Hyperpycnal Flows is a type of sediment-laden turbidity current that occurs when riverine inflow into a standing body of water has a higher density than the ambient water due to suspended sediment, resulting in flow that plunges and travels along the bed.
99
Publications
8.4K
Citations
326
Authors
187
Institutions
Publications per year
2017–2026
31
Variants
Hyperpycnal Currents
Parents
Publications
99
1–5 of 99
Authors
326
- JPJames P. M. Syvitski
Institute of Arctic and Alpine Research, United States
6 publications · 2.1K citations
6
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- CZ
5
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- FL
4
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- DC
4
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- AV
3
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1–5 of 326
Institutions
187
The University of Texas at Austin
Austin, United States
6 h-index
14 publications
1.5K citations
Centre National de la Recherche Scientifique
Paris, France
6 h-index
13 publications
428 citations
Sinopec (China)
Beijing, China
5 h-index
8 publications
421 citations
China University of Petroleum, Beijing
Beijing, China
5 h-index
16 publications
268 citations
Universidad Nacional del Sur
Bahía Blanca, Argentina
4 h-index
5 publications
630 citations
University of Colorado Boulder
Boulder, United States
4 h-index
5 publications
1.8K citations
Institute of Environmental Geology and Geoengineering
Monterotondo, Italy
4 h-index
10 publications
688 citations
Geological Survey of Canada
Ottawa, Canada
4 h-index
4 publications
660 citations
1–8 of 187
Venues
- Sedimentology
16 publications · 1K citations
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- Journal of Sedimentary Research
JSR · 9 publications · 1.5K citations
9
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- Geophysical Research Letters
6 publications · 321 citations
6
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- AAPG Bulletin
5 publications · 953 citations
5
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- Journal of Palaeogeography
6 publications · 237 citations
5
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1–5