Abstract
Richards [1980] conjectured that megaripples of the continental shelf are due to a seabed instability in the presence of seabed ripples. Towards a better understanding of this megaripple formation process, we use a morphodynamical numerical model to investigate the bed roughness influence on the bed load¿induced linear stability of a sandy bed. We find that the linearly most amplified mode shifts from a dune mode (grain roughness) towards a megaripple mode (large bed roughness). Then, we discuss how megaripples could be generated over a flat bed and over dunes.
Original language | English |
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Article number | L13214 |
Number of pages | 5 |
Journal | Geophysical research letters |
Volume | 31 |
Issue number | 13 |
DOIs | |
Publication status | Published - 2004 |
Keywords
- IR-46110
- METIS-214058