Density Current Propagation
Density Current Propagation is a physical fluid dynamics process in which a gravitational flow of water with a higher density than the surrounding ambient fluid advances horizontally along the bottom or interface of a receiving water body, driven primarily by density differences arising from variations in salinity, temperature, or suspended sediment concentration.
39
Publications
3K
Citations
92
Authors
57
Institutions
Publications per year
2017–2026
6
Parents
39
Density Currents Entering Lakes and Reservoirs
Vahid Alavian, Gerhard H. Jirka, Richard A. Denton et al. · Journal of Hydraulic Engineering · 1992 · 138 citations
1–5 of 39
92
4
h-index
4
h-index
NSF National Center for Atmospheric Research, United States
3 publications · 97 citations
3
h-index
3
h-index
University of Illinois Urbana-Champaign, United States
2 publications · 100 citations
2
h-index
1–5 of 92
57
University of Oklahoma
Norman, United States
4 h-index
7 publications
346 citations
University of Florida
Gainesville, United States
3 h-index
5 publications
245 citations

NSF National Center for Atmospheric Research
Boulder, United States
3 h-index
4 publications
114 citations

Cooperative Institute for Mesoscale Meteorological Studies
Norman, United States
3 h-index
3 publications
149 citations
Institut de Mécanique des Fluides de Toulouse
Toulouse, France
3 h-index
4 publications
205 citations

Université Toulouse III - Paul Sabatier
Toulouse, France
2 h-index
2 publications
61 citations
Institut National Polytechnique de Toulouse
Toulouse, France
2 h-index
2 publications
61 citations

Centre National de la Recherche Scientifique
Paris, France
2 h-index
2 publications
61 citations
1–8 of 57
7 publications · 255 citations
7
h-index
4 publications · 132 citations
4
h-index
2 publications · 33 citations
2
h-index
2 publications · 49 citations
2
h-index
2 publications · 159 citations
2
h-index
1–5