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TitleModelling seabed disturbance and sediment mobility on the Canadian Atlantic Shelf
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LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorLi, M ZORCID logo; Wu, Y; Hannah, C G; Perrie, W A; Shen, H; King, E L
SourceGeological Survey of Canada, Open File 8805, 2021, 50 pages, https://doi.org/10.4095/328363 Open Access logo Open Access
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Year2021
PublisherNatural Resources Canada
Documentopen file
Lang.English
Mediaon-line; digital
File formatpdf
ProvinceEastern offshore region; Northern offshore region; Newfoundland and Labrador; Nova Scotia; Prince Edward Island; New Brunswick; Nunavut; Quebec; British Columbia; Alberta; Saskatchewan; Manitoba; Ontario; Quebec; New Brunswick; Nova Scotia; Prince Edward Island; Newfoundland and Labrador; Northwest Territories; Yukon; Nunavut; Canada
NTS1; 2; 3; 10; 11; 12; 13; 14; 15; 16; 20; 21; 22; 24; 25; 26; 27; 28; 29; 37; 38; 39; 120
AreaAtlantic Ocean; Hudson Strait; Gulf of St. Lawrence; Davis Strait; Labrador Sea; Baffin Bay; Nares Strait; Bay of Fundy; Scotian Shelf; The Grand Banks of Newfoundland; Canada; Greenland; Denmark
Lat/Long WENS -80.0000 -42.0000 84.0000 39.0000
Subjectsmarine geology; surficial geology/geomorphology; sedimentology; environmental geology; Nature and Environment; Science and Technology; marine sediments; marine environments; continental margins; continental shelf; oceanography; currents; current circulation; storms; sediment stability; sediment distribution; sediment dispersal; sediment transport; grain size analyses; shear stress; stress analyses; bathymetry; benthos; modelling; models; statistical analyses; Atlantic Continental Shelf; Seabed Disturbance Index (SDI); Sediment Mobility Index (SMI); Habitats; Land management; Methodology; Classification
Illustrationsgeoscientific sketch maps; location maps; tables
ProgramMarine Geoscience for Marine Spatial Planning
Released2021 06 08
Abstract(Summary)
Ocean surface waves and tidal currents can interact to produce strong seabed shear stress and mobilization of sediments that can significantly impact the seabed stability and benthic habitats on continental shelves. Therefore the knowledge of the magnitude and frequency of seabed disturbance by waves and currents and the resulting mobilisation of sediment on continental shelves is critical for the spatial planning and management of Canada's offshore lands. Modelled waves, tidal current and circulation current data for a 3-year period were used in a combined-flow sediment transport model to simulate the seabed shear stresses and the mobilization of observed sediment grain size on the Canadian Atlantic Shelf. The modelling results are presented and analyzed to derive updated framework of seabed disturbance and sediment mobility on the Atlantic Shelf.
The Atlantic Shelf is affected by strong waves and tidal currents. Maximum mean significant wave height can reach 3.5 m and that of the mean tidal currents up to 1.2 m·s-1. Our modeled results indicate that the mean wave and tidal current shear velocities both reach the maximum values of ~4 cm·s-1. Our models predict that observed sediments on the Atlantic Shelf can be mobilized by tidal currents at least once during the modelled 3 year period over 30% of the shelf area while storms can mobilize sediments over 35% of the shelf area suggesting slightly stronger sediment mobilization by storms. Further more waves and currents interact to cause enhanced combined wave-current shear velocity >5 cm·s-1 that is capable to mobilize sediments over 63% of the shelf area, double that due to either tides or waves.
The spatial variation of the relative importance of waves, tidal current and circulation current in mobilizing sediments was used to classify the Atlantic Shelf into six disturbance types. Wave dominant and tide dominant disturbance types are equally important and both occupy ~25% of the shelf area. Mixed disturbance is insignificant and accounts for only 3% of the shelf area. Universal indices of Seabed Disturbance (SDI) and Sediment Mobility (SMI) were applied to better quantify the exposure of the seabed to oceanographic processes and sediment mobility incorporating both the magnitude and frequency of these processes. The applications of these indices have produced different and probably more adequate quantification of seabed forcing and sediment mobility for many areas on the Atlantic Shelf. The values of SDI and SMI on the Canadian Atlantic Shelf are found to be comparable to those on the Australian shelf. These indices, together with the seabed disturbance type classification scheme, potentially can be used as standard parameters to best quantify seabed disturbance and sediment mobility on other shelves of the world.
Summary(Plain Language Summary, not published)
Modelling Seabed Disturbance and Sediment Mobility on the Canadian Atlantic Shelf Modelled waves, tidal current and circulation current for a 3-year period were used in a sediment transport model to quantify the seabed shear stresses and the mobilization of observed sediment grain size on the Canadian Atlantic Shelf. The study results led to the updated framework of seabed disturbance and sediment mobility on the Atlantic Shelf. Strong waves and tidal currents produce mean bed shear velocity > 5 cm/s and cause sediment mobilization for >60% of the time over the Atlantic Shelf. The relative importance of waves, tidal current and circulation current in mobilizing sediments was used to classify the Atlantic Shelf into six disturbance types. The results of the study are important for environmental assessments, planning for seabed infrastructure, and better understanding of seabed fisheries.
GEOSCAN ID328363

 
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