Fjord Circulation
Fjord Circulation is a hydrodynamic process characterized by the net movement and vertical exchange of water masses in a fjord estuary, driven by freshwater discharge and density gradients, which establishes a two-layer flow regime distinct from other estuarine circulation types due to its strong stratification and limited tidal mixing in high-latitude coastal environments.
289
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18.2K
Citations
824
Authors
287
Institutions
Publications per year
2017–2026
81
289
Finlo Cottier, Vigdis Tverberg, Mark Inall et al. · Journal of Geophysical Research Atmospheres · 2005 · 491 citations · Full text
Fjords: Processes and Products
John T. Andrews, James P. M. Syvitski, David C. Burrell et al. · Arctic and Alpine Research · 1988 · 418 citations
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Woods Hole Oceanographic Institution, United States
16 publications · 1.8K citations
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Woods Hole Oceanographic Institution
Falmouth, United States
21 h-index
41 publications
4.5K citations
University of Bergen
Bergen, Norway
20 h-index
55 publications
11K citations

Polish Academy of Sciences
Warsaw, Poland
17 h-index
63 publications
11K citations
Instytut Oceanologii Polskiej Akademii Nauk
Sopot, Poland
16 h-index
57 publications
10.7K citations
Scottish Association For Marine Science
Oban, United Kingdom
16 h-index
29 publications
3.2K citations
Grønlands Naturinstitut
Nuuk, Greenland
15 h-index
50 publications
6.1K citations

Norwegian Polar Institute
Tromsø, Norway
13 h-index
29 publications
4.4K citations
UiT The Arctic University of Norway
Tromsø, Norway
13 h-index
29 publications
2.1K citations
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19 publications · 1.3K citations
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18 publications · 1K citations
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18 publications · 815 citations
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12 publications · 820 citations
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14 publications · 812 citations
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