Alongshore Circulation
Alongshore Circulation is a coastal hydrodynamic process constituting a component of nearshore circulation systems, distinguished by the directed movement of water and associated transport of mass, momentum, and sediments parallel to the shoreline, typically driven by wave obliquity, tidal forcing, or wind stress gradients along the coast.
376
Publications
21.7K
Citations
830
Authors
316
Institutions
Publications per year
2017–2026
58
Variants
Longshore Circulation
Parents
376
1–5 of 376
830
15
h-index
10
h-index
10
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10
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9
h-index
1–5 of 830
316
Oregon State University
Corvallis, United States
29 h-index
80 publications
4.8K citations
Woods Hole Oceanographic Institution
Falmouth, United States
21 h-index
39 publications
2.6K citations

Scripps Institution of Oceanography
La Jolla, United States
18 h-index
54 publications
2.8K citations
University of Washington
Seattle, United States
15 h-index
28 publications
2.1K citations

UNSW Sydney
Sydney, Australia
12 h-index
27 publications
1.1K citations
University of California San Diego
San Diego, United States
12 h-index
32 publications
1.6K citations
Institut de Recherche pour le Développement
Marseille, France
12 h-index
45 publications
2.1K citations

Centre National de la Recherche Scientifique
Paris, France
11 h-index
41 publications
2.1K citations
1–8 of 316
JGR · 111 publications · 8.8K citations
56
h-index
87 publications · 5.2K citations
41
h-index
32 publications · 1.2K citations
20
h-index
14 publications · 758 citations
12
h-index
8 publications · 725 citations
8
h-index
1–5