Research
JSR · 6 publications · 416 citations
6
h-index
- Coastal Engineering Proceedings
Conference · 5 publications · 315 citations
5
h-index
1–5