Publications des scientifiques de l'IRD

Blaas M., Dong C. M., Marchesiello Patrick, McWilliams J. C., Stolzenbach K. D. (2007). Sediment-transport modeling on Southern Californian shelves : a ROMS case study. Continental Shelf Research, 27 (6), p. 832-853. ISSN 0278-4343.

Titre du document
Sediment-transport modeling on Southern Californian shelves : a ROMS case study
Année de publication
2007
Type de document
Article référencé dans le Web of Science WOS:000245622700006
Auteurs
Blaas M., Dong C. M., Marchesiello Patrick, McWilliams J. C., Stolzenbach K. D.
Source
Continental Shelf Research, 2007, 27 (6), p. 832-853 ISSN 0278-4343
Suspended sediment- transport processes in Santa Monica and San Pedro Bay are analyzed using the sedimen t-tran sport capabilities of the Regional Oceanic Modeling System (ROMS). A one-month simulation for December 2001 has been carried out with a set of nested domains. The model inputs include tides, winds, surface waves, and idealized initial sediment conditions for sand and non-cohesive silt. Apart from the control run, the sensitivity of the results to surface waves, ripple roughness and bed armoring has been analyzed. From the control experiment, the horizontal transport of sand turns out to be limited to within a few km of the nearshore erosion zones. During high wave events, silt is transported over further distances and also partly offshelf in distinct plumes. The effectiveness of horizontal silt transport depends strongly on vertical mixing due to both surface wind stress and wave-enhanced bottom stress. High wave events coincident with strong winds (hence strong vertical mixing) are the most optimal conditions for sed iment- transport. Excluding wave effects in the simulation shows that surface waves are the dominant factor in resuspending bed material on the Southern Californian shelves. The sensitivity experiments also show that the direct influence of additional ripple roughness on erosion and deposition is relatively weak. Switching off bed armoring locally results in increases of near-bottom concentrations by a factor of 20 for silt and a factor of 5 for sand as well as stronger spatial gradients in grain size.
Plan de classement
Limnologie physique / Océanographie physique [032] ; Géologie et formations superficielles [064]
Localisation
Fonds IRD [F B010037943]
Identifiant IRD
fdi:010037943
Contact