Abstract
We investigate the effects of storms on finite amplitude sand wave growth using a new idealized nonlinear morphodynamic model. We find that the growth speed initially linearly increases with sand wave amplitude, after which nonlinear effects cause the growth to decrease. This finally leads to an equilibrium amplitude. Storm processes lower the equilibrium amplitude compared to the fair-weather (tide-only) situation.
Original language | English |
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Pages | 1-3 |
Publication status | Published - 28 Jun 2017 |
Event | 4th International Symposium on Shallow Flows, ISSF 2017 - Eindhoven University of Technology, Eindhoven, Netherlands Duration: 26 Jun 2017 → 28 Jun 2017 Conference number: 4 http://issf2017.tue.nl/ http://issf2017.tue.nl/program/programme_ISSF.pdf |
Conference
Conference | 4th International Symposium on Shallow Flows, ISSF 2017 |
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Abbreviated title | ISSF 2017 |
Country/Territory | Netherlands |
City | Eindhoven |
Period | 26/06/17 → 28/06/17 |
Internet address |
Keywords
- tidal sand waves
- storm effects
- nonlinear dynamics
- morphodynamic modelling