Lateral Circulation
Lateral Circulation is a hydrodynamic process in fjord estuaries characterized by the secondary cross-channel flow patterns that arise due to the interaction of density gradients, bathymetric steering, and tidal forcing, distinguishing it from dominant longitudinal estuarine circulation.
60
Publications
3.1K
Citations
136
Authors
77
Institutions
Publications per year
2017–2026
19
60
Hans Burchard, Robert D. Hetland, Elisabeth Schulz et al. · Journal of Physical Oceanography · 2010 · 171 citations · Full text
1–5 of 60
136
University of Maryland Center for Environmental Science, United States
8 publications · 280 citations
8
h-index
6
h-index
Rutgers, The State University of New Jersey, United States
5 publications · 182 citations
5
h-index
Leibniz Institute for Baltic Sea Research Warnemünde, Germany
4 publications · 315 citations
4
h-index
4
h-index
1–5 of 136
77
University of Maryland Center for Environmental Science
Cambridge, United States
10 h-index
20 publications
646 citations
Woods Hole Oceanographic Institution
Falmouth, United States
9 h-index
19 publications
1.1K citations
Rutgers, The State University of New Jersey
New Brunswick, United States
5 h-index
6 publications
240 citations
University of Florida
Gainesville, United States
5 h-index
8 publications
310 citations
University of California, Berkeley
Berkeley, United States
4 h-index
7 publications
263 citations

Leibniz Institute for Baltic Sea Research Warnemünde
Warnemünde, Germany
4 h-index
8 publications
637 citations
William & Mary
Williamsburg, United States
3 h-index
7 publications
185 citations

Old Dominion University
Norfolk, United States
3 h-index
4 publications
342 citations
1–8 of 77
21 publications · 1.4K citations
19
h-index
JGR · 10 publications · 696 citations
10
h-index
6 publications · 270 citations
6
h-index
5 publications · 104 citations
5
h-index
4 publications · 149 citations
4
h-index
1–5