Coastal Inflow
Coastal Inflow is a hydrodynamic process denoting the directed movement of offshore water masses into coastal regions, distinguished by its role in advecting momentum, heat, nutrients, and sediments across the continental shelf break under the influence of meteorological, tidal, and density-driven forcing mechanisms.
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2.2K
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155
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2017–2026
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Causes of Salinity Intrusion in Coastal Belt of Bangladesh
Md. Mahmuduzzaman, Zahir Ahmed, A. K. M. Nuruzzaman et al. · International Journal of Plant Research · 2014 · 138 citations
Some controls on flow and salinity in Bering Strait
Knut Aagaard, Thomas J. Weingartner, Seth L. Danielson et al. · Geophysical Research Letters · 2006 · 129 citations
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Brookhaven National Laboratory
Upton, United States
2 h-index
6 publications
438 citations
University of Washington
Seattle, United States
2 h-index
3 publications
381 citations
University of Maryland Center for Environmental Science
Cambridge, United States
2 h-index
2 publications
159 citations
Woods Hole Oceanographic Institution
Falmouth, United States
2 h-index
3 publications
306 citations
Istituto di Scienze Marine del Consiglio Nazionale delle Ricerche
Venice, Italy
2 h-index
3 publications
102 citations

University of Alaska Fairbanks
Fairbanks, United States
2 h-index
7 publications
675 citations

Centre National de la Recherche Scientifique
Paris, France
2 h-index
8 publications
248 citations

Scripps Institution of Oceanography
La Jolla, United States
2 h-index
2 publications
197 citations
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3 publications · 141 citations
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JCR · 3 publications · 44 citations
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2 publications · 25 citations
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2 publications · 123 citations
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2 publications · 146 citations
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